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首页> 外文期刊>Izvestiya. Physics of the solid earth >Formation dynamics of fault-block structures in the eastern segment of the Baikal-Stanovoi seismic belt
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Formation dynamics of fault-block structures in the eastern segment of the Baikal-Stanovoi seismic belt

机译:贝加尔-Stanovoi地震带东段的断块构造形成动力学

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摘要

The combined analysis of geological-geophysical characteristics of active faults, morphotectonic features of the relief, and data of satellite measurements and on seismicity in the southeastern Aldan-Stanovoi block (the eastern flank of the Olekma-Stanovoi seismotectonic zone) made it possible to reconstruct the kinematic development of recent falt-block structures with the defining conjugate systems of main seismogenerating faults located in the zone of dynamic influence of three major lithospheric plates: Eurasian, Amur, and Sea of Okhotsk.
机译:结合分析活动断层的地质-地球物理特征,浮雕的构造构造特征,Aldan-Stanovoi东南区(Olekma-Stanovoi地震构造带的东翼)的卫星测量数据和地震活动,可以进行重建最近的断块构造的运动学发展,其主要成地震断层的共轭系统位于三个主要岩石圈板块的动态影响区域:欧亚大陆,阿穆尔半岛和鄂霍次克海。

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