The subsidence and thermal history of the Baikit anteclise sedimentary basin


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The Riphean rocks of the Baikit anteclise have been examined using pyrolysis Rock–Eval 6 to evaluate the subsidence history and erosion level. The studied Riphean rocks have the МK3–МK4 catagenesis grade. Based on the catagenesis of organic matter we propose a model of maximum burial before the beginning of the accumulation of Vendian deposits. Estimated calculations of subsidence and erosion have shown that the assessed catagenesis grade could be reached at a depth of 7 km, while the erosion level was approximately 5–7 km.

Sobre autores

K. Vasilieva

St. Petersburg State University

Autor responsável pela correspondência
Email: k.vasilyeva@spbu.ru
Rússia, St. Petersburg

E. Bakay

Moscow State University

Email: k.vasilyeva@spbu.ru
Rússia, Moscow

V. Ershova

St. Petersburg State University

Email: k.vasilyeva@spbu.ru
Rússia, St. Petersburg

R. Khusnitdinov

Gazpromneft STC

Email: k.vasilyeva@spbu.ru
Rússia, Moscow

A. Khudoley

St. Petersburg State University

Email: k.vasilyeva@spbu.ru
Rússia, St. Petersburg

E. Kozlova

Skoltech

Email: k.vasilyeva@spbu.ru
Rússia, Moscow

S. Soloveva

Gazpromneft STC

Email: k.vasilyeva@spbu.ru
Rússia, Moscow

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