CAJ | 학술논문

通过对过去近半个世纪水库诱发地震资料的分析,认为水库诱发地震的诱发因素尽管复杂,但一些国内外水库诱发震例表明,水库诱发地震的断层响应现象是明显的,这种现象由水库诱发地震的非均匀分布性、集中呈带性、地震带与水库位置关系的非确定性、地震带沿库区某些断层展布等方面所反映.
통과대과거근반개세기수고유발지진자료적분석,인위수고유발지진적유발인소진관복잡,단일사국내외수고유발진례표명,수고유발지진적단층향응현상시명현적,저충현상유수고유발지진적비균균분포성、집중정대성、지진대여수고위치관계적비학정성、지진대연고구모사단층전포등방면소반영.
Reservoir-induced seismicity (RIS for short) is "the result from reservoir impounding. According to the re-search during past half century, the cause of RIS may be complex. However, based on the tectonic analysis of some RIS samples in the world and China, there existed obvious faulting response to RIS, which were shown as the heterogeneous distribution of the RIS epicenters, the RIS epicenters centralizing in a belt, the uncertain position relationship between the reservoir and RIS belt, and RIS belt being controlled by some faults in the reservoir area.