Magnetotelluric sounding of Kamchatka View Full Text


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Article Info

DATE

2008-04

AUTHORS

Yu. F. Moroz, N. A. Laguta, T. A. Moroz

ABSTRACT

The MTS data acquired in Kamchatka during the last 30 years have been analyzed and summarized. Our interpretation is based on curves oriented along and across Kamchatka. Longitudinal and transverse curves can be affected by local geoelectric inhomogeneities. These were suppressed by conformal averaging. A bimodal interpretation of average longitudinal and transverse curves yielded a deep geoelectric model, which can be adopted as a starting point to be subsequently refined by 3D numerical modeling. The model involves a crustal conductive layer extending along central Kamchatka. In the east of the peninsula this layer is connected with crustal transverse conductive zones as wide as 50 km. Those zones have extensions toward the Pacific Ocean. Major centers of present-day volcanism occur in the transverse zones. The upper mantle contains an asthenospheric conductive layer forming an uplift beneath the present-day volcanic belt of Kamchatka. More... »

PAGES

83-93

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s0742046308020024

DOI

http://dx.doi.org/10.1134/s0742046308020024

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1019495209


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