The Relationship among Geodynamics, Heat Flow, Deep Structure, and the Oil and Gas Potential of Yamal
- Authors: Ivanov K.S.1, Kostrov N.P.1, Koroteev V.A.1
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Affiliations:
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences
- Issue: Vol 486, No 1 (2019)
- Pages: 490-493
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/194915
- DOI: https://doi.org/10.1134/S1028334X1905012X
- ID: 194915
Cite item
Abstract
The amount of hydrocarbon deposits per unit area of Yamal Peninsula is more than 100 times as much as the global average. The hydrocarbon deposits are generally situated in areas with high current geodynamic activity. According to the data of seismic tomography, in the Yamal area, the mantle structure is abnormal. The southern part of the Kara Sea, the Yamal Peninsula, and the western part of the Gydan Peninsula are involved into the large positive anomaly of the heat flow density, the epicenter of which occurs in the vicinity of the Rusanovskoye deposit. Almost all hydrocarbon deposits of Yamal are situated on the flanks of the West Siberian rift system and, simultaneously, in the gradient zones of the heat flow density.
About the authors
K. S. Ivanov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences
Author for correspondence.
Email: ivanovks@igg.uran.ru
Russian Federation, Yekaterinburg, 620016
N. P. Kostrov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences
Email: ivanovks@igg.uran.ru
Russian Federation, Yekaterinburg, 620016
V. A. Koroteev
Zavaritsky Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences
Email: ivanovks@igg.uran.ru
Russian Federation, Yekaterinburg, 620016
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