| 汶川地震地表破裂线上之古地震研究(英文) |
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| 引用本文： | 陈文山,Yong Kang Ran,Xiwei Xu.汶川地震地表破裂线上之古地震研究(英文)[J].国际地震动态,2010(6):27-27. |
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| 作者姓名： | 陈文山 Yong Kang Ran Xiwei Xu |
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| 作者单位： | 陈文山,Wen Shan Chen(Department of Geosciences, Taiwan University, Taipei 10617);Yong Kang Ran,Xiwei Xu,Yong Kang Ran,Xiwei Xu(Institute of Geology, CEA, Beijing 100029) |
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| 摘 要： | The May 12, 2009 MW8.0 Wenchuan earthquake brought nearly 300 km in length surface ruptures along the frontal Longmenshan orogenic belt where occurred the largest natural disaster in western Sichuan, China. The orogenic belt consists of a series of subparallel thrust faults of Wenchuan-Maoxian, Beichuan and Pengguan faults, which form an east-verging fold-thrust belt.
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Holocene paleoearthquake activity along the 2008 Wenchuan earthquake ruptures of the Beichuan and Pengguan faults |
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| Wen Shan Chen,Yong Kang Ran,Xiwei Xu.Holocene paleoearthquake activity along the 2008 Wenchuan earthquake ruptures of the Beichuan and Pengguan faults[J].Recent Developments in World Seismology,2010(6):27-27. |
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| Authors: | Wen Shan Chen Yong Kang Ran Xiwei Xu |
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| Institution: | 1. Department of Geosciences, Taiwan University, Taipei 10617
2. Institute of Geology, CEA, Beijing 100029 |
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| Abstract: | The May 12, 2009 MW8.0 Wenchuan earthquake brought nearly 300 km in length surface ruptures along the frontal Longmenshan orogenic belt where occurred the largest natural disaster in western Sichuan, China. The orogenic belt consists of a series of subparallel thrust faults of Wenchuan-Maoxian, Beichuan and Pengguan faults, which form an east-verging fold-thrust belt. |
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