| 云南武定1995年地震余震尾波QC |
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| 引用本文： | 李白基,秦嘉政,谢庆茵,蔡绍平.云南武定1995年地震余震尾波QC[J].地震地磁观测与研究,2000,21(2):1-6. |
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| 作者姓名： | 李白基 秦嘉政 谢庆茵 蔡绍平 |
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| 作者单位： | 中国昆明,650041,中国地震局滇西地震预报实验场 |
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| 基金项目： | 中国地震局项目，95-04-05-02-02， |
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| 摘 要： | 用云南武定 1 995地震余震数字化记录测量了震源区尾波 QC(f) ,其值属构造运动活跃区类型。 6 Hz以上 ,云龙台 QC(f )逐渐低于田心台 QC(f) ,这是发窝 -插甸断裂破碎带非弹性吸收的结果
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| 关 键 词： | 尾波QC 非弹性吸收 云南武定 |
The Qc(f) of coda from the aftershocks of the 1995 Wuding earthquake in Yunnan Province |
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| Li Baiji,Qing Jiazheng,Xie Qingyin,Cai Shaoping.The Qc(f) of coda from the aftershocks of the 1995 Wuding earthquake in Yunnan Province[J].Seismological and Geomagnetic Observation and Research,2000,21(2):1-6. |
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| Authors: | Li Baiji Qing Jiazheng Xie Qingyin Cai Shaoping |
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| Abstract: | The Q c( f ) of coda at the source region has been estimated by using the digital recordings for the aftershocks of the 1995 Wuding earthquake,which is the type of tectonics.Above 6 Hz,the Q c( f ) of Yunlong station is gradually lower than that of Tianxin station,which is the consequence of nonelastic absorption in the fragmental zone of Fawo Chadian Fault. |
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| Keywords: | coda Q C nonelastic absorption Wuding in Yunnan Province |
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