ACTIVE FAULTS AND THE STRUCTURE OF KERCH STRAIT ZONE

  • E.A. Rogozhin Schmidt Institute of Physics of the Earth of RAS, 123995, Moscow, B.Gruzinskaya 10/1
  • A.V. Gorbatikov Schmidt Institute of Physics of the Earth of RAS, 123995, Moscow, B.Gruzinskaya 10/1
  • A.N. Ovsyuchenko Schmidt Institute of Physics of the Earth of RAS, 123995, Moscow, B.Gruzinskaya 10/1
Keywords: active faults, geological activity, microseismic sounding

Abstract

Field geologic-geomorphological investigations of active faults zones of connection between Crimea and Caucasus moveable systems were carried out [Rogozhin et al., 2015]. Morphokinematic characteristics of the main tectonic disturbances are given in the article [Trifonov et al., 2002]. Such disturbances are South-Azov fault, Vyshesteblievsk flexure, Kerch strait fault (underwater), Pravdinsk fault.
108  |    57
Published
2015-03-20