The Evolution of the Pegtymel Inverted Rift Based on the Results of Kinematic Reconstruction (Chukchi Sea)

IF 0.3 Q4 GEOLOGY

Moscow University Geology Bulletin Pub Date : 2023-11-16 DOI:10.3103/s0145875223040117

N. V. Pravikova, M. V. Korotaev, K. F. Startseva, M. O. Belyaev, A. M. Nikishin

引用次数: 0

Abstract

A kinematic model has been built for the seismic profile traversing the Pegtymel inverted rift (Chukchi Sea). Three main stages of rift formation have been identified: 125–34, 34–20, and 20–0 Ma. The identified stages are compared with the geological evolution of the Eastern Arctic.

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基于运动学重建结果的楚科奇海Pegtymel倒裂谷演化

摘要建立了穿越Pegtymel逆裂谷(楚科奇海)地震剖面的运动学模型。确定了裂谷形成的三个主要阶段:125-34 Ma、34-20 Ma和20-0 Ma。将所确定的阶段与北极东部的地质演化进行了比较。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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来源期刊

Moscow University Geology Bulletin GEOLOGY-

CiteScore

0.60

自引率

25.00%

发文量

期刊介绍： Moscow University Geology Bulletin is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.