Сonditions of sedimentation and paleogeographic zoning of the Bazhenov horizon (Tithon-Lower Berrias) in West Siberia
In the global Upper Jurassic-Neocomian (Oxford-Valanginian) black-shale interval, the Bazhenov Formation occupies only the Tithonian – Lower Berriasian. The main regional reasons for this localization were the tectonic regime, the morphology of the basin’s bottom and hydrodynamics. Under the conditi...
| Príomhchruthaitheoirí: | , , , |
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| Formáid: | Alt |
| Teanga: | English |
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Georesursy Ltd.
2017-05-01
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| Sraith: | Georesursy |
| Ábhair: | |
| Rochtain ar líne: | https://geors.ru/archive/article/844/ |