TECTONICS AND EVOLUTION OF THE LITHOSPHERE OF THE EASTERN FRAGMENT OF THE MONGOL-OKHOTSK OROGENIC BELT

B. F. Shevchenko; L. I. Popeko; A. N. Didenko

doi:10.5800/GT-2014-5-3-0148

Геодинамика и тектонофизика (Sep 2015)

TECTONICS AND EVOLUTION OF THE LITHOSPHERE OF THE EASTERN FRAGMENT OF THE MONGOL-OKHOTSK OROGENIC BELT

B. F. Shevchenko,
L. I. Popeko,
A. N. Didenko

Affiliations

B. F. Shevchenko: Yu.A. Kosygin Institute of Tectonics and Geophysics, Far East Branch of RAS, Khabarovsk, Russia
L. I. Popeko: Yu.A. Kosygin Institute of Tectonics and Geophysics, Far East Branch of RAS, Khabarovsk, Russia
A. N. Didenko: Yu.A. Kosygin Institute of Tectonics and Geophysics, Far East Branch of RAS, Khabarovsk, Russia

DOI: https://doi.org/10.5800/GT-2014-5-3-0148
Journal volume & issue: Vol. 5, no. 3
pp. 667 – 682

Abstract

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The article describes tectonics and the deep structure of the lithosphere in the eastern fragment of the Mongol-Okhotsk orogenic belt according to results of analysis of the geological and geophysical database. With account of palinspastic reconstructions, the model is developed to show the most probable paleogeodynamics of the lithosphere in the Mongol-Okhotsk orogenic belt and its heterochronous terrains.

Published in Геодинамика и тектонофизика

ISSN: 2078-502X (Online)
Publisher: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
Country of publisher: Russian Federation
LCC subjects: Science
Website: http://gt.crust.irk.ru/index.en.html

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