NEOTECTONIC DEFORMATION IN THE SOUTHWESTERN SIBERIAN CRATON
A.V. Arzhannikova and S.G. Arzhannikov
Institute of the Earth's Crust, Siberian Branch of the RAS, 128 ul. Lermontova, Irkutsk, 664033, Russia
Keywords: Cenozoic tectonics, deformation, southwestern Siberian craton
Pages: 272-277
Abstract
New neotectonic data from the southwestern periphery of the Siberian craton reveal post-Miocene reverse thrusting in the zone of the Alar'-Belaya fault. Traces of activity were found in Late Pleistocene-Holocene sections in the lower reaches of the Belaya River and on the left bank of the Angara as seismogenic rupture in sediments produced by local and remote shocks.
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