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| 1 | Holocene activities of the Taigu fault zone, Shanxi Province, and their relations with the 1303 Hongdong M=8 earthquake显示文摘The Taigu fault zone is one of the major 12 active boundary faults of the Shanxi fault-depression system, located on the eastern boundary of the Jinzhong basin. As the latest investigation indicated, the fault zone had dislocated gully terrace of the first order, forming fault-scarp in front of the loess mesa. It has been discovered in many places in ground surface and trenches that Holocene deposits were dislocated. The latest activity was the 1303 Hongdong earthquake M=8, the fault appeared as right-lateral strike-slip with normal faulting. During that earthquake, the Taigu fault together with the Mianshan western-side fault on the Lingshi upheaval and the Huoshan pediment fault on the eastern boundary of the Linfen basin was being active, forming a surface rupture belt of 160 km in length. Moreover, the Taigu fault were active in the mid-stage of Holocene and near 7 700 aB.P. From these we learnt that, in Shanxi fault-depression system, the run-through activity of two boundary faults of depression-basins might generate great earthquake with M=8. | 谢新生 江娃利 王焕贞 冯西英 | 2004 | 地震学报2004，26，3： | 21 |
| 2 | 1303年山西洪洞8级地震地表破裂带显示文摘综合 2 0世纪 90年代初在霍山山前断裂和近年在绵山西侧断裂和太谷断裂获取的最新调查资料 ,讨论了 130 3年山西洪洞 8级地震地表破裂带的展布和位移特征 .如果太谷断裂、绵山西侧断裂与霍山山前断裂在 130 3年洪洞地震中同时活动 ,则该次地震的地表破裂带长16 3km ,分为 3段 ,即霍山山前断裂段、绵山西侧断裂段和太谷断裂段 .各段长度分别为 5 0 ,35和 70km ,3段之间存在 4和 8km的阶区 .该地震地表破裂带具右旋走滑特征 ,北段和中段右旋走滑位移量 6~ 7m ,南段最大为 10m .在山西断陷带盆地边界的单条断裂一般只对应 7级地震 ,而该次 8级特大地震则突破两个盆地之间的障碍体 。 | 江娃利 邓起东 徐锡伟 谢新生 | 2004 | 地震学报2004，26，4： | 16 |
| 3 | 1303年洪洞地震宏观震中修订的新证据显示文摘1303年9月25日的洪洞地震为依据文献资料确定的中国大陆内部第一个M8. 0地震,因其宏观震中与1695年临汾地震的宏观震中仅相距40km,且2者仅间隔392a而受到持续关注。文中对历史文献进行重新梳理并对震中区同震次生灾害进行系统解译研究,所得结果表明:1) 1303年洪洞地震的极震区包括临汾盆地,也包括太原盆地南部与灵石凸起,后者范围内严重破坏的建筑物的记载数量与临汾盆地相当,说明太原盆地南部与灵石凸起和临汾盆地一样在洪洞地震中遭遇同等或更加严重的破坏,而1695年临汾地震的极震区仅局限在临汾盆地内,且极震区位于洪洞以南; 2)位于灵石凸起上的1. 1万个黄土地震滑坡由1303年洪洞地震触发,基于文献震害记录和地震次生灾害的集中分布特征,建议将1303年洪洞地震的宏观震中从之前的洪洞附近(36. 3°N,111. 7°E)向北移动约60km,这样可以较合理地解释密集黄土地震滑坡与宏观震中的空间对应关系,新的宏观震中(36. 8°N,111. 7°E)位于霍州与灵石之间,同震滑坡加剧了极震区灾情的严重程度; 3)文中为重新认识山西地堑系中部2次重要历史强震的关系提供了新的证据和研究思路。 | 徐岳仁 何宏林 李文巧 张伟恒 田勤俭 | 2018 | 地震地质2018，40，5： | 11 |
| 4 | Surface rupture zone of the 1303 Hongtong M=8 earthquake, Shanxi Province显示文摘Based on the latest displacement of Huoshan piedmont fault, Mianshan west-side fault and Taigu fault obtained from the beginning of 1990's up to the present, the characteristics of distribution and displacement of surface rupture zone of the 1303 Hongtong M = 8 earthquake, Shanxi Province are synthesized and discussed in the paper. If Taigu fault, Mianshan west-side fault and Huoshan piedmont fault were contemporarily active during the 1303 Hongtong M = 8 earthquake, the surface rupture zone would be 160 km long and could be divided into 3 segments, that is, the 50-km-long Huoshan piedmont fault segment, 35-km-long Mianshan west-side fault segment and 70-km-long Taigu fault segment, respectively. Among them, there exist 4 km and 8 km step regions. The surface rupture zone exhibits right-lateral features. The displacements of northern and central segments are respectively 6~7 m and the southern segment has the maximum displacement of 10 m. The single basin-boundary fault of Shanxi fault-depression system usually corresponds to M ≈ 7 earthquake, while this great earthquake (M = 8) broke through the obstacle between two basins. It shows that the surface rupture scale of great earthquake is changeable. | JIANG Wa-li(江娃利) DENG Qi-dong(邓起东) XU Xi-wei(徐锡伟) XIE Xin-sheng(谢新生) | 2004 | Acta Seismologica Sinica(English Edition)2004，17，4： | 4 |
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