Synonymer & Informasjon om | Engelsk ordet CONFORMABLY

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Eksempler på bruk av CONFORMABLY i en setning

• 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.
• The Wrekin Quartzite lies unconformably on Uriconian volcanics and is itself conformably overlain at the Ercall by the sandstones of the Lower Comley Sandstone Formation.
• Gingin Chalk (Kcg) is a weakly consolidated fossiliferous chalk composed of coccoliths, which interfingers and conformably overlies the Molecap Greensand.
• At its base, the Anacleto Formation conformably overlies the Bajo de la Carpa Formation, also of the Río Colorado Subgroup, and it is in turn unconformably overlain by the Allen Formation of the younger Malargüe Group.
• It rests unconformably above the Martinsburg Formation and conformably below the Bloomsburg Formation.
• It rests conformably on the Fox Hills Sandstone and unconformably underlies the Arapahoe Conglomerate.
• It conformably overlies the Lockatong Formation (darker, generally gray shales and mudrocks) and is overlain by the first Watching(Orange Mountain Formation) basalt.
• The Cloverly Formation rests disconformably on the Morrison Formation and is conformably overlain by the Thermopolis Shale.
• 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.
• 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 conformably overlies and interfingers with the "Passage Beds" at the top of the Fernie Formation.
• The Smoky Group is conformably and transgressively followed by the Wapiti Group and rests conformably on the Dunvegan Formation sandstone.
• 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 interfingers with the Lockatong Formation and also rests conformably below the Passaic Formation.
• 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 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.
• 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 Stonewall Formation is overlain by the Interlake Group (conformably in the south, disconformably in the north) and sharply overlays the Stony Mountain Formation.
• The Angoumian sensu stricto conformably overlies the Ligerian and closes with a hardground towards the overlying Coniacian.
• The base of the unit, which rests conformably on the shallower-water Vaqueros Formation, contains a glauconitic layer.
• The formation lies conformably on the prolifically-fossiliferous shallow marine sandstone, siltstone and mudrock of the Staithes Formation.
• 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).
• The Clackmannan Group conformably overlays the rocks of the Strathclyde Group and underlays the Coal Measures, this latter boundary also being conformable.
• The Bloyd Formation conformably overlies the Hale Formation and unconformably underlies the Atoka Formation.
• The Indian Point Formation is conformably overlain by within-plate tholeiitic mafic to intermediate flows and flow breccias of the Archibald Settlement Formation, developed as a synsedimentary normal fault in the Late Silurian, based on the presence of polymictic conglomerate beds in a thickened Indian Point section east of the fault.

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