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246 Sentences With "conformably"

How to use conformably in a sentence? Find typical usage patterns (collocations)/phrases/context for "conformably" and check conjugation/comparative form for "conformably". Mastering all the usages of "conformably" from sentence examples published by news publications.

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Nonetheless, a resolution to approve the pay plans passed conformably, with only 4.5% of investors voting against.
Indeed, it seems to me that, conformably with the sage advice (not a herb or culinary flavour enhancer) given to James Hacker, by his principal private secretary, Bernard Woolley in "Yes, Prime Minister", only a cognitively challenged emulsified high-fat offal tube will do if we are to avoid the lanolin-encased naturally ovine fibres being pulled in front of our ocular enabling mechanisms.
The El Peñón Formation, part of the Villeta Group, conformably overlies the Trincheras Formation and is conformably overlain by the Capotes Formation.
Relative age dating of the Tuscarora places it in the Silurian period. It rests conformably atop the Clinton Group and conformably below the Bloomsburg Formation.
The Fort St. John Group is conformably overlain by the Dunvegan Formation and conformably underlain by the Bullhead Group or may rest disconformably on older units.
It conformably overlies the Mount Hawk Formation or the Southesk Formation, and is conformably overlain by the Sassenach Formation or the Palliser Formation, depending on the location.
The Muskwa Formation is a sub-unit of the Horn River Formation; it is conformably overlain by the Fort Simpson Formation and conformably underlain by the Otter Park Member.
The formation consists of red sandstones and mudstones and has a total thickness in excess of . It conformably overlies the Shinarump Conglomerate and conformably underlies the Petrified Forest Formation.
The Tuscarora rests conformably atop the Juniata Formation and conformably below the Clinton Group in Pennsylvania.Berg, T.M., et al., (1983). Stratagraphic Correlation Chart of Pennsylvania: G75, Pennsylvania Geologic Survey, Harrisburg, Pennsylvania.
The Lower Siwalik is conformably overlain by the Middle Siwalik.
The Middle Siwalik is conformably overlain by the Upper Siwalik.
Relative age dating of the Clinton Group places it in the Lower Silurian period. It rests conformably atop the Tuscarora Formation and conformably below the Lower and Upper Silurian Lockport Group and Bloomsburg Formation.
The Monteith Formation is the basal formation of the Minnes Group. It was deposited conformably over the marine shales of the Fernie Formation and is conformably overlain by the Beattie Peaks Formation. To the south it grades into the Nikanassin Formation.
The Shaunavon Formation is conformably overlain by the Sawtooth Formation and conformably overlays the Gravelbourg Formation. It is equivalent to the Sawtooth Formation in southern Alberta, as well as to the Bowes member and Firemoon Member of the Piper Formation in Montana.
The formation consists mostly of dark green to olive clay shale with some thin siltstone beds and highly fossiliferous calcareous beds. It lies conformably on the Muleros Formation and is conformably overlain by the Mojado Formation. Total thickness is . Lucas et al.
The formation consists of gray shale with some interbedded siltstone and silty limestone, with some fine grained sandstone towards the top of the formation. The total thickness is . It rests conformably on the Del Norte Formation and is conformably overlain by the Muleros Formation.
The Tetcho Formation is conformably overlain by the Kotcho Formation and conformably overlays the Trout River Formation and Fort Simpson Formation. It is equivalent to the lower Wabamun Group in Alberta and to parts of the Besa River Formation in the Liard area of British Columbia.
The Beattie Peaks Formation is part of the Minnes Group. It was deposited conformably on the Monteith Formation and is conformably overlain by the Monach Formation, both of which also belong to the Minnes Group. To the south it grades into the lower part of the Gorman Creek Formation.
Thickness is . The formation rests conformably on the Sandia Formation and is disconformably overlain by the Alamitos Formation.
The Saskatchewan Group is conformably overlain by the Three Forks Group and conformably overlays the Manitoba Group carbonates. It is equivalent to the upper Beaverhill Lake Formation, the Woodbend Group and the lower part of the Winterburn Group in central Alberta, and with the Jefferson Group in Montana and North Dakota.
The micropaleontological content of the Jagüel Formation made it possible to classify it as Maastrichtian–Danian (Early and Late). This formation conformably overlies the Allen Formation and it also conformably underlies the Roca Formation . The Pircala–El Carrizo Formation lies above these formations. All of them belong to the Malargüe Group.
The Clearwater Formation is part of the Mannville Group. It is conformably overlain by the Grand Rapids Formation and conformably overlies the McMurray Formation. It is equivalent to the Bluesky Formation and the lower Spirit River Formation in the Peace River region, and may be equivalent to the Cummings Member in the Lloydminster region.
The Gaviota Formation is deposited conformably on top of the Coldwater-Sacate in the western part of the dual unit's extent, and the Sespe Formation appears conformably on top of it elsewhere.Dibblee, Thomas. Geology of Southwestern Santa Barbara County, California. State of California, Department of Natural Resources, Division of Mines, Bulletin 150. 1950. 28.
The formation is divided into two informal members. The lower member is mostly calcareous shale with some interbedded fine sandstone and nodular limestone, while the upper member is fossiliferous medium-gray limestone interbedded with tan shale. The two sections are and thick. The formation lies conformably on the Finlay Limestone and is conformably overlain by the Smeltertown Formation.
The Debolt Formation is the upper most component of the Rundle Group. It rests conformably on the Shunda Formation, resting on shale and carbonates. It is overlain conformably by the Golata Formation of the Stoddart Group in the west, and the upper contact becomes unconformable with gradually newer formations to the east and north (Permian, Triassic, Jurassic and Cretaceous beds).
The Peace River Formation is a sub-division of the Fort St. John Group. It is conformably overlain by the Shaftesbury Formation shale and is conformably underlain by the Spirit River Formation. It is equivalent to the Commotion Formation in British Columbia and to the Scatter Formation in the Liard River area. It correlates to the Buckinghorse Formation in north-eastern British Columbia.
The Muskiki Formationis is part of the Smoky Group. It is conformably underlain by the Cardium Formation and conformably overlain by the Bad Heart Formation. The Kaskapau Formation in northern Alberta replaces the upper Blackstone Formation, the Cardium Formation, and the Muskiki Formation. Where the Kaskapau Formation includes post Cardium beds, the Muskiki is considered a member of the Wapiabi Formation.
The Stonewall Formation is overlain by the Interlake Group (conformably in the south, disconformably in the north) and sharply overlays the Stony Mountain Formation.
The Kotaneelee Formation is gradually overlain by the Wapiti Group and conformably overlays the Dunvegan Formation. It is equivalent to the Wapiabi Formation in Alberta.
The Monach Formation is part of the Minnes Group. It was deposited conformably on the Beattie Peaks Formation and is conformably overlain by the Bickford Formation, both of which also belong to the Minnes Group. To the east where it was removed by erosion, the Monach Formation is unconformably overlain by the Cadomin Formation. To the south it grades into the Gorman Creek Formation.
The Duvernay Formation is a unit of the Woodbend Group. It is conformably overlain by the Ireton Formation and Grosmont Formation and it conformably overlays the Cooking Lake Formation. It is equivalent to the Leduc Formation reefs. it is equivalent to the Perdrix Formation in the Rocky Mountains, and is the stratigraphical equivalent of the Muskwa Formation in the Fort Nelson area of North-Eastern British Columbia.
Within the Bajuvaric Unit the Ruhpolding Formation conformably overlies the Chiemgau Beds, further west in the Allgäu Alps it overlies the upper Allgäu Beds. It is conformably overlain by the so-called Aptychus Limestone of the Ammergau Formation. The changeover to the Aptychus Limestone is gradual. The lower contact of the Ruhpolding Formation is very distinct and outlined by a several centimeter thick bedding joint.
The Bonneterre Formation is an Upper Cambrian geologic formation which outcrops in the St. Francois Mountains of the Missouri Ozarks. The Bonneterre is a major host rock for the lead ores of the Missouri Lead Belt. The Bonneterre Formation lies conformably on the Lamotte Sandstone and in places lies directly on the Proterozoic igneous core of the mountains. The Bonneterre is conformably overlain by the Davis Formation.
The Dunvegan Formation is conformably overlain by marine shales of the Kaskapau Formation in the Peace River Country and overlies conformably and transitionally the shale of the Fort St. John Group. The relationship between the Dunvegan and the overlying/underlying units is diachronous and the boundaries of the Dunvegan are placed at the first and last appearances of sandstone within the shale- dominated succession.
The St. Mary River Formation conformably overlies the Blood Reserve Sandstone, or the Bearpaw Formation where the Blood Reserve Sandstone is absent, and it is conformably overlain by the Willow Creek Formation. It extends from Glacier County, Montana to as far north as the Little Bow River in Alberta, where it grades into and intertongues with the contemporaneous strata of the Horseshoe Canyon Formation.
Relative age dating of the Wills Creek places it in the Silurian period. It rests conformably a top the Bloomsburg Formation and below the Tonoloway Formation.
The Eldon Formation is present in the southern Rocky Mountains of southwestern Alberta and southeastern British Columbia. It reaches a maximum thickness of about 500 metres (1,640 feet) at Mount Bosworth on the Alberta-British Columbia border. The Eldon conformably overlies the Stephen Formation, which hosts the fossils of the Burgess shale, in the south, and the Snake Indian Formation in the north. It is conformably overlain by the Pika Formation.
The Whitemud Formation is part of the Edmonton Group. It rests conformably on the Eastend Formation in Saskatchewan and in the Cypress Hills area; on the Horseshoe Canyon Formation in the Drumheller area; and on the St. Mary River Formation in the Oldman River area. In southeastern Saskatchewan it is unconformably overlain by the Frenchman Formation; and in all other areas it is conformably overlain by the Battle Formation.
Relative age dating of the Reedsville places it in the Upper Ordovician. It rests conformably atop the Upper Ordovician Coburn Formation at the top of the Trenton Group limestone and conformably below the Bald Eagle Formation. Isotopic dating of shale mylonite in Pennsylvania reveals a K-Ar age of 372+/-8 Ma.Lapham, D.M., and Root, S.I., 1971, Summary of isotopic age determinations in Pennsylvania: Pennsylvania Geological Survey Information Circular, 4th series, no. 70, 29 p.
The Grosmont Formation is conformably overlain by the Nisku Formation of the Winterburn Group or by a thin part of the Ireton Formation (to which it is equivalent in the south). It conformably overlays the Ireton Formation or Duvernay Formation. At the subcrop edge at its northeastern limit it is unconformably overlain by the McMurray Formation of the Mannville Group. The lower Grosmont is equivalent to the Mikkwa Formation in northern Alberta.
The Spirit River Formation is conformably overlain by the Peace River Formation and conformably underlain by the Bluesky Formation. It grades laterally to the Buckinghorse Formation shales to the north-east, and into the sandy facies of the Malcolm Creek Formation south of the Wapiti River. It is equivalent to the upper Mannville Formation in Central Alberta and to the Clearwater Formation and Grand Rapids Formation in the upper Athabaska River area.
The Schooler Creek Group is unconformably overlain by the Fernie shale, or by the Bullhead or Fort St. John Group. It conformably overlies the Toad Formation or the Doig Formation.
Azapa Formation () is a geological formation in northern Chile made up of gravels of fluvial origin. It is conformably overlain by Oxaya Formation. Azapa Formation is deformed by the Oxaya anticline.
The Wapta member has been redefined into the Raymond Quarry member, Emerald Lake member, Odaray member, Paradox member and Marpole member. The thin Stephen grades conformably into the overlying Eldon formation.
The Mist Mountain Formation is the middle unit of the Kootenay Group. It rests conformably on the cliff-forming sandstones of the Moose Mountain Member of the Morrissey Formation, and is conformably overlain by the Elk Formation. In the eastern foothills, the Elk Formation has been removed by erosion and the Mist Mountain Formation is unconformably overlain by the Cadomin Formation. North of the North Saskatchewan River, the Mist Mountain Formation grades into the Nikanassin Formation.
The Viking Formation is conformably overlain by the Big River Formation and conformably and unconformably underlain by the Joli Fou Formation. It is equivalent to the Bow Island Formation in southern Alberta, to the Newcastle Formation in North Dakota, to the Ashville Formation in Manitoba, the Pelican Sandstone in north-eastern Alberta and the Flotten Lake Sand in central Saskatchewan. It can be correlated with the Cadotte Member of the Peace River Formation in north-western Alberta.
The Organ Rock Formation is conformably underlain by the Cedar Mesa Sandstone. It is conformably overlain by the De Chelly Sandstone around Monument Valley and by the White Rim Sandstone in the Canyonlands National Park. In locations where the De Chelly and White Rim are absent, the Organ Rock is unconformably overlain by the Triassic Moenkopi or Chinle Formations by an erosional contact. Toward its eastern extent, the Organ Rock Formation grades into the Cutler Formation, undivided.
Bouchard Lake has given its name to the Bouchard Formation, a geologic unit "composed principally of interbedded micaceous quartzite and quartzose argillite that conformably overlies the Sloway formation" exposed near the lake.
The Three Forks Group conformably overlies the Saskatchewan Group and is disconformably overlain by the Madison Group. It is equivalent to the sum of the Wabamun Group and Exshaw Formation in Alberta.
The Boonton Formation rests conformably above the Hook Mountain Basalt, placing its deposition sometime between approximately 197 and 190 million years ago during the late Hettangian stage and Sinemurian stage of the Jurassic.
The Gravelbourg Formation is conformably overlain by the Shaunavon Formation. It conformably overlies the Watrous Formation in Manitoba and southeastern Saskatchewan, and unconformably overlays the Madison Group in south-eastern Alberta. The Lower Gravelbourg is equivalent to the Reston Formation in Manitoba and parts of the Nesson Formation in North Dakota and Montana, while the Upper Gravelbourg is equivalent to the lower Melita Formation in southeastern Manitoba and the Tampico Shale of the Piper Formation in North Dakota and Montana.
The Morrissey Formation abruptly but conformably overlies the "Passage Beds" at the top of the Fernie Formation, and is in turn abruptly but conformably overlain by the Mist Mountain Formation. To the north in the vicinity of the North Saskatchewan River it interfingers with and grades into the Nikanassin Formation. To the east it was truncated by pre-Aptian erosion and is unconformably overlain by the Cadomin Formation. Its correlation south of the Canada-United States border in Montana is uncertain.
The Santa Teresa Formation conformably overlies the San Juan de Río Seco Formation and is covered by subrecent alluvium. The formation is part of the sequence after the Eocene unconformity.Lamus Ochoa et al., 2013, p.
The Feltville Formation rests conformably above the Orange Mountain Basalt and below the Preakness Basalt, placing its deposition somewhere between approximately 199 and 196 million years ago during the early Jurassic stage known as the Hettangian.
The formation consists mostly of sandstone and shale, with some limestone, and siltstone.Lucas et al. 1998 It rests conformably on the U-Bar Formation and is unconformably overlain by the Cowboy Spring Formation.The total thickness is .
The Towaco Formation rests conformably above the Preakness Mountain Basalt and below the Hook Mountain Basalt, placing its deposition somewhere between approximately 198 and 197 million years ago during the early Jurassic stage known as the Hettangian.
The Slave Point Formation is unconformably overlain by the Beaverhill Lake Group or Waterways Formation in northern Alberta and by the Otter Park Member or Muskwa Member of the Horn River Formation in north-eastern British Columbia. It conformably overlays the Fort Vermilion Formation (or is unconformably overlain by the Watt Mountain Formation) in northern Alberta and it is conformably overlain by the Sulphur Point Formation or Presqu'ile Formation in north-eastern British Columbia. It is equivalent to the lower Swan Hills Formation and partly to the Livock River Formation.
Although some early workers included the Bluesky Formation in the Bullhead Group, it is usually classified as the basal unit of the Fort St. John Group. It is conformably overlain by the Wilrich Member of the Spirit River Formation and conformably underlain by the Gething Formation. Northeast of the town of Peace River it was deposited unconformably on Mississippian limestone. It is equivalent with the Glauconitic Sandstone of the Mannville Group in central and southern Alberta, as well as with the Wabiskaw Member of the Clearwater Formation in the eastern part of northern Alberta.
The Herald Formation is disconformably overlain by the Stony Mountain Formation and conformably overlays the Yeoman Formation. It can be correlated with the Fort Garry Member of the Red River Formation in Manitoba and in the Williston Basin.
At its base it consists of green shale and sandstone and coarsens upwards to arkosic conglomerates. The lower Ordovician Aydos Formation conformably overlies the Soḡuksu. It is a conglomerate of quartzitic sandstone and is 50–200 meters thick.
Tableado Formation is the uppermost member of Way Group. It is made up of limestone and shale deposited in the shallow marine conditions of the continental shelf. The limestones contains fossils. It rests conformably on top of Lombriz Formation.
La Negra Formation deposited diachronously along a series of intra-arc basins and overlies conformably the formations of Pan de Azúcar and Posada de los Hidalgo. The formation is intruded by plutons of varied composition including gabbro and granite.
The Simijaca Formation conformably overlies the Chiquinquirá Sandstone, and the Hiló and Pacho Formations, and is overlain by the La Frontera Formation.Acosta & Ulloa, 2001, p.32 The age has been estimated to be Turonian, or Cenomanian.Acosta & Ulloa, 2001, p.
The Boulder Creek Formation is part of the Fort St. John Group. Originally described as a member of the Commotion Formation, the Boulder Creek was elevated to formational status along with the other members of the Commotion by D.F. Stott in 1982, who proposed that the term 'Commotion Formation' be abandoned. The Boulder Creek Formation conformably overlies the marine shales of the Hulcross Formation, and is conformably overlain by the marine shales of the Hasler Formation. It is equivalent to the Cadotte Member, and possibly the Paddy Member, of the Peace River Formation of the Peace River plains.
The Woodbend Group is conformably overlain by the Winterburn Group and conformably overlays the Beaverhill Lake Group. It is transgressive in the Peace River Arch and Tathlina uplift. Newer deposits rest on the Woodbend group upon an erosional surface in eastern Alberta, south-central Saskatchewan and Manitoba. It is equivalent to the Birdbear Formation and Duperow Formation in northern Montana, southern Saskatchewan and southwestern Manitoba, as well as parts of the Fort Simpson Formation and Muskwa Formation of northeastern British Columbia and southern Yukon, while it corresponds to the Tathlina Formation, Twin Falls Formation and Hay River Formation in the Northwest Territories.
The Flat Landing Brook Formation is the middle member of the Tetagouche Group. Exposures between Route 490 and the headwaters of Flat Landing Brook are the type locality. It is conformably overlain by massive pillowed alkali basalt of the Little River Formation and conformably underlain by crystal tuff as well as quartz-feldspar augen schist of the Nepisiguit Falls Formation. The contact of the Flat Landing Brook and Little River formations is exposed in the Brunswick Mines area and near California Lake whereas the contact of the Flat Landing Brook and Nepisiguit Falls formations is exposed along The Narrows of the Nepisiguit River.
The Thermopolis Shale was first identified in 1914 by geologist Ferdinand F. Hintze, Jr. He called it the "Lower Benton Shale", and included the Mowry Shale in the same formation. Hintze described three members: The basal "rusty beds", a lower shale, a thick "Muddy Sand" (muddy sandstone), and an upper shale member. (The fourth member of the "Lower Benton Shale" was the Mowry Shale.) The Thermopolis Shale was first named by geologist Charles T. Lupton in 1916. Lupton described the rocks as a formation lying conformably atop the Cloverly Formation, and conformably underlying the Mowry Shale.
The Smoky Group is conformably and transgressively followed by the Wapiti Group and rests conformably on the Dunvegan Formation sandstone. The Cardium sandstone and Muskiki shale are replacing the upper parts of the Kaskapau Formation in the south-east of the distribution area. The entire group correlates with the Blackstone Formation, Cardium Formation and Wapiabi Formation of the Alberta Group in the southern foothills. The equivalent stratigraphic sequence in central Alberta consists of the Lea Park Formation and the upper Colorado Group, in north-eastern Alberta it correlates with Labiche Formation, and with the Kotaneelee Formation in the Liard River area.
Folding and foliation occurred in northeast Tasmania during the Devonian after the granites appeared. The Eldon Group finished forming in a shallow marine environment with quartz sandstone and mudstone lying conformably on the Gordon Group rocks. Fossils include brachiopods, gastropods, bryozoans, and tentaculites.
The Wapiti Group forms the present day erosional surface in British Columbia, and is overlain by the Scollard Formation in its eastern reaches. It conformably and gradually overlays the Kotaneelee Formation in British Columbia, and the Smoky Group in north-western Alberta.
The Seca Formation, part of the Ancón Group, conformably overlies the Socorro Formation and is overlain by the Punta Ancón Formation. The Seca Formation comprises grey to greenish shales deposited in a marine platform with submarine fans environment.Lorenzo et al., 2018, p.
It was first seen on the Dassault Milan and later on the Tupolev Tu-144. NASA has also investigated a one-piece slewed equivalent called the conformably stowable canard, where as the surface is stowed one side sweeps backwards and the other forwards..
The Mount Wilson Formation is present in the Rocky Mountains of Alberta and British Columbia. It rests conformably on the Owen Creek Formation in the eastern main ranges and on the Glenogle Formation in the western main ranges, and is overlain by the Beaverfoot Formation.
The Perdrix Formation overlies the Maligne Formation or, where the Maligne is absent, the Flume Formation. It is conformably overlain by the Mount Hawk Formation and the contact is gradational. Laterally it interfingers with the Peechee Formation and the reefs of the Cairn Formation.
The Labiche Formation is overlain by the Belly River Formation and conformably overlays the Pelican Formation. It is equivalent to the parts of the Colorado Group in central Alberta and to the sum of Smoky Group, Dunvegan Formation and Shaftesbury Formation in north- western Alberta.
When in contact with Upper Cretaceous limestone, Nubian Sandstone underlies the latter conformably. In Lebanon, Anti-Lebanon and Hermon it is underlain by Jurassic limestone. Its upper strata is likely from the Lower or Middle Cretaceous age. However, Jurassic limestone is absent in southern areas.
The Nonesuch Shale is a Proterozoic geologic formation that outcrops in Michigan and Wisconsin, United States, but has been found by drill holes to extend in the subsurface as far southwest as Iowa. The Nonesuch is a lacustrine sequence of shale, siltstone, and sandstone, 150 to 210 m thick, that conformably overlies the alluvial Copper Harbor Conglomerate and is conformably overlain by the fluvial Freda Sandstone. Together, the Copper Harbor, Nonesuch, and Freda make up the Oronto Group.Scott W. Imbus and others, "Organic geochemistry and sedimentology of middle Proterozoic Nonesuch Formation - hydrocarbon source rock assessment of a lacustrine rift deposit," in Lacustrine Basin Exploration, Tulsa, Okla.
Dibblee, Thomas. Geology of the central Santa Ynez Mountains, Santa Barbara County, California. Bulletin 186, California Division of Mines and Geology. San Francisco, 1966. 51.Dibblee (1966), 42-43 The base of the unit, which rests conformably on the shallower-water Vaqueros Formation, contains a glauconitic layer.
The Pine Point Formation is overlain by the Presqu'ile Formation and Sulphur Point Formation; It conformably overlays the Chinchaga Formation and Fitzgerald Formation. It is equivalent to Muskeg Formation in northern Alberta, the Dunedin Formation in British Columbia and the upper Nahanni Formation in western Northwest Territories.
The Kotcho Formation is overlain by the Exshaw Formation and conformably overlays the Tetcho Formation. To the east, it grades into the upper Wabamun Group carbonate, and to the south-west into the Palliser Formation. To the east it is replaced by the Besa River Formation shale.
The Drina Formation ("Drina Formacija") is a stratigraphic unit in Bosnia and Herzegovina and Serbia. It was deposited between the Cambrian and the Carboniferous onto Neoproterozoic basement. It is composed of clastic sediments, limestone and volcanic rocks. The Drina Formation is conformably overlain by the Golja Formation.
Due to its large areal extent, the Cardium Formation falls within different stratigraphic groups in different regions (Alberta Group, Colorado Group, and Smoky Group). It is conformably overlain by the Wapiabi Formation and underlain by the Blackstone Formation. The formation is partly equivalent to the Kaskapau Formation.
1, p. 171-181. The Arapahoe Formation consists of alluvial fan and fluvial deposits that prograded eastward from the growing Rocky Mountain Front Ranges. It rests unconformably on the Laramie Formation, and is conformably overlain by the Denver Formation. It reaches a maximum thickness of about .
The formation conformably overlies the Perdrix Formation or, in the Crows Nest Pass area, the Borsato Formation. It is overlain by Sassenach Formation. It is laterally equivalent to the reefal carbonate rocks of the Southesk Formation, and in some areas it interfingers with or is overlain by the Southesk.
The Keg River Formation is conformably overlain by the Muskeg Formation and unconformably overlays the Chinchaga Formation. It is equivalent to the Pine Point Formation, Hume Formation and Nahanni Formation in north-eastern British Columbia and the Northwest Territories and to the Winnipegosis Formation in Saskatchewan and eastern Alberta.
The Manitoba Group is conformably overlain by the Duperow Formation and disconformably overlays the Prairie Evaporite Formation or Winnipegosis Formation of the Elk Point Group. The lower Manitoba Group is equivalent to the Muskeg Formation in northern Alberta, while the upper part correlates with the Beaverhill Lake Formation.
The Judith River Formation conformably overlies the Claggett Formation and Pakowki Formation. It is overlain by the Bearpaw Formation. It is equivalent to the Belly River Formation in the southern Canadian Rockies foothills, the Lea Park Formation in central Alberta and the Wapiti Formation in the northwestern plains.
The Kakisa Formation is disconformably overlain by the Trout River Formation and conformably overlays the Redknife Formation (east) or the Fort Simpson Formation (west). It is equivalent to parts of the Winterburn Group in central Alberta. Towards the west, it becomes shaley and turns into the Fort Simpson Formation.
Relative age dating of the Mahantango places it in the Middle Devonian period, being deposited between 392 and 385 (±3) million years ago. It rests conformably atop the Marcellus Formation shale. Its upper contact is also conformable to the Trimmers Rock Formation and Harrell Shale.Berg, T.M., et al.
In the southern part of the basin, thick sequences of volcanic rock are common. Black shale near Badakshan has been found to contain extensive Triassic fossils. In the east, Jurassic limestone, marl, shale and sandstone conformably overlies Triassic sediments. Volcanic rocks intercalate these units between Kabul and Khost.
Relative age dating of the Stockton places it in the Upper Triassic System, i.e., deposition between 237 and 207 (±5) million years ago. It rests unconformably a top many different formations of the Appalachian Piedmont. It interfingers with the Lockatong Formation and also rests conformably below the Passaic Formation.
The Caballero Formation consists of nodular gray argillaceous limestone, which grades upward into nodular gray marl with shale lenses. It rests conformably on the Percha Shale and is overlain unconformably by the Lake Valley Limestone. The formation likely correlates with the Chouteau Limestone of the upper Mississippi valley.
The south face of the Tanner Graben block shows three distinct geology units, all conformably laid members of the Grand Canyon Supergroup-(and Unkar Group), and are at a paleo-tilted (fault) angle of about 15 degrees. The prominence is horizontal (15 degrees dip to ~north-northeast?) caprock section of distinctively, multi-layered Nankoweap Formation, which is unit 2 of the Grand Canyon Supergroup. The Nankoweap Formation is conformably laid on member units 5 and 4 of the Unkar Group, the lowest and first group of the Grand Canyon Supergroup. The black Cardenas Basalt, unit 5 makes up much of the Tanner Graben; it sits on erodable, softer, reddish, and layered-(inter-bedded) Dox Formation.
Relative age dating of the Bald Eagle places it in the Ordovician period. It rests atop the Axemann Formation (Oa), or the Nittany Formation, for example between Tyrone and Water Street, Pennsylvania, where the Axemann is missing, and the Loysburg Formation of interbedded limestone and dolomite conformably overlies the Bellefonte Formation.
The Gething Formation is the uppermost unit of the Bullhead Group. It conformably overlies the Cadomin Formation and is disconformably overlain by the Bluesky Formation. It is correlated with the Gladstone Formation in the southern foothills, and is equivalent in age to the McMurray Formation that contains the Athabasca Oil Sands.
The Trincheras Formation is the lowermost unit of the Villeta Group,Acosta & Ulloa, 2001, p.22 and conformably overlies the Murca, La Naveta and Útica Formations. The formation is overlain in a transitional pattern by the Socotá and El Peñón Formations. The Trincheras Formation is subdivided into the El Tigre and Anapoima Members.
The Gladstone Formation rests conformably on the Cadomin Formation. It is overlain by the Beaver Mines Formation in the south, and by the Moosebar Formation in the north. It is equivalent to the Gething Formation of northeastern British Columbia. The upper calcareous portion is equivalent to the Ostracod Beds of the Alberta plains.
The Elk Formation is the uppermost unit of the Kootenay Group. It gradationally and conformably overlies the Mist Mountain Formation. It is disconformably overlain by the Cadomin Formation and to the east it was truncated by pre- Cadomin erosion. To the north Elk strata may correlate with part of the Nikanassin Formation.
Geochemical Journal, 41, 201-211 The Yilanli is a dolomitic limestone unit with calcareous black and gray shales. It was deposited in a shallow marine passive margin setting. It is conformably overlain by the Alacaagzi Formation, and has accumulated over 1000 m of sediment. The Alacaagzi Formation contains economic deposits of coal.
The Kozlu is composed of successional conglomerate, sand, silt, mud, and coal deposits. The Karadon Formation conformably overlies the Kozlu. The Karadon is lithologically similar to the Kozlu Formation, but contains less coal seams. An angular unconformity spans the top of the Karadon formation and ranges from 46.5 Ma–194 Ma in duration.
The formation consists mostly of gray red to red or mottled gray green mudstone containing limestone nodules. About 25% of the formation is massive fine-grained laminar gray red sandstone. It rests conformably on the Santa Rosa Formation, and is overlain disconformably by the Trujillo Formation. The total thickness of the formation is .
Relative age dating of the Hamilton places it in the middle and lower Devonian period. In Maryland, it rests conformably atop the Tioga Metabentonite Bed of thinly laminated shale with a thickness less than one foot over the Needmore Shale, and conformably below the Brallier Formation (formerly Woodmont Shale) dark laminated shale in the east, Harrell Shale dark laminated shale in the west, and Tully Limestone in the subsurface of Garrett County. In Pennsylvania it lies atop the Onondaga Formation limestone and shale forming a sharp conformable contact with the Selinsgrove Limestone of that formation, and lies beneath the Portage (Brallier, Harrell, Burket) dark shales of the Harrell Formation. In 2012, Read and Erikson reported the group as dating from the Eifelian to Famennian in Virginia.
Similar sediments collected from a shale folded in the core of the Four Peaks synform yielded a MDA of 1580 Mya. In the Upper Salt River Canyon, overlying the White Ledge Formation (a correlative to the Mazatzal Group), sediments from the conformably overlying Yankee Joe and Blackjack Formations yielded MDA of ca. 1470 Mya.
The Skoki is present in the Canadian Rockies of Alberta and British Columbia. It reaches a thickness of up to 186 metres (610 ft) in the southern Rockies and about 500 metres (1800 ft) in the northern Rockies. It conformably overlies the Outram Formation or the Tipperary Quartzite, depending on the location, and underlies the Owen Creek Formation.
The Green Ammonite Member is up to 31 metres thick predominantly consists of medium grey mudstones, with 3 limestone horizons, Lower Limestone; Red Band, and Upper Limestone, it is conformably overlain by the Dyrham Formation in some areas, but in the Charmouth area there is an erosive unconformable boundary with the much younger Albian aged Gault clays.
The Muskeg Formation is disconformably overlain by the Watt Mountain Formation and conformably underlain by the Keg River Formation. It is correlated with the Pine Point Formation, Presqu'ile Formation and Sulphur Point Formation. It grades into the halite-rich Prairie Evaporite Formation to the southeast through a decrease in its anhydrite content and an increase in its halite content.
The Fernie Formation is conformably overlain by the Morrissey Formation in the south, by the Nikanassin Formation in central Alberta and by the Monteith Formation in northeastern British Columbia. It rests disconformably on Triassic units in the west, and unconformably on upper Paleozoic units such as the Schooler Creek Group and the Montney Formation farther east.
Relative age dating of the Old Port places it in the Lower Devonian period. It rests conformably atop the Keyser Formation and usually unconformably below the Needmore FormationStratigraphic correlation chart of Pennsylvania, T. M. Berg, M. K. McInerney, J. H. Way, and D. B. MacLachlan. 1983; 3rd printing, revised, 1993. 1 sheet, 42" x 58", plus 2 p. addendum.
The Palliser Formation is disconformably overlain by the Exshaw Formation and conformably underlain by the Alexo Formation. It is equivalent to the Wabamun Group in central Alberta, to the middle part of the Three Forks Formation in Saskatchewan and Montana and to the Tetcho Formation and Kotcho Formation in the Fort Nelson area of British Columbia.
The Stoddart Group is overlain by the Ishbel Group in the foothills and the Prophet Formation in the northern plains; it conformably overlays the Debolt Formation. It can be correlated with the Tunnel Mountain Formation, the Kananaskis Formation, the Mattson Formation and the Mount Head Formation of the southern Canadian Rockies, and with the Amsden Formation in Montana.
Simplified stratigraphy of the Angoumian The Angoumian is usually divided into two formations, a lower Angoumien inférieur and an upper Angoumien supérieur. Some authors even attribute the Ligerian (in French Ligérien) to the Angoumian and then call it basal Angoumian. The Angoumian sensu stricto conformably overlies the Ligerian and closes with a hardground towards the overlying Coniacian.
The Eastend Formation is conformably overlain by the Whitemud Formation and gradually overlies the Bearpaw Formation. In the Frenchman River valley, the Eastend Formation is erosionally overlain by the Frenchman Formation. It is equivalent to St. Mary River Formation and Horseshoe Canyon Formation in southern Alberta, as well as the Fox Hills Formation in Montana and North Dakota.
Relative age dating of the Mauch Chunk places it in the late Mississippian epoch, with some of the top layers in the early Pennsylvanian epoch, being deposited between 345 and 320(±3) million years ago. It rests conformably atop many formations. Its upper contact is complex. In certain areas, the contact is conformable in others, there is an unconformity.
Retrieved 8 July 2014. The Hale Formation has two named members: the Cane Hill and the Prairie Grove Members. The lower member is the Cane Hill, a primarily sandstone and shale interval that unconformably overlies the Mississippian-age Pitkin Formation. The upper member, the Prairie Grove Member, is predominately limestone and conformably underlies the Bloyd Formation.
The Rundle Group is disconformably overlain by the Rocky Mountain Formation in the front ranges of the Canadian Rockies and by the Fernie Formation in the foothills and by Cretaceous beds in the prairies. It conformably overlies the Banff Formation. The Rundle Group can be correlated with the Mission Canyon Formation in southern Saskatchewan, northeastern Montana and North Dakota.
The Beaverhill Lake Group is conformably underlain by the formations of the Elk Point Group. In most areas it is conformably overlain by the formations of the Woodbend Group, and in northwestern Alberta and northeastern British Columbia it is disconformably overlain by the Muskwa Formation. It is equivalent to the Souris River Formation in southeastern Alberta, Saskatchewan and Manitoba, and to the Flume Formation of the Fairholme Group in the Canadian Rockies. According to D.L Griffin, it is equivalent to the Slave Point Formation and Waterways Formation in northeastern Alberta, with the Slave Point Formation and the lower Hay River Formation in the District of Mackenzie, as well as the Horn River Formation and Fort Simpson Formation northwest of the Slave Point-Keg River facies in northeastern British Columbia and the Northwest Territories.
The Flume Formation rests unconformably on formations of late Cambrian to Ordovician age or, in parts of the mountains and foothills, on the Middle Devonian Yahatinda Formation. It is conformably overlain by the reefs of the Cairn Formation, or where they are absent, by the Southesk Formation. It is equivalent in part to the upper Beaverhill Lake Group farther to the east.
Geological Survey, Department of Mineral And Energy Affairs, Republic of South Africa. It follows conformably after the Ecca Group and unconformably underlies the Stormberg Group. Based on stratigraphic position, lithostratigraphic and biostratigraphic correlations, palynological analyses, and other means of geological dating, the Beaufort Group rocks are considered to range between Middle Permian (Wordian) to Early Triassic (Anisian) in age.Rubidge, B. S. (ed.) 1995b.
They were held for a few days in Lower Shawneetown before escaping and walking for 23 days to reach Pittsburgh.Samuel Hazard, ed. Pennsylvania Archives: 1st Series: Selected and Arranged from Original Documents in the Office of the Secretary of the Commonwealth, Conformably to Acts of the General Assembly, February 15, 1851, and March 1, 1852. Pennsylvania, Secretary of the Commonwealth.
The type locality of the Portezuelo Formation is the mountain range known as Sierra del Portezuelo in Neuquén Province.Wichmann, 1929 This formation conformably overlies the Lisandro Formation of the Río Limay Subgroup. In the top layers it grades into the Plottier Formation, the younger formation within the Río Neuquén Subgroup. Sandstones and siltstones, probably deposited under fluvial conditions, make up the Portezuelo Formation.
During the Ordovician Tasmania was near the equator and was joined to Gondwana. The Tyennan Block was uplifted with the Great Lyell Scarp as an active fault. The Ordovician Wurawina supergroup comprises the Denison Group and the Gordon group. The Owen Conglomerate, part of the Denison group, lies conformably on the Dundas Group, but unconformably on the Mount Read Volcanics.
The Tunjuelo Formation conformably overlies the Marichuela Formation and in other parts the Subachoque Formation. The Tunjuelo Formation is overlain by the thin Chía Formation. The age has been estimated to be Pleistocene based on palynology and radiocarbon dating, covering the Pleistocene from 2.6 to 0.01 Ma.Montoya & Reyes, 2005, p.72 The depositional environment has been interpreted as fluvio- glacial terraces.
The Grayling Formation unconformably overlies the Permian Fantasque Formation. It is equivalent to the lower Montney Formation in the subsurface of the Peace River plains and to the Phroso Siltstone Member of the Sulphur Mountain Formation in west-central and southwestern Alberta. Its contact with the overlying Toad Formation is gradational. The Toad Formation is conformably overlain by the Liard Formation.
The Ma Butte Formation is also known as the Mill Creek Formation. It disconformably overlies the Beaver Mines Formation. It is conformably overlain by the Crowsnest Formation in the south and the contact between the two is gradational. It is disconformably overlain by the Blackstone Formation in the north, and it is correlative with the Bow Island Formation to the east.
The Nakaye Formation is mostly massive ledges of gray to dark gray, very fine to fine grained limestone with considerable bands, lenses,and nodules of chert. Typical beds are in thickness and are separated by shale beds thick or thin to medium-bedded limestone thick. Sandstone is absent.Kelley and Caswell 1952 The formation is thick and lies conformably on the Red House Formation.
The Albian, 105–100 Ma, Zonguldak Formation is predominantly limestone with areas of dolomitization.Hoşgörmez, H., Yalçin, M.N., Cramer, B., Gerling, P., Faber, E., Schaefer, R.G., and Mann, U. (2002). Isotopic and molecular composition of coal-bed gas in the Amasra region (Zonguldak basin—western Black Sea). Organic Geochemistry,33, 1429-1439 It is conformably overlain by the Albian, 105–112 Ma, Kilimli Formation.
The Baldonnel Formation is the middle member of the Schooler Creek Group. It is conformably overlain by the Pardonet Formation limestone and siltstone or unconformably overlain by the Fernie Formation shale. North of the Williston Lake it overlies the dolomite beds of the Charlie Lake Formation. It is equivalent to the upper parts of the McLearn Formation and Ludington Formation.
The Bullhead Group overlies a major regional unconformity caused by pre-Bullhead erosion. It rests unconformably on the Fernie Formation, the Nikanassin Formation, the Minnes Group or the Kootenay Group, depending on the location and the extent of the erosion. It is overlain conformably by the glauconitic sandstones and marine shales at the base of the Fort St. John Group.
The Southesk Formation is discontinuously present in the Canadian Rockies from Jasper National Park to the Flathead area of southeastern British Columbia. It is also present in the subsurface beneath the adjacent plains to the east. It conformably overlies the Cairn Formation or, in the Crows Nest Pass area, the Borsato Formation. At its margins it may interfinger with the Perdrix and Mount Hawk Formations.
The Mount Whyte Formation outcrops in the southern Rocky Mountains of southwestern Alberta and southeastern British Columbia, and is present in the subsurface beneath the southwestern Alberta plains where it grades onto the Earlie Formation. It grades into the Snake Indian Formation to the north and Naiset Formation to the west. It disconformably overlies the Lower Cambrian Gog Group and is conformably overlain by the Cathedral Formation.
The Trout River Formation is conformably overlain by the Tetcho Formation and disconformably overlays the Kakisa Formation. In its western extent, it overlies and grades into the Fort Simpson Formation. It is equivalent to the Sassenach Formation in the central Alberta Rockies, with the Graminia Formation in central Alberta, the Crowfoot Formation in southern Alberta, the Torquay Formation in Saskatchewan and Lyleton Formation in Manitoba.
The Kootenay Group conformably overlies the marine shales of the Fernie Formation. In most areas it is disconformably overlain by the nonmarine strata of the Blairmore Group, although in some western areas the contact may be conformable. North of the North Saskatchewan River the Kootenay Group grades into the Nikanassin Formation. To the south it may correlate with the upper part of the Morrison Formation in Montana.
The Cretaceous Seaway was already retreating east and to the south by the time the locally thick Straight Cliffs Formation was deposited.Davis and Pollock (2003). Geology of Bryce Canyon National Park, page 46 Its members represent various stages in this process. The cliff- forming sandstone of the Tibbet Canyon Member was conformably deposited on top of the Tropic Shale in shallow marine and later near shore environments.
Heinrich Harder's reconstruction of Arsinoitherium zitteli in the Oligocene grassland of Jebel Qatrani escarpment. The Jebel Qatrani Formation (also Gebel Qatrani) is a palaeontological and geologic formation located in the Faiyum Governorate of central Egypt. Conformably overlying the Qasr el Sagha Formation. It is exposed namely between the Jebel Qatrani escarpment and the Qasr el Sagha escarpment, north of Birket Qarun lake near Faiyum.
The Belly River Formation is conformably overlain by the Bearpaw Formation and gradually overlies the Wapiabi Formation, the Colorado Group shale or the Lea Park Formation shale. It is equivalent to the Milk River Formation and Pakowki Formation. The Belly River has group status in the Canadian Rockies foothills and is replaced by the Oldman Formation (Judith River Formation in Montana) and Foremost Formation in southern Alberta.
It is conformably overlain by the Haumurian to Teurian Whangai Formation. It consist of three members, the Maungataniwha Sandstone Member, the Mutuera Member and the Houpapa Member. It is named for Tahora Station, south of Matawai in the Gisborne Region. The aptly named Maungataniwha (Māori for "mountain of monsters") Sandstone Member is known for its rich reptile fossil remains, first investigated by amateur palaeontologist Joan Wiffen.
The Tunnel Mountain Formation is present in the front ranges of the Canadian Rockies of western Alberta, and reaches a maximum thickness of about 200 metres (600 ft). It unconformably overlies the Etherington Formation or the Todhunter Formation of the Mississippian Rundle Group, and is conformably overlain by the Late Pennsylvanian Kananaskis Formation. In areas where the Kananaskis is not present, it is unconformably overlain by the Permian Ishbel Group.
A piece of the Becraft Formation showing an abundance of crinoid and brachiopod fossils. The Becraft Formation is a geologic formation of marine sedimentary rock found in New York State. The Becraft is a part of the lower Devonian Helderberg Group and conformably overlies the New Scotland Formation and is overlain by the Alsen Formation throughout the lower Hudson Valley of New York State. The formation is Gedinnian in age.
The Whitehorse Formation is present in the Rocky Mountains and their foothills from the Canada–United States border in Alberta to the Sukunka River area of northeastern British Columbia. It is disconformably overlain by the Jurassic Fernie Formation and conformably underlain by the Sulphur Mountain Formation. It is correlative with the Charlie Lake, Ludington, Baldonnel and lower Pardonet Formations and, in the subsurface of northeastern British Columbia, the Schooler Creek Group.
The type locality of the Huincul Formation is near the town of Plaza Huincul in Neuquén Province after which the formation was named by Wichmann in 1929.Wichmann, 1929 This formation conformably overlies the Candeleros Formation, and it is in turn overlain by the Lisandro Formation. The Huincul Formation is thought to represent an arid environment with ephemeral or seasonal streams.Coria & Currie, 2006 In some areas, it is up to thick.
Such figures are frequently inscribed with formulas of dedication. Gods and goddesses posed conformably with their traditional characters and bearing their distinctive attributes are the most numerously represented class of later statuettes. They are a religious genre, appearing first in 4th-century sculpture and particularly favoured by Hellenistic sentiment and Roman pedantry. Many of them were doubtless votive figures, others were images in domestic shrines, and some were certainly ornaments.
The Tapinocephalus Assemblage Zone correlates with the Abrahamskraal Formation, Adelaide Subgroup of the Beaufort Group. Outcrops of this biozone are known from the south-western and central margins of the Abrahamskraal Formation where it conformably overlies the Eodicynodon Assemblage Zone in its south-western localities. In its northern and eastern localities it inter-fingers with Ecca Group-aged deposits. This biozone is considered to be Middle Permian (Guadalupian) in age.
The shale was deposited in the deep sea as turbidites. It can be found in Yarralumla, Parkes, Acton, north and south of Black Mountain, and from Lawson, to Crace and Ngunnawal. ;Black Mountain Sandstone Black Mountain Sandstone is deposited on top of State Circle Shale conformably. It is made up from thick beds of grey quartz sandstone mostly, but has some beds included of siltstone and grey shale.
The formation consists of interbedded gray to red sandstone and mudstone with minor conglomerate with a total thickness of . The formation disconformably rests on the Mesaverde Group and conformably underlies unnamed volcanic debris beds. In the vicinity of Sierra Blanca, the formation is intruded by dikes with K-Ar ages of 47.7 +/-2.9 Ma (million years ago). The formation is interpreted as deposited in a braided stream environment.
It is comprised predominantly of crossbedded black shales and silts in the lower sections of the unit and progressively becomes composed of sands, shale bearing coals, and conglomerates towards the top of the formation. Facies analysis in the Alacaagzi Formation is suggestive of coastal environments including lacustrine, fluviatial, and fan deposits. Conformably overlaying the Alacaagzi Formation is the Kozlu Formation. The Kozlu contains 19 coal seams totalling 30–32 m.
The Winterburn Group is conformably overlain by the Wabamun Group and overlays the Ireton Formation, except in the Peace River Arch, where it rests on the Precambrian basement. It is correlated with the Birdbear Formation and part of the Three Forks Group in Saskatchewan, with the Southesk Formation and Alexo Formation in the Canadian Rockies and with the Redknife Formation and Kakisa Formation in north-eastern British Columbia.
Leupold says "But at the same time a crushed head spells utter defeat." In the 1899 Douay-Rheims Bible, the footnote on Genesis 3:15 states: > "She shall crush": Ipsa, the woman; so divers of the fathers read this > place, conformably to the Latin: others read it ipsum, viz., the seed. The > sense is the same: for it is by her seed, Jesus Christ, that the woman > crushes the serpent's head.
The Lower Jurassic rocks conformably overlie the Upper Triassic units; so are the Early Cretaceous deposits over the Upper Jurassic strata (e.g., Zagros). In North and Central Iran, the Upper Triassic and Lower–Middle Jurassic sediments have a detrital nature, consisting mainly of shale and sandstone with thicknesses varying from a few meters to more than . The presence of plant remains and coal beds suggest a continental or lagoon environment for the deposits.
A section near the Neuquén City airport, north of the town of Plottier, is the type locality of the Plottier Formation.Fossa Mancini et al., 1938 At its base, this formation grades into the Portezuelo Formation, and it is in turn overlain conformably by the Bajo de la Carpa Formation, a unit of the Río Colorado Subgroup. The Plottier Formation is the thinnest formation within the Neuquén Group, with a maximum thickness of only .
Precambrian Environment in Hainan Island The Shilu Group was composed of siliciclastic and carbonate sedimentary rocks from shallow oceanic rifting environment with low grade metamorphism. Conformably lying above the Shilu Group was the Shihuiding Formation which was generally low-grade, siliciclastic rocks deposited in foreland basin. The sedimentation took place in the period between Late Mesoproterozoic and Early Neoproterozoic. The rocks were then regionally metamorphosed in the late South China Jinningian event.
Subduction in Late Paleozoic Above the angular unconformity, the Carboniferous and Permian units lied conformably with each other, both having similar characteristics in the rock layers. They showed low-grade metamorphism in siliciclastic and carbonate sedimentary rocks deposited in shallow to deep marine environment with fine-to-medium grain size. Also, there were granites (syenogranites and monzogranites) intruded at the age of ca. 300–250 Ma. They were generally seen with foliations as well.
Late Triassic (220 Ma) The Elliot Formation unconformably overlies the Molteno Formation and is conformably overlain by the Clarens Formation. Due to the reddish colour of the rocks, the Elliot Formation is colloquially referred to as the “Red Beds” in older literature. The Elliot Formation is dominated by mudstones and siltstones that can be finely laminated. However, the internal structures in the mudstones are often not visible due to locally poor laminations.
It is the lowest unit of the Nanxiong Basin, a small graben created during Mesozoic rifting. Buck et al. state that it overlies Jurassic granite basement, and is conformably overlain by the Shanghu Formation. Alternative stratigraphic schemes for the Nanxiong basin have been proposed, one of which refers to the Nanxiong succession as the Nanxiong Group, and dividing it into the Yuanfu, Zhutian and Zhenshui formations, and overlying the Albian to Turonian Changba Formation.
Detrital zircons from the Hopi Springs Shale in the northern Mazatzal Mountains yielded a maximum depositional age (MDA) of 1571 Mya. Similar sediments collected from a shale folded in the core of the Four Peaks synform yielded a MDA of 1580 Mya. In the Upper Salt River Canyon, overlying the White Ledge Formation (a correlative to the Mazatzal Group), sediments from the conformably overlying Yankee Joe and Blackjack Formations yielded MDA of ca. 1470 Mya.
The Blood Reserve Formation rests conformably on the marine shales and siltstones of the Bearpaw Formation, and is overlain by the floodplain deposits of the St. Mary River Formation. Its contacts with both are sharp. It is a continuation of the Horsethief Sandstone of northern Montana. It is correlated with the Black Eagle Member of the Bearpaw Formation in the Cypress Hills of southeastern Alberta, and with the lower part of the Horseshoe Canyon Formation to the north.
There is strong stratigraphic evidence that transition from Vendian to Lower Cambrian was a progressive one, without hiatuses; there is no evidence for any orogenic or epeirogenic movements in Iran at this time (e.g., south of Zanjan, Valiabad Chalus, Shahin Dezh). Early Cambrian started with an alternation of shale, phosphate-bearing limestone, and dolomite sitting conformably and transitionally over Vendian dolomites. Transition from Soltanieh Formation to Barut, Zaigoon, and Laloon Formations is very difficult to recognize in the field.
The Yorktown unconformably overlies the Miocene Eastover Formation, and conformably underlies the Pliocene Croatan Formation. The Yorktown was divided into members by Ward and Blackwelder (1980). These are in ascending order: Sunken Meadow Member, Rushmere Member, Morgarts Beach Member, and Moore House Member.Ward, L.W., and Blackwelder, B.W., 1980, Stratigraphic revision of upper Miocene and lower Pliocene beds of the Chesapeake Group, middle Atlantic Coastal Plain, IN Contributions to stratigraphy: U.S. Geological Survey Bulletin, 1482-D, 61 p.
The Ellerslie Member represents the lower part of the Mannville Group in southern and central Alberta. It is conformably overlain by the Ostracod Beds of the Manville Group and rests unconformably on Paleozoic strata such as the Banff Formation or Pekisko Formation, often separated by a Detrital Zone. It is correlated to the McMurray Formation in the Athabasca Oil Sands of north-eastern Alberta and the Dina Member in east-central Alberta and west-central Saskatchewan.
Devil's Peak as viewed from the Summit of Table Mountain. The upper, rocky parts of Devil's Peak, Table Mountain and Lion's Head consist of a hard, uniform and resistant sandstone commonly known as the Table Mountain sandstone or TMS. (This is, however, no longer used as a formal geological name). The tough sandstone rests conformably upon a basal shale that in turn lies unconformably upon a basement of older (Late Precambrian) rocks (Malmesbury shale/slate and the Cape Granite).
The Ardvreck Group is a stratigraphic group of early Cambrian age found in the Northwest Highlands of Scotland. It lies unconformably on gneisses of the Lewisian complex or sandstones of the Torridonian Supergroup. It consists of two formations, the basal quartzites and quartz arenites of the Eriboll Formation and the overlying dolomitic siltstones and sandstones and quartz arenites of the An-t-Sron Formation. It is overlain conformably by the Ghrudaidh Formation of the Durness Group.
The Bearpaw Formation conformably overlies the Dinosaur Park Formation of the Belly River Group in central Alberta, and the Judith River Formation in the plains to the east and Montana. It is overlain by the Horseshoe Canyon Formation in central Alberta; by the Blood Reserve Formation and the St. Mary River Formation in southern Alberta; by the Eastend Formation in southern Saskatchewan; and by the Fox Hills Formation in Montana. To the east, it merges into the Pierre Shale.
Early Ordovician (470 Ma) Early Silurian (440 Ma) The Letná Formation was first formally defined in 1966 by Havlíček and Vaněk and crops out in the Prague Basin, a northeast–southwest trending minibasin stretching over between Rokycany in the southwest and Úvaly in the northeast. The Prague Basin contains an Ordovician to Devonian succession in the larger Bohemian Massif.Mikuláš, 1998b, p.143 The formation conformably overlies the Libeň Formation and is overlain by the Vinice Formation.
The Pitkin Formation, or Pitkin Limestone, is a fossiliferous geologic formation in northern Arkansas that dates to the Chesterian Series of the late Mississippian. This formation was first named the "Archimedes Limestone" by David Dale Owen in 1858, but was replaced in 1904. The Pitkin conformably overlies the Fayetteville Shale and unconformably underlies the Pennsylvanian- age Hale Formation. Some workers have considered the top of the Pitkin Formation to be a separate formation called the Imo Formation.
The Oldman Formation is a member of the Belly River Group (also known as the Judith River Group). It conformably overlies the Foremost Formation, and is separated from the overlying Dinosaur Park Formation by a regional disconformity. The sediments of the Oldman are superficially similar to those of the Dinosaur Park, which was included in the Oldman Formation prior to the recognition of the disconformity. The two formations can also be distinguished by petrographic and sedimentologic differences.
Early-Mid Jurassic (170 Ma) They are part of the Perth Basin, and are a sequence of non-marine, probably fluvial sandstones, shales and silts including bituminous coal, and are up to 300 m thick. The Cattamarra Coal Measures conformably overly the Eneabba Formation. \- the summary to this thesis in Trove is a detailed overview The Cattamarra Coal Measures are a tight gas reservoir. There are well preserved fossil insects from the Jurassic age in the deposit.
The Wapiti Formation rests conformably on the marine shales of the Smoky Group. It is more than thick in the foothills of the Canadian Rockies in the west, and it thins eastward to its erosional edge. It is correlative with the entire sequence of the Belly River Group, Bearpaw Formation, Edmonton Group and Scollard Formation in south-central Alberta. In most areas it is unconformably overlain by glacial and post-glacial sediments of Quaternary age, or exposed at surface.
The oldest Tertiary formation in the graben is the O'Brien Creek Formation, which is up to thick, and composed tuffaceous rock with volcanic ash and rounded quartz grains. The top of this formation is characterized by an igneous-cemented conglomerate, conformably overlain by the Sanpoil Volcanics, which are about thick. Correlated with these volcanics is the Scatter Creek Rhyodacite, which is generally found along the fault zones defining the graben. Eocene and Oligocene ore deposits are found within the Republic mining district.
The Infrahelvetic complex consists of Mesozoic cover rocks, most notably massive limestones from the European continental shelf. These limestones have a shallower marine facies than contemporary sediments from the Helvetic nappes since they were originally deposited north of those units. The Triassic and Permian consist of dolomites, marls and conglomerates. In contrast to the completely detached Helvetic nappes, the Infrahelvetic complex is still lying conformably on top of a Hercynian basement which forms the external massifs of the Aar and Gotthard nappes.
Environment and Planning B 28 (1): 103–121. and is applied with the help of a fuzzy system with a Mamdami inference system based on fuzzy logic within any architectural space. Fuzzy architectural spatial analysis model analyses the space by considering the perceivable architectural element by their boundary and stress characteristics and intensity properties. The method is capable of taking all sensorial factors into account during analyses in conformably with the perception process of architectural space which is a multi-sensorial act.
The Arroyo del Agua Formation consists of siliclastic red beds with a total thickness of roughly . These lie conformably on the El Cobre Canyon Formation and are in turn overlain in most locations by the Shinarump Conglomerate. In a few locations in the southernmost Chama Basin, there is a tongue of De Chelly Sandstone between the Arroyo del Agua and Shinarump.Lucas and Krainer 2005 The formation is 58% siltstone and 34% sandstone, with minor conglomerate and calcrete (each about 4%).
The Subachoque Formation is the lowermost of the lagunal and alluvial sequence of the Bogotá savanna. In parts, it conformably overlies the Tilatá Formation and other parts unconformably the Cretaceous Guadalupe Group and the Paleogene Guaduas, Cacho, Bogotá, and Regadera Formations. The Subachoque Formation is overlain by other Quaternary deposits of Lake Humboldt. The age has been estimated to be Early to Middle Pleistocene based on fission track analysis, with reported ages between 2.5 and 1 Ma.Montoya & Reyes, 2005, p.
The Ecca Group is the second of the main subdivisions of the Karoo Supergroup of geological strata in southern Africa. It mainly follows conformably after the Dwyka Group in some sections, but in some localities overlying unconformably over much older basement rocks. It underlies the Beaufort Group in all known outcrops and exposures. Based on stratigraphic position, lithostratigraphic correlation, palynological analyses, and other means of geological dating, the Ecca Group ranges between Early to earliest Middle Permian (Asselian - Roadian) in age.
The Red River Formation lies unconformably on the Winnipeg, and consists of shallow marine carbonate, anhydrite, and salt sedimentation. Conformably overlying the Red River is the Ordovician Stony Mountain Formation and Stonewall Formation, followed by the Silurian Interlake Group. During the Devonian, the Williston Basin became the southeastern corner of the Elk Point Basin when the Elk Point Group, Manitoba Group, and Saskatchewan Group were deposited. The Bakken Formation, an organic-rich marine shale, was deposited in the Late Devonian.
The Whitehill Formation has been subdivided into two major subunits according to their weathering color in outcrops. The lower and thicker part consists mainly of bluish- to greenish-grey shales and mudstones, which grade upward into more light brownish, buff weathering, slightly coarser grained siltstones. This zone is conformably overlain by white weathering shales, with intermittent chert lenses and pyritic stringers; the latter rarely exceeding in thickness. The sedimentary structure is generally massive, however laminations do occur that resemble algal lamellae.
Climatic zones of the Carboniferous-Permian boundary The Cisularian Epoch contained two ages, the Wolfcampian and the Leonardian, both of which have a geological formation in the Permian Basin named after them. The Wolfcampian Formation lies conformably on top of the Pennsylvanian Formation and is the first formation from the Permian Period. Its composition varies depending on its location in the Basin, with the northernmost part being more rich in shale. The thickness of this formation also varies, reaching a maximum of .
The Nikanassin is roughly equivalent to the Kootenay Group of the southern Alberta foothills and the Minnes Group north of northeastern British Columbia. It conformably overlies and interfingers with the "Passage Beds" at the top of the Fernie Formation. A major period of regional erosion occurred after the deposition of the Nikanassin, removing some of the uppermost Nikanassin strata prior to the deposition of the overlying conglomerates of the Cadomin Formation. The contact between the two formations is thus sharp and unconformable.
The Kiskatinaw Formation is generally conformably overlain by the Taylor Flat Formation (with some exceptions in the Peace River and Fort St. John areas) and unconformably underlain by Golata Formation due to pre-Kiskatinaw erosion. Some Kiskatinaw channels cut down into the Debolt Formation in the eastern parts of its extents. The Kiskatinaw Formation is correlated with the upper Mattson Formation in the Liard area, with the upper Etherington Formation in southern Alberta and with the Otter Formation in Montana.
The sandstones within the Kitadani Formation are light gray and green and range in clast size from fine to coarse. The type section of the Kitadani Formation occurs along the Nakanomatadani branch of the Takinami River:ja:滝波川 near the city of Katsuyama, where it is approximately 100 m (~328 feet) in thickness. The Kitadani Formation conformably overlies the Akaiwa Formation and is unconformably overlain by the Omichidani Formation. The Kitadani Formation has had varying nomenclature throughout the history of its study.
The Glenogle Formation is present in the Kootenay Ranges of southeastern British Columbia and is not known to be present west of the Columbia River. It rests conformably on the McKay Group and is overlain, probably disconformably, by the Mount Wilson Formation. It is equivalent to the Owen Creek and Skoki Formations and the upper part of the Outram Formation in the eastern main ranges of the Canadian Rockies, and the upper part of the McKay Group in some parts of the western main ranges.
The corresponding unconformity, which exists only in the western Pyrenees, belongs to an early deformation phase of the Variscan orogeny (Breton Phase). Only in the western Pyrenees is the Lower Carboniferous (Mississippian) distinguished from the Devonian sediments by an unconformity, starting off marine with a transgressive quartz–pebble bed. Anywhere else, the Supragriotte limestones are conformably overlain by pre- orogenic sediments that begin with the Lower Cherts of the Tournaisian. The Lower Cherts comprise 50 m of black, phosphate nodule-bearing cherts interlayered with black shales.
The type section of the Emu Bay Shale crops out on the east side of Emu Bay where it conformably overlies the White Point Conglomerate. Here it yields a rich assemblage of Estaingia, Redlichia, hyolithids, brachiopods, and the scleritome-bearing Chancelloria. At the Big Gully locality (8 km east of White Point), its presumed correlative is unconformable on the White Point Conglomerate and yields soft-bodied fossils in addition to the trilobites, including two species of the giant predator Anomalocaris (A. briggsi and Anomalocaris cf.
The Nahanni Formation is conformably overlain by the Fort Simpson Formation in the west and by the Horn River Formation in the east. It overlays the Headless Formation diachronically and transitionally, with younger deposits occurring in the west. It is equivalent to the upper part of the Hume Formation in the Mackenzie River area, as well as the Lonely Bay Formation, Pine Point Formation and Little Buffalo Formation in the Great Slave Lake area. In northern Alberta it corresponds to the Keg River Formation.
Sriperumbudur belongs to the Sriperumbudur Formation, which is characterised by arenaceous and argillaceous rock units composed of splintery green shale, clays, and sandstones with ironstone intercalation. The rock units conformably"(of rock strata) lying in a parallel arrangement so that their original relative positions have remained undisturbed" overlie either the Precambrian basement or Precambrian boulder beds and green shales. The beds contain marine intercalations. Their lithologic suites and fossil fauna are suggestive of deposition under shallow and brackish conditions, probably close to the shoreline.
The remaining members are the Bonney Canyon Member, a relatively thin section of thin-bedded limestone with local gypsum beds, and the upper Fourmile Draw Member, which is primarily marine carbonates. The Fourmile Draw grades into the Brushy Canyon and Cherry Canyon Formations in the Delaware Basin and contains considerable gypsum in the Guadalupe Mountains. The entire San Andres Formation tends to become more dolomitic to the north. The formation is conformably overlain by the Grayburg Formation or, where this is not present, unconformably by Triassic units.
The Pennsylvanian Period also led to the development of other geologic formations, although none had the importance of the Morrow Formation. The Atoka Formation lies conformably on top of the Morrow Formation, and is characterized by its fossil-rich limestone inter- bedded with shale, reaching a max thickness of . During the formation of the Atoka, uplift was still occurring in the region, leading to increased sedimentation as the surrounding highlands were eroded. The increased sedimentation led to the formation of medium- to coarse-grained sandstone.
The Cadomin Formation overlies a major regional unconformity caused by pre-Cadomin erosion, although little or no evidence of the angular nature of that unconformity is apparent at most outcrops. It rests unconformably on the Fernie Formation, the Nikanassin Formation, the Minnes Group or the Kootenay Group, depending on the location and the extent of the erosion. It is conformably overlain by the Gladstone Formation in Alberta and Gething Formation in northeastern British Columbia, and it is equivalent to the base of the Mannville Group.
In central Alberta the Leduc Formation conformably overlies the platform limestones and dolomites of the Cooking Lake and Beaverhill Lake Formations. In northern Alberta near the Peace River Arch it rests on older red beds or on the Granite Wash. The Leduc reefs are surrounded by shales of the Duvernay and Ireton Formations and the Woodbend Group that were deposited in non-reefal, open marine environments. The Leduc reefs are the same ages as, but not contiguous with, the reefs of the Cairn Formation farther west.
The Beaverfoot Formation is present in the western ranges of the Rocky Mountains of British Columbia and forms cliffs along the eastern wall of the Rocky Mountain Trench. It is also present in the Purcell Range west of Radium, British Columbia, and in the main ranges of the Alberta Rockies between the Clearwater and North Saskatchewan Rivers. It disconformably overlies the Mount Wilson Formation or older rocks. It is conformably overlain by the Tegart Formation in the western ranges, and unconformably overlain by the Late Devonian Cairn Formation to the east in Alberta.
The lowermost lithofacies corresponds to the stratigraphic level of El Espinal quarry, defined by Steele and Waite (1986) as dolomite and dolomitic breccia, located between from the base of the formation, which rests conformably on top of the Late Jurassic to Early Cretaceous San Ricardo Formation. The top is covered unconformably by the Campanian to Maastrichtian Ocozocoautla Formation. The depositional environment is described as an environment with high oxygen concentration and high primary productivity with sporadic influence of strong waves and/or currents in a brackish marginal marine environment; shallow lagoon or estuary.
The Liard Formation overlies the Toad Formation, and the contact is conformable in most areas. It is conformably overlain by the Charlie Lake Formation in the southern part of its extent. To the north in the Liard River area, it is unconformably overlain by the Garbutt Formation and Buckinghorse Formation. It is laterally equivalent to the Halfway Formation in the subsurface of the Peace River plains, and to the upper part of the Llama Member of the Sulphur Mountain Formation in the southern Canadian Rockies and their foothills.
Since the Middle Ages the pope is the judge of first instance in all more important episcopal causes (), the number and extent of which are in no way exactly definable, but to which above all belong the —more serious criminal charges against bishops() Conformably to this the diocesan bishop or his representative (the vicar-general, or , or some other diocesan authority) became the judge of the court of first instance, so far as common law has not withdrawn from him this jurisdiction.(Council of Trent, Sess. XXIV, De ref., c.
The formation was named by Garrido in 2010 as sandy unit conformably and transitionally overlying the Los Bastos Formation, which in turns overlies the Portezuelo Formation within which both units were formerly included. The formation in the same manner underlies the Plottier Formation, all belonging to the Río Neuquén Subgroup of the Neuquén Group in the Neuquén Basin. The unit now known as Sierra Barrosa Formation was included in the original definition by Herrero Ducloux (1938, 1939) as "Portezuelo Superior", as part of the "Portezuelo Beds" he described.Garrido, 2011, p.
The Hayang Group consists of Chilgok, Silla, Hakbong, Haman, Banyawol, Songnaedong, Chaeyaksan and Geoncheonri Formations in ascending order. The Geoncheonri Formation is conformably underlain by the Chaeyaksan Formation and overlain by the Jusasan Formation, the lowermost of the Yucheon Group. Since plant fossils were first reported in the Geoncheonri Formation in 1925, a series of paleontological studies has been made with molluscs, spores and pollen, charophytes, and dinosaur footprints. Plant fossils from the Geoncheonri Formation were correlated with the Monobegawa Group and the Gyliak Series (Lower to "Middle" Cretaceous) in Japan.
The Passaic is Late Triassic with an astronomically calibrated age of 219 to 201.7 million years ago (Ma) and is about 13,000 ft (~4 km) thick in the basin depocenter. It conformably overlies the Lockaton Formation (darker, generally gray shales and mudrocks) and is overlain by the first Watching(Orange Mountain Formation) basalt. The Triassic/Jurassic boundary and correlated by pollen is located in the uppermost part of the formation, ~ 2 precessional cycles (~10-12 m) below the Orange Mountain Basalt. There are numerous diabase intrusions into the Passaic with local contact metamorphic rocks.
The McMurray Formation is conformably overlain by the Wabiskaw Member of the Clearwater Formation. It is underlain by Devonian formations that were tilted and eroded prior to the deposition of the McMurray, resulting in a shallow angular unconformity between the McMurray and the underlying units. The McMurray therefore rests on different Devonian units in different parts of the basin. These range from the Elk Point Group in the east near the Saskatchewan border, to the Waterways Formation along the Athabasca River, and the Banff, Wabamun, and Winterburn Formations farther west.
The Wabamun Formation is disconformably overlain by the Exshaw Formation in southern Alberta, by the Blairmore Group in western Alberta and by the Mannville Group in eastern Alberta. It rests conformably on the Graminia Formation siltstone of the Winterburn Group. In the Calgary area, the formation is divided into a lower and an upper part separated by the porous dolomitic Crossfield Member. It is equivalent to the Three Forks Formation in Montana, the Palliser Formation in the Canadian Rockies, the sum of the Kotcho Formation and Tetcho Formation in northeastern British Columbia.
The Fort Simpson Formation is overlain by the Jean Marie Member of the Redknife Formation in its eastern reaches, and progressively by the Kakisa Formation, Trout River Formation or Tetcho Formation towards the west. It is conformably underlain by the Muskwa Member of the Horn River Formation. It is replaced by the Besa River Formation in the Liard River area. It is equivalent to the Imperial Formation to the north, the Tathlina Formation, Twin Falls Formation and Hay River Formation to the east, and the Woodbend Group in Alberta.
Boulder of the conglomerate along Crone Road near the top of the Conewago Mountains (rock hammer for scale) The Gettysburg Formation is conformably underlain by the New Oxford Formation, which is the basal unit of the Newark Supergroup in south-central Pennsylvania. The Gettysburg is mapped from the Maryland border through Adams, Cumberland, Lancaster, and York Counties to the southern borders of Dauphin and Lebanon Counties. In these counties and to the north the rock unit is called the Hammer Creek Formation. The Gettysburg Formation is divided into several members.
The Hammer Creek Formation is conformably underlain by the New Oxford Formation, which is the basal unit of the Newark Supergroup in south-central Pennsylvania. The Hammer Creek is mapped from the southern borders of Dauphin and Lebanon Counties to the northeast to the Schuylkill River. A laterally equivalent rock unit called the Brunswick Formation is mapped on the east side of the river and into New Jersey.Van Houten, F.B., 1980, Late Triassic part of Newark Supergroup, Delaware River section, west-central New Jersey, IN Manspeizer, Warren, ed.
The Joli Fou Formation is the basal (oldest) formation of the Colorado Group. It is overlain by the Viking Formation (disconformably in south-eastern Saskatchewan) and conformably underlain by the upper Mannville Group (Grand Rapids Formation in north-eastern Alberta, Pelican Formation in southern Alberta). It is equivalent to the lower Ashville Formation in southern Manitoba, the Skull Creek Shale in North Dakota and parts of the Blackleaf Formation in northern Montana. In south-eastern Alberta, the base of the Formation contains the Cessford Sand marker, consisting of sandstone, siltstone and mudstone.
Organized alphabetically, its content does indeed contain explanation not merely of the terms used in the arts and sciences, but of the arts and sciences themselves. Sir Isaac Newton contributed his only published work on chemistry to the second volume of 1710. Its emphasis was on science—and conformably to the broad 18th-century understanding of the term 'science', its content extends beyond what would be called science or technology today, and includes topics from the humanities and fine arts, e.g. a substantial number from law, commerce, music, and heraldry.
The formation consists of highly fossiliferous nodular argillaceous limestone at its base and in its upper portion, with shale dominating the middle section and interbedding with the limestone towards the top of the formation. Total thickness is . The formation conformably overlies the Smeltertown Formation and grades into the overlying Mesilla Valley Formation. The formation is interpreted as an outer shelf formation that later experienced shallowing and deposition of limestone in an inner shelf environment subject to storm influence, then deepened again to deposit shale with some storm layers.
There is also a shale horizon called the Ban Na Shale, interbedded with Ordovician limestone. The presence of shale suggests a deeper water environment in the Silurian. The Thong Pha Phum Group conformably overlies the Thung Song Group in the west with a thick sequence of non-fossil bearing clastic marine sedimentary rocks that likely deposited in a forearc basin. Volcanic activity was common in the Devonian and Carboniferous as limestone accumulated on a western facing continental margin (exposures of these rocks are visible at Petchabun-Loei in east-central Thailand).
For instance, coarser grained sediments such as sand may be deposited at angles of up to 15 degrees, held up by the internal friction between grains which prevents them slumping to a lower angle without additional reworking or effort. This is known as the angle of repose, and a prime example is the surface of sand dunes. Similarly, sediments may drape over a pre-existing inclined surface: these sediments are usually deposited conformably to the pre-existing surface. Also sedimentary beds may pinch out along strike, implying that slight angles existed during their deposition.
The formation lies conformably on the prolifically- fossiliferous shallow marine sandstone, siltstone and mudrock of the Staithes Formation. There are six named ironstone seams which are, in order of deposition, the Osmotherley, Avicula,The bivalve Avicula has since been reclassified as the genus Oxytoma. Raisdale, Two-foot, Pecten and Main Seams. At its type locality, on the coast around Staithes, North Yorkshire, the formation attains a thickness of 25.3 metres and comprises five 'coarsening- upward' cycles of marine shale and siltstone each capped by a seam of ironstone of varying thickness, composition and iron-content.
Rocks in the area are limestones and dolomites from the Ordovician Period, which implies deposition about 470 million years ago. The carbonates of the Natural Bridge occur within the Chepultepec Formation, making the buttress of the bridge, and the Beekmantown Formation, deposited conformably over the Chepultepec and comprising the span and the upper part of the bridge.Spencer, Edgard W. ,1968, Geology of the Natural Bridge, Sugarloaf Mountain, Buchanan, and Arnold Valley quadrangles, Virginia: Report of Investigations 13, Virginia Division of Mineral Resources, Charlottesville, VA, 55 p. and 4 plates.
It is dominated by mudrock that accumulated in offshore and marine environments of the Cretaceous North American Inland Sea. The Mancos was deposited during the Cenomanian (locally Albian) through Campanian ages, approximately from 95 Ma to 80 Ma. Stratigraphically the Mancos Shale fills the interval between the Dakota Group and the Mesaverde Formation Group.Weimer, R. J. (1960) "Upper Cretaceous Stratigraphy, Rocky Mountain Area" American Association of Petroleum Geologists Bulletin 44: pp. 1-20 The Mancos Shale rests conformably on the Dakota and in its upper part grades into and intertongues with the Mesaverde Group.
The Yaquina Formation represents a coastal marine depositional environment, and is considered late late Oligocene in age (Chattian) based on foraminifera and mollusc stages; approximately 24-25 million years in age. A. weltoni is also known from the Yaquina Formation and occurs along the same cliff face as A. cotylalveus, but occurs higher in the stratigraphic section. This specimen was found in situ near the contact of the conformably overlying Nye Formation, which is Miocene in age. Thus, A. weltoni is very close to the Oligocene-Miocene boundary.
Kaskapau shale exposed along the Pouce Coupe River The formation is thick in the Peace River and Smoky River area, and thickens up to in the foothills of the Northern Rocky Mountains in British Columbia. It is exposed along the Peace River near Dunvegan, as well as in the Smoky River area. The formation is part of the Smoky River Group, and is conformably overlain by the Bad Heart Formation in the western area, and unconformably by the Cardium Formation in the Pouce Coupe River area. It is conformable underlain by the Dunvegan Formation.
The Sulphur Mountain Formation is laterally equivalent to Montney, Doig, and Halfway Formations in the subsurface beneath the plains of Alberta and northeastern British Columbia, and to the Toad, Grayling, and Liard Formations in the foothills of northeastern British Columbia. It unconformably overlies the Permian Ishbel Group or, in some areas, the Mississippian Rundle Group. It is conformably overlain by the Whitehorse Formation in the southern part of its extent and by the laterally equivalent Charlie Lake Formation in the north. In areas where those formations were removed by erosion it is unconformably overlain by the Jurassic Fernie Formation.
The Bohío Formation is characterized by the presence of poorly sorted debris, mostly basaltic: very coarse debris in the form of boulders and cobbles, and finer debris forming beds of sandstone, and the matrix of conglomerate. The facies are non-marine, but marine fossils are found in thin units in the upper part of the formation, in algal limestone and in both poorly sorted and fairly well sorted subgraywacke. The Bohío Formation overlies the Gatuncillo Formation conformably in most areas, although may lap onto the Gatuncillo Formation or basement. The thickness of the formation is about .
The Sleat Group, which outcrops on the Sleat peninsula on Skye, underlies the Torridon Group conformably, but the relationship with the Stoer Group is nowhere exposed. It is presumed to have been in deposited later that the Stoer Group, but possibly in a separate sub-basin. It is metamorphosed to greenschist facies and sits within the Kishorn Nappe, part of the Caledonian thrust belt, making its exact relationship to the other outcrops difficult to assess. The sequence consists of mainly coarse-grained feldspathic sandstones deposited in a fluvial environment with some less common grey shales, probably deposited in a lacustrine environment.
To the northwest of the Santander Massif, the formation overlies the Bocas Formation and is unconformably overlain by the Tablazo Formation. In some locations in this area, the formation is found in faulted contact with the Bucaramanga Gneiss, La Virgen Formation and the Tablazo and La Luna Formations. In the Serranía de San Lucas, the Noreán Formation conformably overlies the Morrocoyal Formation and in this area is overlain by the Tablazo Formation and the Arenal Conglomeratic Unit. Across the San Lucas mountains, the formation is in faulted and discordant contact with the Norosí Batholith, the San Lucas Gneiss and the Sudán Formation.
Studies by Frey, Watts, and Whitehead have also documented that the sediments filling Carolina bays are generally undisturbed. Several cores have found that the sediments that fill Carolina bays have distinct and conformably layers or beds. The dating of the sand rims of a number of Carolina bays by optically stimulated luminescence (OSL) techniques has yielded ages ranging from ~109,000 to ~2,000 years ago, but most ages from the sand rims range from ~40,000 to ~11,000 years ago.Savannah River Archaeological Research Program Staff (2010) Annual review of Cultural Resource Investigations by Savannah River Archaeological Research Program.
In the north and northwest wall of the Valles caldera, the Paliza Canyon Formation appears to be conformably overlain with dacite and quartz latite flows of the Tschicoma Formation (Polvadera Group). However, the alteration of the Paliza Canyon beds in contrast with the fresh appearance of the Tschicoma beds suggests a disconformity between the formations. The Paliza Canyon Formation is also locally overlain unconformably by the Bandelier Tuff. Beds assigned to the Basalt of Chamisa Mesa have since been found to be unremarkable in age and composition and are now assigned to the Paliza Canyon Formation.
Megaripples in the quartz arenites of the Random Formation The formation is difficult to date, but is considered Precambrian, as it lies unconformably under the Bonavista Formation and conformably above Ediacaran strata. It does sit above the Chapel Island Formation on the Burin peninsula meaning that, at that location, the lower boundary is in the Lower Cambrian. Inarticulate brachiopods have been found in its upper strata, dating these to the late early or even early mid Cambrian. However, it is likely that the unit is diachronous and may date into the Ediacaran further to the east.
Several thin layers of bentonite occur within the unit, and the unit is capped by one as well, which forms the base of the conformably overlying Monterey Formation. North of the Santa Ynez River, the Rincon is typically capped not by the Monterey but by the Temblor Formation, a sandstone similar to the underlying Vaqueros; additionally, north of the river the Rincon Formation grades into this sandstone to the east.Dibblee (1966), 43 Northeast of Blue Canyon and the Little Pine Fault, in the backcountry of easternmost Santa Barbara County and Ventura County, the Rincon Formation disappears, and the Temblor Formation rests unconformably on the much older Cozy Dell Shale.
Entrada Sandstone conformably overlies the Carmel Formation, Park Avenue, Arches National Park The Entrada Sandstone is a formation in the San Rafael Group found in the U.S. states of Wyoming, Colorado, northwest New Mexico, northeast Arizona, and southeast Utah. Part of the Colorado Plateau, this formation was deposited during the Jurassic period sometime between 180 and 140 million years ago in various environments, including tidal mudflats, beaches, and sand dunes. The Middle Jurassic San Rafael Group was dominantly deposited as ergs (sand seas) in a desert environment around the shallow Sundance Sea.The formation of the Entrada Sandstone: Tectonics, Accommodation space, Wind and lots of Sand.
The Laramie Formation is exposed around the edges of the Denver Basin and ranges from 400–500 feet (120–150 m) on the western side of the basin, and 200–300 feet (60–90 m) thick on the eastern side. It rests conformably on the Fox Hills Sandstone and unconformably underlies the Arapahoe Conglomerate. The formation can be divided into an unnamed lower member containing bedded sandstone, clay and coal; and an unnamed upper member composed predominately of 90 to 190 m of drab-colored mudstone, some sandstone, and thin coal beds.Eldridge, G.H., 1888, On some stratigraphical and structural features of the country about Denver, Colorado: Colorado.
These Constitutions were observed until the Revolution, but when the various houses re-opened, the bishops of the different dioceses modified them according to their own views. In 1898, upon request of the religious of Tours, the original Constitutions, revised conformably to the new regulations of the Church for religious institutes, were definitively approved by Leo XIII,The Catholic Church in America, Vol.II, Catholic Editing Company, 1914 and their branch erected as a generalate. In 1902 the words "Of the Blessed Virgin", were added to the title to distinguish the non-cloistered daughters of Anne de Xainctonge from the cloistered daughters of St. Angela.
The congregation was established by Pope Sixtus V. It also communicated instructions to the legates of the Holy See for the maintenance of due decorum in transacting the affairs of their missions. This congregation also instructed the members of the Noble Guard and the ablegate who were sent to convey to new cardinals, living in Catholic states outside of Rome, the news of their promotion, together with the cardinal's hat and the red biretta. It instructed newly promoted cardinals, too, on the etiquette to be followed conformably with their new dignity. Finally, it solved the questions of precedence which arose among cardinals or among ambassadors to the Holy See.
The Doig Formation is unconformably overlain by the Halfway Formation of the Schooler Creek Group; the contact is marked by a dolomitic bed and a chert and quartz conglomerate bed. To the west it is overlain by younger Jurassic beds. It conformably overlies the Montney Formation and the contact is marked by a phosphate pellet bed in the base of the Doig. The formation correlates with the lower Llama Member of the Sulphur Mountain Formation in the southern ranges of the Canadian Rockies, with the Whistler Member of the Whitehorse Formation in the Muskwa Ranges, and with the Toad Formation in the upper Liard River area.
The Alberta Group is conformably overlain by the Belly River Formation and rests unconformably on deposits of the Blairmore Group and Luscar Group in the Canadian Rockies foothills and on the volcanic Crowsnest Formation in southern Alberta's west. The group is equivalent with the Colorado Group and Lea Park Formation in southern Alberta's prairies, and with the Smoky Group in northern Alberta and north-east British Columbia. The Wapiabi Formation is equivalent to the upper Colorado Group shales and Lea Park Formation in central Alberta and the sum of Puskwaskau Formation, Bad Heart Formation and Muskiki Formation in the west part of northern Alberta.
" To Price, that, and the lack of any evidence of erosion between the strata, implied that little time could have occurred between the two layers of rock. Price also discovered in the literature examples of similar conformable strata, but in the reverse order, the old rocks on top and the young strata below according to interpretation of the fossils. Although appearing "to succeed one another conformably" the Canadian Geologic Survey contended for over-thrusting principally based on the fossil content. Price's interpretation of the evidence was that "the geological record does not prove succession of ages, but rather shows a "taxonomic" series representing different but contemporaneous zones of antediluvian life.
The Besa River Formation is conformably overlain by the Prophet Formation or Banff Formation in its eastern extent, while to the west it is overlain by the Mattson Formation and Stoddart Group, and abruptly overlays the Dunedin Formation in the west of its extent in British Columbia, and the Slave Point Formation in the east. In the Northwest Territories, it rests on the Nahanni Formation in the east and the Road River Formation in the west. Towards the southwest, it passes laterally into the Fort Simpson Formation and Exshaw Formation. To the south, it passes into the Dunedin Formation, Horn River Formation and Exshaw Formation.
It is exposed in the San Rafael Reef, the Waterpocket Fold, in the Henry Mountains, with additional exposures scattered across the region from the San Rafael Reef to the Paradox Basin, and in north-central New Mexico. The thin bedding is characteristic throughout the formation, but gypsum is not found in the San Juan Basin and some conglomerate is found on the south and southwestern margins of the formation.Lucas and Anderson 1992, p.81 The formation rests conformably on the underlying Curtis Formation (Utah and western Colorado) or Todilto Formation (southwest Colorado and New Mexico) but is separated from the overlying Morrison Formation by the regional J5 unconformity.
The Elk Point Group is conformably overlain by the Manitoba Group in Manitoba and Saskatchewan, and by the Beaverhill Lake Group in Alberta. It rests unconformably on Precambrian basement rocks in northern Alberta, on Cambrian strata in northeastern Alberta and in Saskatchewan, and on Ordovician to Silurian formations in western Alberta, Saskatchewan and southwestern Manitoba. In the Northwest Territories, some of its uppermost units are exposed at surface or are unconformably overlain by Cretaceous strata. The Lower Elk Point Group is equivalent to the Stone Formation and its equivalents, and the Headless and Nahanni Formations, in northerneastern British Columbia and the southwestern Northwest Territories.
In Ancient Roman civil law, acceptilatio is defined to be a release by mutual interrogation between debtor and creditor, by which each party is exonerated from the same contract. In other words, acceptilatio is the form of words by which a creditor releases his debtor from a debt or obligation, and acknowledges he has received that which in fact he has not received (veluti imaginaria solutio). It is equivalent to the modern acceptilation. This release of debt by acceptilatio applies only to such debts as have been contracted by stipulatio, conformably to a rule of Roman law, that only contracts made by words can be ended by words.
A debate has arise of whether the Dagshai Formation overlies conformably or unconformably on top of the Subathu formation. recent research by dating detrital micas and fission track dating of detrital zircons shows conclusively that there is an unconformable nature between the Subathu and Dagshai Formation. Magnetostratigraphic data suggests that the Daghsai formation was deposited at approximately 27 Ma with 2 Ma uncertainty. Previously, multiple studies of facies interpretation of the Dagshai formation has been conducted with varying results regarding the past depositional environment; the presence of quartzitic sandstones was thought to be leftovers of an extensive and prolonged weathering in alluvial plains in which time tropical weathering was intensifying.
The Miners Delight formation which hosts several epigenetic shear zone and vein gold deposits is subdivided into several lithologic units, the relative ages of which are not known. The Roundtop Mountain Greenstone is predominantly greenstone, greenschist, and amphibolite, but also includes mica schist, hornblende-mica schist, and metabasalt, accompanied by minor metagreywacke, metatuff, chlorite schist, tremolite-actinolite schist and rare grunerite schist. The unit is exposed on both limbs of the South Pass synclinorium, and in most places conformably, but locally unconformably, overlies the Goldman Meadows Formation. Much of the unit is composed of metamorphosed pillow basalts and cusp-shaped pillow structures are preserved on Roundtop Mountain.
Cambrian rocks of Araba and Naqus Formations occur throughout the region above a planar unconformity, a result of peneplaination. These red and white sandstone units have a combined thickness of about 500 m. They were deposited in a continental environment except in the northeastern part of the gulf where they become marine. The next preserved sequence is the Umm Bogma or Abu Durba Formations of lower Carboniferous age, which sit apparently conformably on the Cambrian, although the base represents a hiatus of about 150 Ma. The Umm Bogma Formation is dolomitic, while the stratigraphically equivalent Abur Durba Formation consists of black shales and mudstones.
These examples showed de Moivre using his hypothesis in a piecewise fashion, wherein he assumed that the overall pattern of human mortality could be approximated by several straight- line segments (see his illustration to the right). He wrote that "since the Decrements of Life may without any sensible Error be supposed equal, for any short Interval of Time, it follows that if the whole Extent of Life be divided into several shorter Intervals, ... , the Values of Annuities for Life ... may easily be calculated ... conformably to any Table of Observations, and for any Rate of Interest".page 24 of Annuities upon Lives. Italics and capitalization per original.
After absolution from excommunication has been given, the judge sends the person absolved to a confessor, that his sin may be remitted; when absolution from censure is given in the confessional, it should always precede sacramental absolution, conformably to the instruction in the Ritual and the very tenor of the formula for sacramental absolution. It may be noted at once that the principal effect. of absolution from excommunication may be acquired without the excommunicated person's being wholly reinstated in his former position. Thus, an ecclesiastic might not necessarily recover the benefice which he had lost; indeed he might be admitted to lay communion only.
Brown then applied to the Superior Court of Quebec for an order of mandamus compelling the church officials to provide a burial for her husband in the Côte des Neiges Cemetery. The pleadings filed by both sides were complex, with several supplemental pleadings from both sides. Brown sought to have Guibord's remains buried in the Roman Catholic portion of the cemetery, "conformably to custom and law," and argued that her husband had been a practising Roman Catholic at the time of his death, filing his baptismal certificate and their wedding certificate.pp. 161-162. (L.R.) The church officials challenged the availability of the remedy of mandamus, as well as denying that they had refused civil burial to Guibord.
6 km thick. The non-marine ORS is conformably succeeded by latest Devonian coastal plain and shallow marine clastic deposits (the Toe Head Sandstone and Old Head Sandstone Formations, and equivalents), followed by shallow to deeper marine Carboniferous sandstones, mudstones and limestones of the South Munster Basin.MacCarthy, I.A.J. (1987) Transgressive facies in the South Munster Basin, Ireland. Sedimentology, 34, 389-422 During the Late Palaeozoic Variscan (or Hercynian) orogeny the deposits in the basin were subjected to compressional deformation that resulted in pressure solution cleavage formation, buckle folding and contractional faultingCooper, M.A., Collins, D., Ford, M., Murphy, F.X. & Trayner, P.M. (1984) Structural style, shortening estimates and the thrust front of the Irish Variscides.
The formation was named by Garrido in 2010 as shaly unit conformably and transitionally overlying the Portezuelo Formation, to which the layers were formerly defined and in the same manner underlying the Sierra Barrosa Formation, all belonging to the Río Neuquén Subgroup of the Neuquén Group in the Neuquén Basin. The unit now known as Los Bastos Formation was included in the original definition by Herrero Ducloux (1938, 1939) as "Portezuelo Medio", as part of the "Portezuelo Beds" he described.Garrido, 2011, p.236 The type locality of the formation is located at the foot of the outcrop of the eponymous Los Bastos Field, between the localities of Sierra Barrosa and Cerro Senillosa.
The fossilized leaf of Sabalites, a Cretaceous palm, documents the wet, warm climate that prevailed in Late Cretaceous New Mexico Titanoceratops is known from OMNH 10165, a skeleton from the lowermost Fruitland or uppermost Kirtland Formation. The Fruitland Formation is about thick, and consists of sandstones, mudstones, and abundant coals deposited in a coastal floodplain. Fossil trees are abundant in the area from which the holotype was collected, suggesting a wet, well-forested environment. A fossil tree stump from the Coal Creek area where Titanoceratops was found, showing the extensive coal beds of the area The Kirtland Formation, which conformably overlays the Fruitland, is approximately thick, and made up of sandstone, siltstone, mudstone, and shale.
The type locality for the Coldwater Sandstone is in Coldwater Canyon, a western branch of the Sespe River a few miles north of Fillmore. The unit is typically around half a mile thick, ranging from 2,500 to 3,200 feet through most of its extent, although it thins westward to around 1,000 feet thick in the hills north of El Capitan State Beach. From there going west to Gaviota, the unit gradually grades into the Sacate Formation, a similar but shalier and more siltstone-rich unit which is also conformably overlain on the Cozy Dell Formation. The Coldwater and Sacate Formations are sometimes considered as a single unit, particularly underneath the Santa Barbara Channel where they appear in drill cores.
Without referral to an aether, this physical interpretation of relativistic effects was shared by Kennedy and Thorndike in 1932 as they concluded that the interferometer's arm contracts and also the frequency of its light source "very nearly" varies in the way required by relativity.They commented in a footnote: "From [the Michelson–Morley] experiment it is not inferred that the velocity of the earth is but a few kilometers per second, but rather that the dimensions of the apparatus vary very nearly as required by relativity. From the present experiment we similarly infer that the frequency of light varies conformably to the theory." Similarly the Sagnac effect, observed by G. Sagnac in 1913, was immediately seen to be fully consistent with special relativity.
The Nemunas Formation is the oldest Mesozoic formation, from the Triassic, overlying Permian, Carboniferous, Neoproterozoic and Devonian rocks with clay, argillite, marl and siltstone up to 131 meters thick. It is conformably overlain by the clay, argillite and sandstones of the Palanga Formation up to 776 meters thick, the 54 meter Taurage Formation oolitic limestones, marl and clay, and the reddish clays with sandstone-siltstone layers of the Sarkuva Formation. The Upper Triassic is marked by the Nida Formation, which lies disconformably on older Triassic rocks with 15 meters of sandstone, siltstone and clay. Basal conglomerate marks the beginning of the Lower Jurassic Neringa Formation with 33 meters of sandstone and clay, with the 45 meter siltstones, clay and sandstone of the Lave Formation.
The Franciscans, unlike the Dominicans, Carmelites and other orders, have never had a peculiar rite properly so called, but conformably to the mind of St. Francis of Assisi always followed the Roman Rite for the celebration of Mass. However, the Friars Minor and the Capuchins wear the amice, instead of the biretta, over the head, and are accustomed to say Mass with their feet uncovered, save only by sandals. They also enjoy certain privileges in regard to the time and place of celebrating Mass, and the Missale Romano-Seraphicum contains many proper Masses not found in the Roman Missal. These are mostly feasts of Franciscan saints and blessed, which are not celebrated throughout the Church, or other feasts having a peculiar connexion with the order, e.g.
The U20 side progressed conformably beating Stirling University 4-0 at Forthbank Stadium with Josh Jeffries scoring a brace. A second round tie with Scottish League One side Stenhousemuir was set-up, again played at Forthbank, however, the side could not match its previous performance and went down 3-1 with Ryan Hardie netting the Rangers goal. Rangers fan groups Rangers Supporters' Trust, Rangers Supporters Assembly and Rangers First merged to form Club 1872 in late May, and two-weeks later it announced that the new organisation had purchased enough shares to make it the sixth largest shareholder in RIFC. Harmony did not last for long amongst the support, however, as three directors of the Rangers First resigned from the organisation over a row regarding its governance, with Rangers First now the shareholding vehicle for Club 1872.
Yannai was prominent both as halakhist and aggadist. His name is mentioned in the Babylonian Talmud 176 times, and in the Jerusalem Talmud 254 times. He shared Hiyya's opinion regarding to the Mishnah; he granted it no greater authority than to the collections of halakhot or baraitot compiled by Hiyya and other disciples of Judah haNasi.Compare Yerushalmi Pesachim 1:5; Yerushalmi Yoma 4:2 When his pupil R. Johanan remarked that the Mishnah rendered a decision different from his, he answered, "The Mishnah gives only the decision of a single tanna, while I decide conformably to the Rabbis as a whole".Shabbat 140a He was independent in his decisions, and sometimes had all his contemporaries against him.Yerushalmi Niddah 3:4; Shabbat 65a His decisions were generally rigid regarding individuals,Yerushalmi Berachot 2:6; Yerushalmi Ketuvot 1:10; Shabbat 14a but liberal when the whole community was concerned.
The Edmonton Group is disconformably overlain by the Paskapoo Formation and conformably overlies the Bearpaw Formation or, where the Bearpaw is absent, the Belly River Formation. The Edmonton Group grades into the sequence of the Blood Reserve Formation, St. Mary River Formation and Willow Creek Formation in the southern Alberta plains; into the upper part of the Wapiti Group in the northern Alberta and northeastern British Columbia; and into the upper part of the Brazeau Formation and the Coalspur Formation in the foothills of the Canadian Rockies. It is equivalent to, but not contiguous with, the Eastend Formation, Whitemud Formation, Battle Formation and Frenchman Formation in the Cypress Hills of southeastern Alberta and southwestern Saskatchewan; and with the Fox Hills Formation in Saskatchewan. Formations that are stratigraphically equivalent in the western United States are the Horsethief Formation in Montana; the Fox Hills Formation and Lace Formation in Montana; and the Lennup Formation and Muteetse Formation in Wyoming.
Meltyukhov 2000:379-80 This fact and the absence of a connection between a possible strike by the enemy and the actions of the Red Army makes the suggestion of a 'counter-strike strategy' very implausible to Meltyukhov.Meltyukhov 2000:413 On the other hand, the concentration of Red Army on the borders was elaborated throughout different plans (Meltyukhov reports five different versions) and went through substantial changes. As also indicated by M. A. Gareyev, who is himself skeptical of the Soviet strike thesis, "the direction of the concentration of basic efforts by Soviet command was chosen not in the interests of the strategic defensive operation (this operation was simply not provided and was not planned), and conformably entirely to other methods of operations." Meltyukhov 2000:381 Military actions would have begun with the surprise blow by the Soviet Air Force on the airfields of Eastern Prussia, Poland and Romania. The overall Soviet superiority in aviation would have made it possible to subject German airfields in a 250 km-deep border zone to continuous airstrikes, which would have led to a significant weakening of the enemy and would have facilitated Red Army ground forces operations.
About four months later Alvarez presented their joint product under the title "Apologetica fratrum prædicatorum in provinciâ Hispaniæ sacræ theologiæ professorum, adversus novas quasdam assertiones cujusdam doctoris Ludovici Molinæ nuncupati", published at Madrid, 20 November 1595. [...] Nearly two years later, 28 October 1597, Báñez resumed the case in a new summary and petitioned the pope to permit the Dominican schools to take up their teaching again on the disputed questions. This was the Libellus supplex Clementi VIII oblatus pro impetrandâ immunitate a lege silentii utrique litigantium parti impositâ, published at Salamanca. An answer to the "Libellus" was conveyed in a letter of Cardinal Madruzzi, 25 February 1598, written in the name of the pope, to the nuncio in Spain: :Inform the Fathers of the Order of Preachers that His Holiness, moderating the prohibition that was made, grants them the faculty freely to teach and discuss, as they did in the past, the subject-matter de auxiliis divinae gratia, et eorum efficaciâ, conformably to the doctrine of St. Thomas; and likewise the Fathers of the Society, that they also may teach and discuss the same subject-matter, always holding, however, to sound Catholic doctrine.

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