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The Jurassic Stage in the Evolution of Mesozoic Sedimentation in the Eastern Mongol–Okhotsk Fold System

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Abstract

Based on new ideas, the most studied sections of the Jurassic deposits have been described along the structural–formational zones within the Mongol–Okhotsk Fold System from the Upper Amur to the Sea of Okhotsk. The presented modern ideas on the geology of this region may provide a reliable base for geodynamic and mineragenic reconstructions.

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Authors and Affiliations

  1. Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences, 680000, Khabarovsk, Russia

    G. L. Kirillova

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  1. G. L. Kirillova
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Correspondence to G. L. Kirillova.

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Recommended for publishing by I.B. Tsoi

Translated by A. Bobrov

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Kirillova, G.L. The Jurassic Stage in the Evolution of Mesozoic Sedimentation in the Eastern Mongol–Okhotsk Fold System. Russ. J. of Pac. Geol. 16, 455–464 (2022). https://doi.org/10.1134/S1819714022050037

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  • DOI: https://doi.org/10.1134/S1819714022050037

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