| 上拉秀一小苏莽断裂带新活动特征与地震关系探讨 |
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| 引用本文： | 何岗,张兴.上拉秀一小苏莽断裂带新活动特征与地震关系探讨[J].高原地震,2013(3):22-24. |
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| 作者姓名： | 何岗 张兴 |
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| 作者单位： | 青海省地震局,青海西宁810001 |
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| 摘 要： | 青海省玉树县上拉秀乡至小苏莽乡曾发生过多次中强地震，由于震级不高、危害不大及条件所限，未能进行详细的野外地质调查，只是初步判断上拉秀-小苏莽断裂带为全新世活动断裂带，为多次中强地震的发震构造。
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| 关 键 词： | 活动断裂带 发震构造 玉树 |
DISCUSSION ON THE RELATIONSHIP BETWEEN ACTIVE CHARACTERISTICS AND EARTHQUAKES IN SHANGLAXIU-XIAOSUMANG FAULT ZONE |
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| HE Gang,ZHANG Xing.DISCUSSION ON THE RELATIONSHIP BETWEEN ACTIVE CHARACTERISTICS AND EARTHQUAKES IN SHANGLAXIU-XIAOSUMANG FAULT ZONE[J].Plateau Earthquake Research,2013(3):22-24. |
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| Authors: | HE Gang ZHANG Xing |
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| Institution: | (Earthquake Administration of Qinghai Province, Xining 810001, China) |
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| Abstract: | Many middle-strong earthquakes occurred in Shanglaxiu-Xiaosumang fault zone in Yushu county, Qinghai province. Because of the lower magnitudes and harmless, the detailed field geological investigation could not be made,it was preliminarily determined that this fault was holocene active fault, it was also seis- mogenic structure of middle-strong earthquakes. |
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| Keywords: | Active fault zone Seismogenic structure Yushu |
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