2015山东平邑石膏矿塌陷地震震源参数测定  

Source characterization of the 2015 gypsum mining earthquake in Pingyi,Shandong

作　　者：杨慧 储日升 盛敏汉 

机构地区：[1]中国科学院测量与地球物理研究所大地测量与地球动力学国家重点实验室,武汉430077 [2]中国科学院大学,北京100049

出　　处：《地球物理学进展》2018年第1期125-132,共8页Progress in Geophysics

基　　金：国家重点基础研究发展计划(973计划)课题(2013CB733203);国家自然科学基金(41474049)联合资助

摘　　要：北京时间2015年12月25日07时56分,山东省临沂市平邑县(北纬35.5°,东经117.7°)发生4.0级地震,造成了较大的人员伤亡和经济损失.本文利用国家测震台网提供的宽频地震台波形数据,采用SCC(Sliding-window Cross-Correlation)方法确定了地震发生后10 min内有至少6次余震事件发生,并使用gCAP(generalized Cut and Paste)方法反演了此次地震和最大一次余震事件的震源机制解和深度.反演的结果显示,两次事件的震源机制均含有非常明显的非双力偶成分,且表现为体积缩小的内爆机制.这些结果表明,本次事件与石膏矿区的结构和应力场状态密切相关,可能是由于石膏矿内采空区的闭合,同时伴随顶板或底板的剪切运动造成的.Source parameters of mining earthquakes are essential to investigate pressure redistribution and accumulation due to underground excavation. On 25 December 2015,a local magnitude4. 0 earthquake occurred at 07： 56： 12 BJT in Pingyi county,China（ latitude： 35. 5° N,longitude： 117. 7° E） with a depth of 0 km.This earthquake is caused by underground cave collapse. In this paper,we used sliding-window cross-correlation method to detect aftershocks of this event. The result indicates there are at least six aftershocks within ten minutes after the earthquake. Then we inverted focal mechanisms and depths of the mainshock and the largest aftershock with three-component broadband seismic waveform data recorded by the National Seismic Network. We used the generalized Cut-and-Paste（ gCAP） method to obtain their moment tensors,which allows for a characterization of the relative amounts of deviatoric and isotropic source components. This gCAP method divides three component waveforms into Pnl and surface wave segments,and allows adjustable time shifts between observed and synthetic data,so that it reduces the influence of uncertainties in the 1-D velocity model. The results show that both events have similar focal mechanisms, which contains obvious non-doublecouple component with a large proportion of isotropic source component. The mechanisms are dominated by 80% implosive isotropic energy and 20% thrusting double couple energy. Such mechanisms might be explained by an asymmetric collapse of the mine cavity due to unevenly distributed in situ stresses,sympathetic shear on a roof fault,or between the roof and floor of the mine.

关 键 词：gCAP方法 震源机制 塌陷地震 

分 类 号：P315[天文地球—地震学]