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Seismically mobilized moraines in the Tien Shan

机译:天山地震动mo

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Moraines studied in the Chon-Kyzylsuu River valley (southeastern Lake Issyk-Kul region, Tien Shan) were mobilized during historic and prehistoric large earthquakes. Seismic triggers of moraine mobilization included the M > 8 Kebin earthquake of 1911 and prehistoric events that produced rockslides, landslides, and multiple fault scarps. Rockslides in the Chon-Kyzylsuu basin are located in the hanging wall of the Terskey border thrust fault. The observed deformation results from at least four prehistoric earthquakes in the second half of the Holocene (early 20th century BC, early 11th century BC, middle 8th century BC, and early 2nd century BC), with local shaking intensity I >= 7. (C) 2015, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
机译:在历史和史前大地震中,动员了在Chon-Kyzylsuu河谷(天山伊塞克湖南部地区的东南湖)研究的蒙古人。冰ora运动的地震触发因素包括1911年的M> 8克宾地震和史前事件,这些事件产生了岩石滑坡,滑坡和多个断层陡坡。 Chon-Kyzylsuu盆地的滑坡位于Terskey边界逆冲断层的悬挂壁上。观测到的变形是由全新世后半期(公元前20世纪初,公元前11世纪初,公元前8世纪中叶和公元前2世纪初)至少四次史前地震导致的,局部震荡强度I> = 7。 C)2015年,VS Sobolev IGM,RAS的西伯利亚分公司。由Elsevier B.V.发布。保留所有权利。

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