Petrophysical features of the tectonic structures of the Okhotsk continent–ocean transition zone
- Авторы: Ivolga E.G.1, Gurovich V.G.1, Romanovsky N.P.1, Manilov Y.O.1
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Учреждения:
- Kosygin Institute of Tectonics and Geophysics, Far East Branch
- Выпуск: Том 10, № 5 (2016)
- Страницы: 351-364
- Раздел: Article
- URL: https://journal-vniispk.ru/1819-7140/article/view/211131
- DOI: https://doi.org/10.1134/S1819714016050031
- ID: 211131
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Аннотация
Petrophysical characteristics are determined for the rock complexes of the Okhotsk margin within the continent–ocean transition zone. Petrophysical maps showing the major inhomogeneities of the main tectonic elements of the studied area are constructed. Petrophysical inhomogeneities and the corresponding geophysical field anomalies are compared. A relationship between the magnetic field anomalies and subsurface rock complexes is revealed. The gravity field anomalies are related to deep inhomogeneities and are almost independent of the subsurface rock complexes of relatively low thickness.
Об авторах
E. Ivolga
Kosygin Institute of Tectonics and Geophysics, Far East Branch
Автор, ответственный за переписку.
Email: ivolga@itig.as.khb.ru
Россия, ul. Kim Yu Chena 65, Khabarovsk, 680000
V. Gurovich
Kosygin Institute of Tectonics and Geophysics, Far East Branch
Email: ivolga@itig.as.khb.ru
Россия, ul. Kim Yu Chena 65, Khabarovsk, 680000
N. Romanovsky
Kosygin Institute of Tectonics and Geophysics, Far East Branch
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
Email: ivolga@itig.as.khb.ru
Россия, ul. Kim Yu Chena 65, Khabarovsk, 680000
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