Gravity flow deposits in Mesozoic sediments of Chukotka microplate (North‐East Russia)
Abstract In the Mesozoic succession of the Anyui–Chukotka fold system (North‐East Russia), five stratigraphic intervals were recognised that have an abundance of gravity flow deposits. These are the Olenekian (Lower Triassic), Upper Carnian, Upper Norian, Oxfordian–Kimmeridgian and Valanginian. The...
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| Hlavní autoři: | , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Wiley
2024-02-01
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| Edice: | The Depositional Record |
| Témata: | |
| On-line přístup: | https://doi.org/10.1002/dep2.269 |
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