A sequence stratigraphic analysis of the late Jurassic-Turonian in the context of the evolution of the West Siberian basin
During the Triassic, Siberia was a basin approximately 1800 kilometers wide filled by red beds and the widespread Tunguska basalts. Rifting occurred in the northern part of the basin. The western part of the Siberian basin became the West Siberian basin, which was bounded by rising uplifts both to t...
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| Format: | Others |
| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/1911/17478 |