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TECTONIC ZONING OF THE SEDIMENTARY COVER IN THE DERYUGIN BASIN OF THE SEA OF OKHOTSK BASED ON STRUCTURAL-MATERIAL (LITHOPHYSICAL) INDICATORS

In terms of tectonics, the Deryugin basin (Fig. 1) is a part of the epi-Mesozoic Okhotsk plate comprising the heterogeneous basement that is mainly pre-Cenozoic (the lower structural stage) and the sedimentary cover that is mainly represented by the Paleogenic-Neogenic-Quaternary deposits with the U...

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Autori principali: V. P. Semakin, A. V. Kochergin
Natura: Artigo
Lingua:Inglês
Pubblicazione: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2015-09-01
Serie:Геодинамика и тектонофизика
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Accesso online:https://www.gt-crust.ru/jour/article/view/70
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