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The subsidence and thermal history of the Baikit anteclise sedimentary basin. / Vasilieva, K. Yu; Bakay, E. A.; Ershova, V. B.; Khusnitdinov, R. R.; Khudoley, A. K.; Kozlova, E. V.; Soloveva, S. A.

In: Moscow University Geology Bulletin, Vol. 71, No. 6, 01.11.2016, p. 445-450.

Research output: Contribution to journalArticlepeer-review

Harvard

Vasilieva, KY, Bakay, EA, Ershova, VB, Khusnitdinov, RR, Khudoley, AK, Kozlova, EV & Soloveva, SA 2016, 'The subsidence and thermal history of the Baikit anteclise sedimentary basin', Moscow University Geology Bulletin, vol. 71, no. 6, pp. 445-450. https://doi.org/10.3103/S0145875216060120

APA

Vasilieva, K. Y., Bakay, E. A., Ershova, V. B., Khusnitdinov, R. R., Khudoley, A. K., Kozlova, E. V., & Soloveva, S. A. (2016). The subsidence and thermal history of the Baikit anteclise sedimentary basin. Moscow University Geology Bulletin, 71(6), 445-450. https://doi.org/10.3103/S0145875216060120

Vancouver

Vasilieva KY, Bakay EA, Ershova VB, Khusnitdinov RR, Khudoley AK, Kozlova EV et al. The subsidence and thermal history of the Baikit anteclise sedimentary basin. Moscow University Geology Bulletin. 2016 Nov 1;71(6):445-450. https://doi.org/10.3103/S0145875216060120

Author

Vasilieva, K. Yu ; Bakay, E. A. ; Ershova, V. B. ; Khusnitdinov, R. R. ; Khudoley, A. K. ; Kozlova, E. V. ; Soloveva, S. A. / The subsidence and thermal history of the Baikit anteclise sedimentary basin. In: Moscow University Geology Bulletin. 2016 ; Vol. 71, No. 6. pp. 445-450.

BibTeX

@article{61c15f06781c4daf85815775ebeb4f51,
title = "The subsidence and thermal history of the Baikit anteclise sedimentary basin",
abstract = "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.",
keywords = "Baikit anteclise, Riphean sediments, Rock–Eval, thermal history of sedimentary basin",
author = "Vasilieva, {K. Yu} and Bakay, {E. A.} and Ershova, {V. B.} and Khusnitdinov, {R. R.} and Khudoley, {A. K.} and Kozlova, {E. V.} and Soloveva, {S. A.}",
year = "2016",
month = nov,
day = "1",
doi = "10.3103/S0145875216060120",
language = "English",
volume = "71",
pages = "445--450",
journal = "Moscow University Geology Bulletin",
issn = "0145-8752",
publisher = "Springer Nature",
number = "6",

}

RIS

TY - JOUR

T1 - The subsidence and thermal history of the Baikit anteclise sedimentary basin

AU - Vasilieva, K. Yu

AU - Bakay, E. A.

AU - Ershova, V. B.

AU - Khusnitdinov, R. R.

AU - Khudoley, A. K.

AU - Kozlova, E. V.

AU - Soloveva, S. A.

PY - 2016/11/1

Y1 - 2016/11/1

N2 - 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.

AB - 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.

KW - Baikit anteclise

KW - Riphean sediments

KW - Rock–Eval

KW - thermal history of sedimentary basin

UR - http://www.scopus.com/inward/record.url?scp=85017591546&partnerID=8YFLogxK

U2 - 10.3103/S0145875216060120

DO - 10.3103/S0145875216060120

M3 - Article

AN - SCOPUS:85017591546

VL - 71

SP - 445

EP - 450

JO - Moscow University Geology Bulletin

JF - Moscow University Geology Bulletin

SN - 0145-8752

IS - 6

ER -

ID: 43292900