作者:XIE Fan,REN Yaqiong,HOU Jinxin
摘要:We monitored the amplitude changes of coda transmission waves around 500 kHz across the frictional interface of a simulated 1. 5-meter-long fault during normal stress holding test.We find that the amplitude of coda transmission waves increases with the logarithm of stationary contact time. Localized increase amounted to a level ranging from 4% to 16%along the fault is observed during the 1-hour experiment. We discuss that the frictional strength at mesoscopic scale,which is related to the amplitude of coda transmission waves,is responsible for the phenomenon. Combining the reported method with other complementary approaches will enhance the understanding of fault mechanism either at laboratory or on-site applications.
發文機構:Institute of Geophysics
關鍵詞:CODAtransmissionwavesLABORATORYFAULTFrictionalcontactarea
分類號: P31[天文地球—固體地球物理學][天文地球—地球物理學]