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上海地震台阵与台网的定位及视慢度研究
引用本文:任隽,朱元清,潘纪顺,陈运平.上海地震台阵与台网的定位及视慢度研究[J].地震研究,2002,25(4):335-340.
作者姓名:任隽  朱元清  潘纪顺  陈运平
作者单位:1. 中国科学技术大学地球和空间科学系,合肥,230026;陕西省地震局,西安,710068
2. 上海市地震局,上海,200062
3. 中国科学技术大学地球和空间科学系,合肥,230026
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,对上海台队与台网导致定位误差的横向速度变化的位置和范围给出了矢量校正的结果并进行了初步讨论。

关 键 词:台阵标定  视慢度  波阵面法  上海地震台阵  地震台网

The Research on the Apparent Slowness and the Location of Seismographic Network and Seismological Array Station in Shanghai
Ren Jun , Zhu Yuanqing Pan Jishun Chen Yunping.The Research on the Apparent Slowness and the Location of Seismographic Network and Seismological Array Station in Shanghai[J].Journal of Seismological Research,2002,25(4):335-340.
Authors:Ren Jun  Zhu Yuanqing Pan Jishun Chen Yunping
Institution:Ren Jun 1,3 Zhu Yuanqing 2 Pan Jishun 1 Chen Yunping 1
Abstract: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.
Keywords:Calibration of array station  apparent slowness  wave front method  shanghai seismological array station  
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