摘要
唐山等大地震地电阻率中期下降系压缩应变积累所致 ,为基线缩短、井水位下降所支持。地电阻率、自然电位对起潮力的异常响应及自然电位快急始、慢衰减特殊图象与废油井喷油同步等短临前兆 ,与中期前兆相反显示出向震中迁移的规律 ,表明能量积累从震中向外围传播 ,而能量释放从外围向震中传播。海城地震时喷砂冒水可引起自然电位垂直分量跃变及地光。IIMT法和过剩海洋电流H极化结果表明 ,唐山地震与地壳高阻层及其中存在深大断裂有关。
Resistivity measurement with an active source has been practised for thirty years at an enormous number of station in China. Resistivity decreases of several percent, which began 2～3 years prior to the Tangshan earthquake and other events and gradual increases afterward were observed. These anomalous variations were larger than their background fluctuations and hence statistically significant. Resistivity decreases were generally seen first and larger at stations close to epicenters and later and smaller at more distant stations. This implies that in the preseismic intermediate term stage, the fault was closed and the accumulated strain started first in the epicentral area and then migrated outwards from the epicentre. Anomalies in self-potential of the specific pattern of rapid onset and slow decay recorded at the station XZ are almost simultaneous with oil blowouts from the borehole W11. These short term or impending earthquake precursors migrated towards the epicentre, i.e., strain energy releasing occurred first at stations more distant to the epicentre, later at closer stations and at last the main shock took place. For short periods the industrial interference magnetotellurics (IIMT) determined that the Tangshan earthquake took place in the resistive crust. TM mode (H polarization) data at long periods of the MT measurements determined that electrical properties of resistive zone and the existence of a deep fault zone (fluid leakage paths) was found in resistive crust of the Tangshan earthquake area. Electrical measurements are the geophysical measurements most closely related to fluid volumes, connectivities and pressures, and applicable to earthquake prediction.
出处
《地震地质》
EI
CSCD
北大核心
2001年第2期277-285,共9页
Seismology and Geology
