华北地下释放氦、氢气体异常的时、空、强特征及其与地震关系的探讨  

RELATIONSHIP BETWEEN THE ANOMALOUS RELEASE OF SUBSURFACE HELIUM AND HYDROGEN GASSES AND THE THREE MAIN ELEMENTS OF EARTHQUAKE PREDICTION

作　　者：范树全[1] 宋贯一[1] 

机构地区：[1]国家地震局地质研究所,河北省地震局怀来地震台

出　　处：《地震地质》1996年第4期417-420,共4页Seismology and Geology

摘　　要：在系统整理华北９个气体观测井多年观测资料基础上，初步探讨了华北地下释放氦、氢异常的时、空、强特征及其与发震时间、地点、震级的关系，从而总结为以京棉二厂井的氦、氢异常为依据，其它测点的氦、氢异常为参考，预报华北北部５级以上地震的初步经验。Based on the measuing data from 9 observation points and the cases of 5 moderate earthquakes in North China during the time period from 1989 to 1991,the relationship between the anomaluos release of subsurface helium and hydrogen gasses and the occurrence time,locality and magnitude of earthquake has been discussed in this paper. An empirical method was proposed for determining the three main elements of earthquake prdeiction.It is proposed that the occurrence time of a possible earthquake can be predicted on basis of synchronus anomaly of helium and hydrogen in various observation points, and specially the dropping and truning of the curves of anomalies. The possible locality of earthquke occurrence can be delineated according to the fact that the starting time of the anomaly becomes later toward the epicentral area,i.e.the closer to the epicentral area,the later the starting time of the anomaly.The magnitude of the predicted earthquake can be estimated through the intensity (a combination of duration time and amplitade )and range of anomaly,as well as the number of the observation points that show anomalous release of helium and hydrogen gasses.

关 键 词：地震关系 氦 氢 气体异常 地震前兆 

分 类 号：P315.7[天文地球—地震学]