THE BAZHENOV HORIZON OF WEST SIBERIA: STRUCTURE, CORRELATION, AND THICKNESS

2018 ◽  
Keyword(s):  
West Siberia ◽  
Structure Correlation ◽  
Bazhenov Horizon

The Bazhenov Horizon of West Siberia: structure, correlation, and thickness

2018 ◽  
Vol 59 (7) ◽  
pp. 846-863 ◽  
Author(s):  
S.V. Ryzhkova ◽  
L.M. Burshtein ◽  
S.V. Ershov ◽  
V.A. Kazanenkov ◽  
A.E. Kontorovich ◽  
...  
Keyword(s):  
West Siberia ◽  
Structure Correlation ◽  
Bazhenov Horizon

Distribution of organic matter in rocks of the Bazhenov horizon ( West Siberia )

2018 ◽  
Vol 59 (3) ◽  
pp. 285-298 ◽  
Author(s):  
A.E. Kontorovich ◽  
E.V. Ponomareva ◽  
L.M. Burshtein ◽  
V.N. Glinskikh ◽  
N.S. Kim ◽  
...  
Keyword(s):  
Organic Matter ◽  
West Siberia ◽  
Bazhenov Horizon

scholarly journals Сonditions of sedimentation and paleogeographic zoning of the Bazhenov horizon (Tithon-Lower Berrias) in West Siberia

Georesursy ◽  
2017 ◽  
Vol 19 (Special) ◽  
pp. 134-143 ◽  
Author(s):  
A.N. Stafeev ◽  
◽  
A.V. Stoupakova ◽  
A.A. Suslova ◽  
R.M. Gilaev ◽  
...  
Keyword(s):  
West Siberia ◽  
Bazhenov Horizon

The Structure of the Bazhenov Horizon in the Northeast Part of West Siberia

2018 ◽  
Vol 73 (4) ◽  
pp. 361-365
Author(s):  
R. M. Gilaev ◽  
A. V. Stupakova ◽  
A. N. Stafeev ◽  
A. A. Suslova ◽  
E. S. Shelkov
Keyword(s):  
West Siberia ◽  
Bazhenov Horizon

STRUCTURE OF BAZHENOV HORIZON IN THE NORTH-EAST OF WEST SIBERIA

2018 ◽  
pp. 41-45
Author(s):  
R. M. Gilaev ◽  
A. V. Stupakova ◽  
A. N. Stafeev ◽  
A. A. Suslova ◽  
E. S. Shelkov
Keyword(s):  
West Siberia ◽  
High Carbon ◽  
Bazhenov Formation ◽  
North East ◽  
The North ◽  
New Variant ◽  
North Eastern ◽  
Bazhenov Horizon ◽  
Lower Berriasian ◽  
North Eastern Part

Based on the lithofacies and structural analysis we consider a new variant of the structuralfacies zonation of the Bazhenov horizon (Tithonian — lower Berriasian) in the north-eastern part of West Siberia. The low content of terrigenous sedimentary material in high-carbon facies the bazhenov formation, due to its capture of relatively deep Pur-Tazovsky paleobasins, which formed the cone of the Yenisei-Khatanga sea strait. Pur-Tazovsky basin filled with the yanovstanskaya formation, he adjoined from the north-east to extensive relatively shallow Obsky paleobasin — the accumulation of black shale bazhenov formation.

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