Some Aspects of Petroleum System Modeling in the North-Eastern Part of West Siberia Basin

Author(s):  
A. Kazanenkova
2016 ◽  
Vol 9 (4) ◽  
Author(s):  
Mohamed Arab ◽  
Djelloul Belhai ◽  
Didier Granjeon ◽  
François Roure ◽  
Arnaud Arbeaumont ◽  
...  

2021 ◽  
Vol 2 (1) ◽  
pp. 52-61
Author(s):  
Aleksey A. Deshin ◽  
Svetlana A. Yazikova

One-dimensional modeling of four well of the North-Eastern part of West Siberia was conducted. When using kinetic parameters of II type kerogen (Menil-2) and calculated kerogen characteristics for the Upper Jurassic source rocks hydrocarbons generation volume was estimated.


Author(s):  
R. M. Gilaev ◽  
A. V. Stupakova ◽  
A. N. Stafeev ◽  
A. A. Suslova ◽  
E. S. Shelkov

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.


2020 ◽  
Vol 122 ◽  
pp. 104664
Author(s):  
Adriana Lemgruber-Traby ◽  
Nicolas Espurt ◽  
Christine Souque ◽  
Pierre Henry ◽  
Ysabel Calderon ◽  
...  

Author(s):  
Sergey B. Kuklev ◽  
Vladimir A. Silkin ◽  
Valeriy K. Chasovnikov ◽  
Andrey G. Zatsepin ◽  
Larisa A. Pautova ◽  
...  

On June 7, 2018, a sub-mesoscale anticyclonic eddy induced by the wind (north-east) was registered on the shelf in the area of the city of Gelendzhik. With the help of field multidisciplinary expedition ship surveys, it was shown that this eddy exists in the layer above the seasonal thermocline. At the periphery of the eddy weak variability of hydrochemical parameters and quantitative indicators of phytoplankton were recorded. The result of the formation of such eddy structure was a shift in the structure of phytoplankton – the annual observed coccolithophores bloom was not registered.


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