1887

Abstract

Magnetotelluric and seismic (P-SV converted waves data) field works were fulfilled in Western and Central Caucasus. These exploration works showed, that the sedimentary cover of Indolo-Cuban depression is about 12 km. In the limits of Scifian plate was framed lover floor folded basis (r = 100-300 Ohm.m). Zones of conductivity under the Elbrus mountain are correlated with the absence converted waves. The boundaries between geoelectric inhomogeneities are corresponded with deep faults.

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/content/papers/10.3997/2214-4609-pdb.20.P134
2006-10-16
2020-04-04
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.20.P134
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