LENA-KHATANGA杂流（西伯利亚地台以北）的陆源沉积作用（С3–K）的演化

Q4 Earth and Planetary Sciences

Geology and Mineral Resources of Siberia Pub Date : 2022-10-01 DOI:10.20403/2078-0575-2022-3-17-29

V. Devyatov

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引用次数: 1

摘要

在分析地质和地球物理资料的基础上，给出了Lena-Khatanga界面上古生代、三叠纪、侏罗系和白垩纪陆相沉积的厚度、组成、形成条件和演化数据，并提出了沉积与地壳大型线理和构造事件的关系。晚古生代、早三叠纪、侏罗系-白垩纪和新生代构造运动阶段完成了构造的形成。

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EVOLUTION OF TERRIGENOUS SEDIMENTOGENESIS (С3–K) OF THE LENA-KHATANGA INTERFLUVES (NORTH OF THE SIBERIAN PLATFORM)

Based on the analysis of geological and geophysical materials, data on the thickness, composition, conditions of formation and evolution of terrigenous sedimentogenesis of Upper Paleozoic, Triassic, Jurassic and Cretaceous deposits of the Lena-Khatanga interfluve are given, the relationship of sedimentation with large lineaments of the Earth’s crust and tectonic events is presented. The Late Paleozoic, Early Triassic, Jurassic-Cretaceous and Cenozoic stages of tectogenesis that completed the formation of structures are identified and confirmed.

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来源期刊

Geology and Mineral Resources of Siberia Earth and Planetary Sciences-Geology

CiteScore

0.30

自引率

0.00%

发文量