The role of the tectonic factor in the formation of the berriasian-valanginian clinoforms of the Western part of Yenisei-Khatanga regional trough and the neighboring areas of Western Siberian geosyneclysis
It has been established that the Nizhnexetskaya and Sukhodudinskaya (lower part) formations, and probably, the underlying deposits - Golchihinskaya (upper part) and Yanovstanskaya (roof), represent the clinoform complex. The article presents the argument that the tectonic factor in the formation of clinoforms was the main. The largest amount of debris material moved in this geodynamically active zone due to seismic disturbances that generate earthquakes, tsunamis and associated underwater landslides and turbidite flows, which as a result formed wedge-shaped bodies.
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2014 ◽
Vol 34
(20)
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pp. 6759-6771
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2012 ◽
Vol 197
(1)
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pp. 75-88
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2021 ◽
Vol 118
(13)
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pp. e2016304118