上海地震台阵与台网的定位及视慢度研究  

The Research on the Apparent Slowness and the Location of Seismographic Network and Seismological Array Station in Shanghai

作　　者：任隽[1] 朱元清[2] 潘纪顺[1] 陈运平[1] 

机构地区：[1]中国科学技术大学地球和空间科学系 [2]上海市地震局,上海200062

出　　处：《地震研究》2002年第4期335-340,共6页Journal of Seismological Research

摘　　要：阐述了台阵的地震定位原理和视慢度在台阵与台网定位中的一些重要特性 ,并比较了相同位置上的上海地震台阵与台网对同一地震的定位结果。最后 。The principle of earthquake location by way of seismological array station is discussed.Some important characteristics of apparent slowness used in the earthquake locations by seismological array station and by seismographic network in Shanghai are discussed too.Furthermore,taking the earthquake as a sample,the location made by seismological array station is compared with the location made by seismographic network.Finally,the vector-correction value of the area and range where the transverse velocity changes is given and discussed.It is the transverse vector-correction which causes the error between the location made by seismological array station and the location made by seismographic network.

关 键 词：台阵标定 视慢度 波阵面法 上海地震台阵 地震台网 

分 类 号：P315.75[天文地球—地震学] P315.78[天文地球—固体地球物理学]