| 利用反射横波测定震源深度 |
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| 引用本文： | 蒋维强,王迪洁.利用反射横波测定震源深度[J].华南地震,1999,19(4):22-27. |
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| 作者姓名： | 蒋维强 王迪洁 |
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| 作者单位： | 广东省地震局,广东,广州,510070 |
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| 摘 要： | 提出了联合使用反射波横波Ｓ１１，Ｓｉｌ，Ｓｉ２在地震台网较疏的地区求解地震震源深度的原理和方法，并以新丰江水库区１２次地震为例，对该方法的结果进行检验。结果表明，利用反射皮法测定的震源深度与新丰江遥测台网的测定结果吻合较好。
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| 关 键 词： | 震源深度测定 反射波 反射横波 新丰江遥测地震台网 |
| 文章编号： | 1001-8662(1999)04-0022-07 |
| 修稿时间： | 1999－07－05 |
Determination of focal depth by reflected transverse waves |
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| JIANG Wei-qiang,WANG Di-jie.Determination of focal depth by reflected transverse waves[J].South China Journal of Seismology,1999,19(4):22-27. |
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| Authors: | JIANG Wei-qiang WANG Di-jie |
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| Abstract: | A method for determining the depth of seismic focus in the area that has thin seismic network with reflected transverse waves S 11 , S i 1 and S i 2 is proposed in this paper. The method is tested by using 12 earthquakes in Xinfeng jiang reservoir region. The results show that the depth of 12 events determined by the method are agree well with the results (the error range is 1 km)determined by Xinfengjiang redio linked seismic network. |
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| Keywords: | Focal depth determination Reflected wave Reflected transverse wave Xinfengjiang redio-linked seismic network |
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