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| 汶川8.0地震地表破裂平通镇段的变形特征 | |
| 引用本文： | 何仲太,马保起,田勤俭,张世民.汶川8.0地震地表破裂平通镇段的变形特征[J].第四纪研究,2008,28(5):789-795. |
| 作者姓名： | 何仲太 马保起 田勤俭 张世民 |
| 作者单位： | 1. 中国地震局地壳应力研究所,北京,100085 2. 中国地震灾害防御中心,北京,100029 |
| 基金项目： | 中国地震局地壳应力研究所基本科研业务专项项目(2008年度)资助 |
| 摘 要： | 2008年5月12日14时28分04秒,四川省汶川县发生MS8.0大地震。发震断裂为龙门山断裂带,地震地表破裂带分布在北川-映秀断裂上的映秀-石坎子段和江油-灌县断裂上的磁峰-睢水段。平武县平通镇地表破裂现象典型,在T1和T2阶地上形成了地震断坎和裂缝。应用高精度GPSRTK技术对平通镇地震断坎及两侧作详细的地形测量,并测量了线性显著的路面中线和鱼塘西边壁。在室内生成高分辨率DEM与大比例尺地形剖面图,量取同震垂直与水平位移,并估算压缩缩短量和断层产状。结果显示汶川8.0级地震在平通镇形成的同震垂直位移为3.0±0.1m,右旋水平位移为4.0±0.2m,压缩缩短量为2.5m,断层产状为NE40°/NW∠50°。平通镇的同震右旋位移与本次地震的最大右旋位移相近,而逆冲垂直位移有所降低。 |
| 关 键 词： | 汶川8.0地震 龙门山断裂带 地表破裂 平通镇 GPS RTK 同震位移 |
| 收稿时间： | 2008-08-05 |
| 修稿时间： | 2008-08-17 |
DEFORMATION FEATURES OF SURFACE RUPTURE OF THE WENCHUAN EARTHQUAKE(M8.0)AT THE PINGTONG TOWN |
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| He Zhongtai,Ma Baoqi,Tian Qinjian,Zhang Shimin.DEFORMATION FEATURES OF SURFACE RUPTURE OF THE WENCHUAN EARTHQUAKE(M8.0)AT THE PINGTONG TOWN[J].Quaternary Sciences,2008,28(5):789-795. | |
| Authors: | He Zhongtai Ma Baoqi Tian Qinjian Zhang Shimin |
| Institution: | 1. The Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085; 2. China Earthquake Disaster Prevention Center, Beijing 100029 |
| Abstract: | On May 12,2008,a devastating M8.0 earthquake struck Wenchuan County,Sichuan Province.Its seismogenic structure is long the Longmenshan fault zone.Its surface rupture occurs on the Beichuan-Yingxiu and the Jiangyou-Guanxian faults with lengths of 200km and 70km,respectively.The surface rupture at the Pingtong town is a typical form,including co-seismic scarps and echelon fissures on T1and T2 terraces of the Ping River.We surveyed the rupture surface at the site with GPS RTK technique,especially the middle line of the road and the western wall of the fishpond for estimate the co-seismic displacement.We plotted high resolution DEM and large-scale topographic maps.From the DEM and the topographic map we can infer that the co-seismic vertical and strike-slip displacements are 3.0±0.1m and 4.0±0.2m,respectively.The compressed shortening is about 2.5m derived from calculating the original length of the western deformed fishpond wall.At Pington town,the attitude of the seismogenic fault is NE40°/NW∠50°.The strike-slip displacement at Pingtong town is close to the maximum co-seismic strike-slip displacements created by the earthquake,while the vertical one is smaller than the maximum co-seismic vertical displacement. |
| Keywords: | Wenchuan 8 0 Earthquake Longmenshan fault zone surface rupture Pingtong town GPS RTK co-seismic displacement |
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