Petrophysical features of the tectonic structures of the Okhotsk continent–ocean transition zone


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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.

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E. Ivolga

Kosygin Institute of Tectonics and Geophysics, Far East Branch

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Email: ivolga@itig.as.khb.ru
俄罗斯联邦, ul. Kim Yu Chena 65, Khabarovsk, 680000

V. Gurovich

Kosygin Institute of Tectonics and Geophysics, Far East Branch

Email: ivolga@itig.as.khb.ru
俄罗斯联邦, ul. Kim Yu Chena 65, Khabarovsk, 680000

N. Romanovsky

Kosygin Institute of Tectonics and Geophysics, Far East Branch

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

Email: ivolga@itig.as.khb.ru
俄罗斯联邦, ul. Kim Yu Chena 65, Khabarovsk, 680000

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