Яндекс.Метрика

K.Zh.Seminsky,R.M.Zaripov, V.V. Olenchenko

Выпуск: 2 , Том: 464 , Год издания: 2015
Сериальное издание: Doklady Earth Sciences
Страницы: 1044-1048

Аннотация

A new tectonophysical approach to the interpretation of the electrical resistivity tomography of shallow fault zones is proposed. The approach is based on ideas about their stage-to-stage development, which suggests a regular occurrence of different designation levels of the rock substratum. The levels distinguished on the basis of a statistical analysis of ERT data allow one to determine the boundaries of the fault zone and inner subzones, connected with the formation of the main fault plane and second-order fractures, on a geoelectrical section.
индекс в базе ИАЦ: 048106