Earthquake potential across the North–South seismic belt of China  

作　　者：Yanchuan Li Xinjian Shan Chunyan Qu Guohong Zhang Xiaogang Song 

机构地区：[1]State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China

出　　处：《Science Bulletin》2024年第2期179-182,共4页科学通报（英文版）

基　　金：supported by the National Natural Science Foundation of China(42104007);the Basic Scientific Funding of the Institute of Geology,China Earthquake Administration(IGCEA2307)。

摘　　要：The elastic rebound theory,which frames our understanding of earthquakes,suggests that the accumulated elastic strain on faults will ultimately be released through earthquakes[1].As such,identifying the location,rate,and accumulation of slip deficit on faults constitutes a basis for seismic potential assessment[2].Interseismic coupling(ISC)refers to the ratio of the slip deficit rate on a fault to the far-field loading rate,where full and no coupling correspond to 100%and 0%slip deficits,respectively.

关 键 词：SEISMIC BELT FAULT 

分 类 号：P315[天文地球—地震学]