Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
The Bazhenov Horizon of West Siberia : structure, correlation, and thickness. / Ryzhkova, S. V.; Burshtein, L. M.; Ershov, S. V. и др.
в: Russian Geology and Geophysics, Том 59, № 7, 01.07.2018, стр. 846-863.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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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