The geochemical signature caused by earthquake propagation in carbonate-hosted faults
The geochemical signature caused by earthquake propagation in carbonate-hosted faults
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DOI：
10.1016/j.epsl.2011.09.001
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发表时间：
2011-10-15
影响因子：
5.3
通讯作者：
Shimamoto, Toshihiko
中科院分区：
文献类型：
--
作者：
De Paola, Nicola;Chiodini, Giovanni;Shimamoto, Toshihiko
摩擦实验室实验已经在次地震（大约0.01 m/s）到地震滑动速率（>1 m/s）下对三叠纪白云岩的白云岩泥进行了，这些白云岩泥承载了五次主震（5
Friction laboratory experiments have been performed at sub-seismic (approximate to 0.01 m/s) to seismic slip rates (>1 m/s) on dolomite gouges of the Triassic evaporites, which hosted the five mainshocks (5