DEFORMATION CHANGES IN THE FAMENNIAN-TOURNAISSIAN CARBONATE ROCKS IN THE NORTHWESTERN MARGINAL FAULT ZONE OF THE CASPIAN BASIN

DEFORMATION CHANGES IN THE FAMENNIAN-TOURNAISSIAN CARBONATE ROCKS IN THE NORTHWESTERN MARGINAL FAULT ZONE OF THE CASPIAN BASIN

The Northwestern marginal fault zone is a part of the Caspian Basin and a boundary transition structure separating the basin from the Volga-Ural region. It has been found that this fault zone is characterized by a complex kinematic development leading to the formation of a linear salt-dome structure...

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Bibliographic Details
Main Authors: V. V. Korobkin, Zh. S. Tulemissova, A. E. Chaklikov
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2025-06-01
Series:Геодинамика и тектонофизика
Subjects:
caspian basin
northwestern marginal fault zone
carbonate reservoir
deformation changes
detachment and shear fractures
microscopic analysis
x-ray diffractometric analysis
thermal analysis
probe microanalysis
Online Access:https://www.gt-crust.ru/jour/article/view/2043
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https://www.gt-crust.ru/jour/article/view/2043

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