甘肃平凉地区地震活动特征及其发震机理研究

Study on Seismicity Characteristics and Mechanism in Pingliang Area, Gansu Province

摘要:

针对2001年以来甘肃省平凉地区中小地震活动增强现象比较突出问题,通过遗传算法重新定位地震深度,利用矩张量反演方法反演震源机制解,并根据平凉地区地震时空分布特征、震相特征以及区域地质构造环境,认为平凉地区地震主要为煤矿诱发地震,可能发震机理为煤体压缩、顶底板拉伸、断层矿震等。

Abstract:

Since 2001, small -moderate seismicity has been increasing obviously in Pingliang area, Gansu province. In this paper, the focal depths are definited by the locating method based on genetic algorithm, the focal mechanism is calculated by the moment tensor inversion. According to seismic spatio-temporal distribution, seismic phase and regional geological structural environment, it is considered that the earthquakes in Pingliang area are mainly mining-induced earthquakes, and the kinds of initial mechanism are coal body compression, work face stretching and fault rockburst.