The subsidence and thermal history of the Baikit anteclise sedimentary basin
- Авторлар: Vasilieva K.Y.1, Bakay E.A.2, Ershova V.B.1, Khusnitdinov R.R.3, Khudoley A.K.1, Kozlova E.V.4, Soloveva S.A.3
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Мекемелер:
- St. Petersburg State University
- Moscow State University
- Gazpromneft STC
- Skoltech
- Шығарылым: Том 71, № 6 (2016)
- Беттер: 445-450
- Бөлім: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174334
- DOI: https://doi.org/10.3103/S0145875216060120
- ID: 174334
Дәйексөз келтіру
Аннотация
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.
Негізгі сөздер
Авторлар туралы
K. Vasilieva
St. Petersburg State University
Хат алмасуға жауапты Автор.
Email: k.vasilyeva@spbu.ru
Ресей, St. Petersburg
E. Bakay
Moscow State University
Email: k.vasilyeva@spbu.ru
Ресей, Moscow
V. Ershova
St. Petersburg State University
Email: k.vasilyeva@spbu.ru
Ресей, St. Petersburg
R. Khusnitdinov
Gazpromneft STC
Email: k.vasilyeva@spbu.ru
Ресей, Moscow
A. Khudoley
St. Petersburg State University
Email: k.vasilyeva@spbu.ru
Ресей, St. Petersburg
E. Kozlova
Skoltech
Email: k.vasilyeva@spbu.ru
Ресей, Moscow
S. Soloveva
Gazpromneft STC
Email: k.vasilyeva@spbu.ru
Ресей, Moscow
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