History of the inversion megaswells of the Yenisei-Khatanga basin development-Reference-Cited by-同舟云学术

History of the inversion megaswells of the Yenisei-Khatanga basin development

Published:2017-04-28 Issue:2 Volume: Page:8-15
ISSN:0579-9406
Container-title:Moscow University Bulletin. Series 4. Geology
language:
Short-container-title:Vestnik Moskovskogo universiteta. Seriâ 4, Geologiâ

Author:

Unger A. V.,Nikishin A. M.,Kuzlyapina M. A.,Afanasenkov A. P.

Abstract

Paper presents description of Balakhninsky and Rassohinsky swells, which were located in the central part of the Yenisei-Khatanga Basin by seismic and drilling data, and the results of its geological structure comparative analysis. History of swells formation discussed in de- tails, including rift initiation in the Late Permian-Early Triassic time and stages of inversion structures growth intensification in the Middle Triassic, Late Jurassic, Early Cretaceous and Cenozoic time. Asynchronous development of these structures established on the base of paleoreconstruction analysis.

Publisher

Faculty of Geology Lomonosov Moscow State University

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference8 articles.

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5. Tal'virskii D.B. Tektonika Enisei-Khatangskoi neftegazonosnoi oblasti i sopredel'nykh territorii po geofizicheskim dannym. M.: Nedra, 1976.

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