Paleobathymetry of the Late Jurassic-Neocomian basin in northern West Siberia and the impact of natural processes |
| |
| Institution: | 1. ERAAUB: Equip de Recerca Arqueològica i Arqueomètrica de la Universitat de Barcelona, Spain;2. Department of Materials Science and Metallurgical Engineering, Universitat Politècnica de Catalunya, Spain;3. Dipartimento di Scienze della Terra e del Mare (DiSTeM), Università degli Studi di Palermo, Italy;1. National Center for Biotechnology, Life Science and Environment Research Institute, King Abdulaziz City for Science and Technology (KACST), Riyadh, Saudi Arabia;2. National Center for Biotechnology, King Abdulaziz City for Science and Technology, Riyadh, Saudi Arabia;3. Adelaide Medical School, The University of Adelaide, Adelaide, South Australia, Australia;4. School of Information Technology and Mathematical Sciences, Division of Information Technology, Engineering and the Environment, The University of South Australia, Adelaide, SA, Australia;5. Institute of Biotechnology, Shiraz University, Shiraz, Iran;6. School of Biological Sciences, Faculty of Science and Engineering, Flinders University, Adelaide, SA, Australia;7. School of Animal and Veterinary Sciences, The University of Adelaide, South Australia, Australia |
| |
| Abstract: | Paleobathymetrical reconstructions were performed for the Volgian-Neocomian basin in northern West Siberia. The proposed technique takes into account a number of factors, such as the rates of basin subsidence and sedimentation, sediment lithification and types of lithology, sea level changes, and isostasy. The role of each factor controlling the depth of the paleobasin is considered. The study reveals several stages of formation of the Neocomian clinoform complex of West Siberia, with different regimes of basin subsidence, sedimentation, and isostatic compensation. |
| |
| Keywords: | |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
