| 2013年云南香格里拉、德钦-四川得荣交界5.9级地震灾害及发震构造 |
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| 引用本文： | 杨捷,曾佐勋,李茂华,房艳国,谭朝爽,吴世泽,龚成.2013年云南香格里拉、德钦-四川得荣交界5.9级地震灾害及发震构造[J].地球科学,2015,40(10):1701-1709. |
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| 作者姓名： | 杨捷 曾佐勋 李茂华 房艳国 谭朝爽 吴世泽 龚成 |
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| 作者单位： | 1.中国地质大学地球科学学院, 湖北武汉 430074 |
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| 基金项目： | 国家自然科学基金重点项目41230206 |
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| 摘 要： | 2013年8月28日、31日, 云南迪庆藏族自治州香格里拉县、德钦县、四川省甘孜藏族自治州得荣县交界地区连续发生5.1级、5.9级地震.为了查明此次地震的影响破坏程度, 进行了地震现场建筑物震害考察并对震中附近断裂进行了野外构造地质剖面调查.两次地震在短时间内并在相近位置连续发生, 造成了此次云南香格里拉、德钦-四川得荣交界地震比以往同级地震的破坏程度要高, 地震烈度最高为Ⅷ级, 有感范围大, 5.9级地震宏观震中大致处在整个灾区破坏最严重的奔子栏镇争古村一带(28.20°N, 99.36°E), 距离地震微观震中约5.1km.等震线沿德钦-中甸断裂呈北西向分布, 近似为椭球状, 结合此次地震震中附近区域现场断裂调查、震源机制解数据以及地震余震空间分布特征, 初步推断此次地震的发震构造为德钦-中甸断层, 其主要表现为一次以正断为主兼有左旋走滑错动的地震事件.
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| 关 键 词： | 云南香格里拉、德钦-四川得荣交界地震 地震灾害 德钦-中甸断裂 发震构造 天然地震. |
| 收稿时间： | 2014-12-15 |
The Seismo-Geological Hazards and Seismogenic Structure of the 2013 Deqing-Derong 5.9 Earthquake |
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| Abstract: | On August 28st and 31st, 2013, two earthquakes with magnitude of 5.1 and 5.9 occurred on the boundary between Deqing County, Yunnan Province, and Derong County, Sichuan Province. In order to evaluate the damage of the earthquake, we investigated on lots of seismo-geological hazards induced by the earthquakes and conducted the field investigation of geological structural section about the fractures near the epicenter. Those two earthquakes successively occurring at the adjacent position led to the intensity of this earthquake higher than that of the same magnitude. The maximum intensity of the 5.9 earthquake is Ⅷ degree and the perceptible area is relatively large. The macroseismic epicenter is about 5.1km from the 5.1 microseismic epicenter is roughly located at the middle of the two microseismic epicenter (28.20°N, 99.36°E). The isoseismic line is shaped as an anomalous ellipse and the orientation of its long axis is NW-SE orientation along the Deqin-Zhongdian fault. According to the field investigation of geological structural section about the fractures near the epicenter, the focal mechanism solution data and the special distribution characteristics of the aftershocks, we preliminary infer that the seismogenic structure is Deqin-Zhongdian fault and the Deqing-Derong 5.9 earthquake is a normal fault type earthquake characterized by strike-slip. |
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