| 尖扎渡口一隆务河口断裂带活动性初步研究 |
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| 引用本文： | 姚生海,黄伟.尖扎渡口一隆务河口断裂带活动性初步研究[J].高原地震,2013,25(2):31-34. |
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| 作者姓名： | 姚生海 黄伟 |
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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： | 尖扎盆地发育一组近南北向断裂带，即尖扎渡口—隆务河口断裂带。通过对该断裂带野外调查，表明该断裂带长约20km，为逆冲断层，最新活动为早中更新世，晚更新世以来未见活动。
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| 关 键 词： | 坳陷 隆起 断裂带 活动性 |
PRELIMINARY RESEARCH ON JIANZA FERRY-LONGWU ESTUARY FAULT ACTIVITY |
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| YAO Shenghai
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HUANG Wei.PRELIMINARY RESEARCH ON JIANZA FERRY-LONGWU ESTUARY FAULT ACTIVITY[J].Plateau Earthquake Research,2013,25(2):31-34. |
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| Authors: | YAO Shenghai HUANG Wei |
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| Institution: | ( Earthquake Administration of Qinghai Province, Xining 810001, China) |
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| Abstract: | The Jianza basin developed a group of nearly north-south trending faults, which was Jianzha ferry- Longwuhe estuary fracture. Field investigation of this fracture, it is found that the fault is about 20 km long, they are thrust faults, and their activity was about in the early Pleistocene, and no activities since the late Pleis- tocene. |
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| Keywords: | Depression Apophysis Fault Activity |
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