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The Bazhenov Horizon of West Siberia : structure, correlation, and thickness. / Ryzhkova, S. V.; Burshtein, L. M.; Ershov, S. V. et al.

In: Russian Geology and Geophysics, Vol. 59, No. 7, 01.07.2018, p. 846-863.

Research output: Contribution to journal › Article › peer-review

Harvard

Ryzhkova, SV, Burshtein, LM, Ershov, SV, Kazanenkov, VA, Kontorovich, AE, Kontorovich, VA, Nekhaev, AY, Nikitenko, BL, Fomin, MA, Shurygin, BN, Beizel, AL, Borisov, EV, Zolotova, OV, Kalinina, LM & Ponomareva, EV 2018, 'The Bazhenov Horizon of West Siberia: structure, correlation, and thickness', Russian Geology and Geophysics, vol. 59, no. 7, pp. 846-863. https://doi.org/10.1016/j.rgg.2018.07.009

APA

Ryzhkova, S. V., Burshtein, L. M., Ershov, S. V., Kazanenkov, V. A., Kontorovich, A. E., Kontorovich, V. A., Nekhaev, A. Y., Nikitenko, B. L., Fomin, M. A., Shurygin, B. N., Beizel, A. L., Borisov, E. V., Zolotova, O. V., Kalinina, L. M., & Ponomareva, E. V. (2018). The Bazhenov Horizon of West Siberia: structure, correlation, and thickness. Russian Geology and Geophysics, 59(7), 846-863. https://doi.org/10.1016/j.rgg.2018.07.009

Vancouver

Ryzhkova SV, Burshtein LM, Ershov SV, Kazanenkov VA, Kontorovich AE, Kontorovich VA et al. The Bazhenov Horizon of West Siberia: structure, correlation, and thickness. Russian Geology and Geophysics. 2018 Jul 1;59(7):846-863. doi: 10.1016/j.rgg.2018.07.009

Author

Ryzhkova, S. V. ; Burshtein, L. M. ; Ershov, S. V. et al. / The Bazhenov Horizon of West Siberia : structure, correlation, and thickness. In: Russian Geology and Geophysics. 2018 ; Vol. 59, No. 7. pp. 846-863.

BibTeX

@article{42e10e7dc2e44882a26b2b973ae36031,
title = "The Bazhenov Horizon of West Siberia: structure, correlation, and thickness",
abstract = "The type sections of the Bazhenov Horizon and formations recognized within this horizon have been identified based on a comprehensive analysis of paleontological, lithological, geophysical (well-log and CDP seismic data), and geochemical data on the West Siberian Basin. The Bazhenov Horizon was traced throughout the entire West Siberian sedimentary basin. The criteria for the recognition of the top and base of this horizon within the stratigraphic equivalents of the Bazhenov Formation were suggested. The proposed facies-stratigraphic zonation of the Bazhenov Horizon reflects the spatial location of all formations identified within this horizon. As seen on the newly proposed thickness map, the Bazhenov Horizon reaches a thickness of 15-25 m within the Bazhenov and Tutleim Formations, 30-35 m within the Mulym'ya Formation, 30-45 m within the Danilov Formation, 40-65 m within the Mar'yanovka Formation, up to 100 m within the Golchikha Formation, > 350 m within the Yanovstan Formation, up to 35 m within the Bagan Formation, and 35-40 m within the Maksimkin Yar Formation. A marginal filter (according to A.P. Lisitzin) has been identified along the East Siberian land.",
keywords = "Bazhenov Formation, Bazhenov Horizon, marginal filter, well-to-well correlation, West Siberia, CLASSIFICATION",
author = "Ryzhkova, {S. V.} and Burshtein, {L. M.} and Ershov, {S. V.} and Kazanenkov, {V. A.} and Kontorovich, {A. E.} and Kontorovich, {V. A.} and Nekhaev, {A. Yu} and Nikitenko, {B. L.} and Fomin, {M. A.} and Shurygin, {B. N.} and Beizel, {A. L.} and Borisov, {E. V.} and Zolotova, {O. V.} and Kalinina, {L. M.} and Ponomareva, {E. V.}",
year = "2018",
month = jul,
day = "1",
doi = "10.1016/j.rgg.2018.07.009",
language = "English",
volume = "59",
pages = "846--863",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "7",

}

RIS

TY - JOUR

T1 - The Bazhenov Horizon of West Siberia

T2 - structure, correlation, and thickness

AU - Ryzhkova, S. V.

AU - Burshtein, L. M.

AU - Ershov, S. V.

AU - Kazanenkov, V. A.

AU - Kontorovich, A. E.

AU - Kontorovich, V. A.

AU - Nekhaev, A. Yu

AU - Nikitenko, B. L.

AU - Fomin, M. A.

AU - Shurygin, B. N.

AU - Beizel, A. L.

AU - Borisov, E. V.

AU - Zolotova, O. V.

AU - Kalinina, L. M.

AU - Ponomareva, E. V.

PY - 2018/7/1

Y1 - 2018/7/1

N2 - The type sections of the Bazhenov Horizon and formations recognized within this horizon have been identified based on a comprehensive analysis of paleontological, lithological, geophysical (well-log and CDP seismic data), and geochemical data on the West Siberian Basin. The Bazhenov Horizon was traced throughout the entire West Siberian sedimentary basin. The criteria for the recognition of the top and base of this horizon within the stratigraphic equivalents of the Bazhenov Formation were suggested. The proposed facies-stratigraphic zonation of the Bazhenov Horizon reflects the spatial location of all formations identified within this horizon. As seen on the newly proposed thickness map, the Bazhenov Horizon reaches a thickness of 15-25 m within the Bazhenov and Tutleim Formations, 30-35 m within the Mulym'ya Formation, 30-45 m within the Danilov Formation, 40-65 m within the Mar'yanovka Formation, up to 100 m within the Golchikha Formation, > 350 m within the Yanovstan Formation, up to 35 m within the Bagan Formation, and 35-40 m within the Maksimkin Yar Formation. A marginal filter (according to A.P. Lisitzin) has been identified along the East Siberian land.

AB - The type sections of the Bazhenov Horizon and formations recognized within this horizon have been identified based on a comprehensive analysis of paleontological, lithological, geophysical (well-log and CDP seismic data), and geochemical data on the West Siberian Basin. The Bazhenov Horizon was traced throughout the entire West Siberian sedimentary basin. The criteria for the recognition of the top and base of this horizon within the stratigraphic equivalents of the Bazhenov Formation were suggested. The proposed facies-stratigraphic zonation of the Bazhenov Horizon reflects the spatial location of all formations identified within this horizon. As seen on the newly proposed thickness map, the Bazhenov Horizon reaches a thickness of 15-25 m within the Bazhenov and Tutleim Formations, 30-35 m within the Mulym'ya Formation, 30-45 m within the Danilov Formation, 40-65 m within the Mar'yanovka Formation, up to 100 m within the Golchikha Formation, > 350 m within the Yanovstan Formation, up to 35 m within the Bagan Formation, and 35-40 m within the Maksimkin Yar Formation. A marginal filter (according to A.P. Lisitzin) has been identified along the East Siberian land.

KW - Bazhenov Formation

KW - Bazhenov Horizon

KW - marginal filter

KW - well-to-well correlation

KW - West Siberia

KW - CLASSIFICATION

UR - http://www.scopus.com/inward/record.url?scp=85049993158&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2018.07.009

DO - 10.1016/j.rgg.2018.07.009

M3 - Article

AN - SCOPUS:85049993158

VL - 59

SP - 846

EP - 863

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 7

ER -

ID: 15965111