Construction of regional geophysical models based on the joint interpretation of gravitaty and seismic data

The technique of solving the inverse structural gravity problem based on the joint interpretation of gravity and seismic data is described in this paper. The method of solving is based on the method of local corrections, but involves some modifications described in the paper. An area of the northeas...

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Veröffentlicht in:Izvestiya. Physics of the solid earth 2010-11, Vol.46 (11), p.931-942
Hauptverfasser: Martyshko, P. S., Ladovskii, I. V., Tsidaev, A. G.
Format: Artikel
Sprache:eng
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Zusammenfassung:The technique of solving the inverse structural gravity problem based on the joint interpretation of gravity and seismic data is described in this paper. The method of solving is based on the method of local corrections, but involves some modifications described in the paper. An area of the northeastern part of the Urals and West Siberia (60°-65°N, 54°-72°E) was studied with the use of this technology and the spatial position of the boundaries of the crystalline crust of the Earth (its roof K 0 and base M) were determined from seismic and gravity data.
ISSN:1069-3513
1555-6506
DOI:10.1134/S1069351310110030