The Stress–Strain State of Recent Structures in the Northeastern Sector of the Russian Arctic Region


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Complex research to determine the stress–strain state of the Earth’s crust and the types of seismotectonic destruction for the northeastern sector of the Russian Arctic was conducted. The principles of regional ranking of neotectonic structures were developed according to the activity of geodynamic processes, and argumentation for their class differentiation is presented. The structural-tectonic position, the parameters of the deep structure, the system of active faults, and the tectonic stress fields, calculated on the basis of both tectonophysical analysis of discontinuous and folded late Cenozoic deformations and seismological data, were analyzed. This complex of investigations made it possible to determine the directions of the main axes of deformations of the stress–strain state of the Earth’s crust and to reveal the regularity in the change of tectonic regimes.

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L. Imaeva

Institute of the Earth’s Crust, Siberian Branch; Institute of Geology of Diamonds and Precious Metals, Siberian Branch

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Email: imaeva@crust.irk.ru
俄罗斯联邦, Irkutsk, 664033; Yakutsk, 677891

V. Imaev

Institute of the Earth’s Crust, Siberian Branch; Institute of Geology of Diamonds and Precious Metals, Siberian Branch

Email: imaeva@crust.irk.ru
俄罗斯联邦, Irkutsk, 664033; Yakutsk, 677891

V. Mel’nikova

Institute of the Earth’s Crust, Siberian Branch; Institute of Geology of Diamonds and Precious Metals, Siberian Branch

Email: imaeva@crust.irk.ru
俄罗斯联邦, Irkutsk, 664033; Yakutsk, 677891

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