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南阳盆地特殊震相研究
引用本文:王林昌,王勉,王晓谦,张予川,刘东欣,刘晓东.南阳盆地特殊震相研究[J].高原地震,2011,23(3):30-33.
作者姓名:王林昌  王勉  王晓谦  张予川  刘东欣  刘晓东
作者单位:1. 河南省南阳地震台,河南南阳,473000
2. 河南省南阳市地震局,河南南阳,473061
摘    要:南阳盆地内发生的地震在仪器记录图上与其他地震波形有所不同,在直达横波正常出现后立即开始衰减,紧接着二次出现大振幅、大周期波形。对此进行了分析,证明在南阳地区地壳中存在一个硬度较大的界面,地震波到达该界面时发生反射,反射波与直达波叠加,即出现了第二个较大振幅的波形。

关 键 词:南阳盆地  特殊震相  波形异常

STUDY ON THE SPECIAL SEISMIC PHASES IN NANYANG BASIN
WANG Linchang,WANG Mian,WANG Xiaoqian,ZHANG Yuchuan,LIU Dongxin,LIU Xiaodong.STUDY ON THE SPECIAL SEISMIC PHASES IN NANYANG BASIN[J].Plateau Earthquake Research,2011,23(3):30-33.
Authors:WANG Linchang  WANG Mian  WANG Xiaoqian  ZHANG Yuchuan  LIU Dongxin  LIU Xiaodong
Institution:WANG Linchang1,WANG Mian2,WANG Xiaoqian2,ZHANG Yuchuan2,LIU Dongxin2,LIU Xiaodong1 (1.Nanyang Seismic Station,Henan Province,Nanyang 473000,China,2.Earthquake Administration of Nanyang City,Nanyang 473061,China)
Abstract:The earthquake waves in Nanyang Basin are different from other areas,the S wave attenuated as soon as it arrived,and then appeared large amplitude and periodic wave.The big hard interface was found in Nanyang crust,and the seismic waves were reflected when they reached there,so the second large amplitude waves appeared when the reflected wave and S wave were superposed.
Keywords:Nanyang Basin  Special seismic phase  Wave anomaly  
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