RESULTS OF GEOPHYSICAL INVESTIGATIONS ON ADYGEYA PROFILE
Keywords:
big Caucasus, Caucasus movement, deep geophysical study
Abstract
In recent years, several organizations have been implemented geophysical surveys in the western part of the Central Caucasus using a variety of methods. Along the Adygeya profile (Dagomys-Abadzekhskaya-Giaginskaia) were received a comprehensive geophysical characteristics of deep crustal section across the entire structure of the Greater Caucasus. Examines material МТZ, IGAD and gravimagnetsurvey. The structure of the Greater Caucasus, as part of the Alpine collision belt, appeared with creeping of the Scythian plate on one of the Caucasus’s consolidated crust microplate.
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Published
2015-02-11
Section
Articles