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
- Авторы: Ivolga E.1, Manilov Y.1
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Учреждения:
- Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
- Выпуск: Том 13, № 6 (2019)
- Страницы: 493-509
- Раздел: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211714
- DOI: https://doi.org/10.1134/S1819714019060034
- ID: 211714
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Аннотация
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.
Об авторах
E. Ivolga
Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: ivolga@itig.as.khb.ru
Россия, ul. Kim Yu Chena 65, Khabarovsk, 680000
Yu. Manilov
Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: ymanilov@itig.as.khb.ru
Россия, ul. Kim Yu Chena 65, Khabarovsk, 680000