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渭河断陷及邻近地区地壳S波速度图象
引用本文:袁志祥,丁韫玉,狄秀玲.渭河断陷及邻近地区地壳S波速度图象[J].地震地质,1999,21(1):9-11.
作者姓名:袁志祥  丁韫玉  狄秀玲
作者单位:陕西省地震局,地震研究所,西安,710068
摘    要:选取104~112°E,32.5~38°N区域内陕西、山西、河南、湖北、甘肃、宁夏等省区的区域地震台网1984~1993年的1946个天然地震的S波观测资料,用地震层析成像方法反演了渭河断陷及其邻近地区的地壳S波速度图象,其结果表明地壳深部S波速度结构的不均匀性与该区大地构造单元、断裂构造及地震活动密切相关

关 键 词:渭河地堑系  地震层析成像  S波  波速构造

THE CRUSTAL SEISMIC S WAVE VELOCITY IMAGE IN THE WEIHE DOWNFAULTED BASIN AND ITS ADJACENT AREAS
Yuan Zhixiang,Ding Yunyu,Di Xiuling.THE CRUSTAL SEISMIC S WAVE VELOCITY IMAGE IN THE WEIHE DOWNFAULTED BASIN AND ITS ADJACENT AREAS[J].Seismology and Geology,1999,21(1):9-11.
Authors:Yuan Zhixiang  Ding Yunyu  Di Xiuling
Abstract:The S wave data are selected from the records of 1 946 earthquakes observed in the period from 1984 to 1993 by seismic network in the zone of 104~112°E, 31.5~38°N in Shaanxi, Shanxi, Henan, Hubei, Gansu and Ningxia Provinces.The S wave velocity image of the crust beneath the Weihe downfaulted basin and adjacent areas is obtained by means of seismic tomographic technique. The results show that the non uniform S wave velocity structure of deep crust is closely related to the difference of geotectonic ele
Keywords:Weihe graben system  Seismic tomography  S  wave  Velocity structure  
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