Structure of the Lithosphere in the Zone of the Continent–Ocean Transition in the Southern Part of the Russian Far East: Evidence from the Density Modeling
- 作者: Ivolga E.1, Manilov Y.1
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隶属关系:
- Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
- 期: 卷 13, 编号 6 (2019)
- 页面: 493-509
- 栏目: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211714
- DOI: https://doi.org/10.1134/S1819714019060034
- ID: 211714
如何引用文章
详细
The quantitative processing of gravimetric data is performed and the 3D density model is calculated for the southern part of the Russian margin of Eurasian continent. Based on the density model, new patterns of disjunctive tectonics at different depth levels are revealed and the position of the region at the global tectonic level is shown. It is established that the transition zone is an integrated lithospheric structure of the northeastern orientation, in which there are mantle blocks with the boundaries corresponding to the borders of depressions and major tectonic objects. The data obtained may be applied for refinement of the deep structure and paleogeodynamics of the studied area.
作者简介
E. Ivolga
Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
编辑信件的主要联系方式.
Email: ivolga@itig.as.khb.ru
俄罗斯联邦, ul. Kim Yu Chena 65, Khabarovsk, 680000
Yu. Manilov
Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
编辑信件的主要联系方式.
Email: ymanilov@itig.as.khb.ru
俄罗斯联邦, ul. Kim Yu Chena 65, Khabarovsk, 680000