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| 1 | Jurassic Tectonic Revolution in China and New Interpretation of the “Yanshan Movement”显示文摘摘要:与结构的地质的调查的新数据和高分辨率的同位素的标明日期数据的获得和累积,我们极大地改进了我们从迟了的侏罗记在时期期间发生在东方中国到早白垩纪的构造事件的理解并且可以给性质的新解释,预定并且 Yanshan 运动的 geodynamic 背景。在中间迟了的侏罗记期间(165 挠慬獳漠 ?? | DONG Shuwen ZHANG Yueqiao LONG Changxing YANG Zhenyu JI Qiang WANG Tao HU Jianmin CHEN Xuanhua | 2008 | Acta Geologica Sinica(English Edition)2008，82，2： | 41 |
| 2 | Seismogenic Structure around the Epicenter of the May 12,2008 Wenchuan Earthquake from Micro-seismic Tomography显示文摘一个三维的本地规模的 P 速度模型在下面到 25 km,在主要吃惊震中区域附近的深度用从 5856 余震的地震光线由一个最新部署的暂时的地震网络记录了的 83821 event-to-receiver 被构造。棋盘测试证明我们的 tomographic 模型有 ∼2 km 的侧面、垂直的分辨率。高分辨率的 P 速度模型在 seismogenic 层揭示了有趣的结构:(1 ) Guanxian-Anxian 差错, Yingxiu-Beichuan 差错和 Longmen 掸人差错地区的 Wenchuan-Maoxian 差错好由突然地上面的外壳的速度变化描出;(2 ) Pengguan 山岳比它的包围区域有通常更高的速度,并且可以延长在下面到从表面的至少 ∼10 km;(3 ) 在 Wenchuan-Maoxian 差错下面的一个突然地侧面的速度变化可以显示 Pengguan 山岳的西方的边界或 Wenchuan-Maoxian 差错是垂直的,并且 Wenchuan 地震的低亚硫酸钠中心可能在蘸 Yingxiu-Beichuan 和 Guanxian-Anxian 差错,和垂直 Wenchuan-Maoxian 差错的 NW 的连词点定位;(4 ) 沿着 Yingxiu-Beichuan 差错的附近被很低的速度和低 seismicity 在浅深度描绘,可能由于孔和破裂的高内容;(5 ) 二块低速度的异例分别地与 ∼5 km 与 ∼7 km 偏移量在挂的墙和 Guanxian-Anxian 差错的脚墙中被想象垂直部件。 | AN Meijian FENG Mei DONG Shuwen LONG Changxing ZHAO Yue YANG Nong ZHAO Wenjin ZHANG Jizhong | 2009 | Acta Geologica Sinica(English Edition)2009，83，4： | 7 |
| 3 | Co-seismic Faults and Geological Hazards and Incidence of Active Fault of Wenchuan Ms 8.0 Earthquake,Sichuan,China显示文摘There are two co-seismic faults which developed when the Wenchuan earthquake happened. One occurred along the active fault zone in the central Longmen Mts.and the other in the front of Longmen Mts.The length of which is more than 270 km and about 80 km respectively.The co-seismic fault shows a reverse flexure belt with strike of N45°-60°E in the ground,which caused uplift at its northwest side and subsidence at the southeast.The fault face dips to the northwest with a dip angle ranging from 50°to 60°.The vertical offset of the co-seismic fault ranges 2.5-3.0 m along the Yingxiu-Beichuan co-seismic fault,and 1.5-1.1 m along the Doujiangyan-Hanwang fault.Movement of the coseismic fault presents obvious segmented features along the active fault zone in central Longmen Mts. For instance,in the section from Yingxiu to Leigu town,thrust without evident slip occurred;while from Beichuan to Qingchuan,thrust and dextral strike-slip take place.Main movement along the front Longmen Mts.shows thrust without slip and segmented features.The area of earthquake intensity more thanⅨdegree and the distribution of secondary geological hazards occurred along the hanging wall of co-seismic faults,and were consistent with the area of aftershock,and its width is less than 40km from co-seismic faults in the hanging wall.The secondary geological hazards,collapses,landslides, debris flows et al.,concentrated in the hanging wall of co-seismic fault within 0-20 km from co-seismic fault. | MA Yinsheng LONG Changxing TAN Chengxuan WANG Tao GONG Mingquan LIAO Chunting WU Manlu SHI Wei DU Jianjun PAN Feng | 2009 | Acta Geologica Sinica(English Edition)2009，83，4： | 7 |
| 4 | Seismogenic Tectonics and Dynamics of the 2011 Ms5.9 Yingjiang Earthquake in Yunnan, China显示文摘在南部的南方北方地震地区,中国,在西方的云南的 Yingjiang 区域的地震活动从 2010 年 12 月增加了,并且最后, Ms5.9 的破坏地震在 2011 年 3 月 10 日发生在 Yingjiang 镇附近。焦点的机制和 mainshock 的 hypocenter 地点建议 Dayingjiang 差错是 mainshock 破裂的地点。然而,大多数前震和定位的一个便携式的地震数组记录的所有余震关门到 mainshock 沿着 N-S-striking Sudian 差错发生了,显示这个差错在这些上有重要影响震惊。库仑压力计算显示出那三强壮(大小 ≥5.0 ) 在 2008 发生在学习区域的地震沿着飞机平行增加了库仑压力到 Dayingjiang 差错。这支持 Dayingjiang 差错,和并非 Sudian 差错,作为 2011 Ms5.9 Yingjiang 地震的 seismogenic 差错。在 2008 的强烈地震也沿着全部 Sudian 差错在 ≤5 km 的深度增加了库仑压力,并且那么沿着差错由做增加了浅地震活动。这解释 2011 Yingjiang 地震的前震和余震为什么主要位于它切浅外壳的 Sudian 差错。在 Sudian 和 Dayingjiang 差错的交叉的地震沿着在 ∼40° 蘸到东南的一条带主要是分布式的,建议在 mainshock 区域的 Dayingjiang 差错也蘸到在 ∼40° 的东南。 | SUN Yao AN Meijian FENG Mei LONG Changxing YANG Zhenyu | 2014 | Acta Geologica Sinica(English Edition)2014，88，2： | 3 |
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