BASIC CHARACTERISTICS OF THE MAIN ACTIVE FAULTS AND SEISMIC ACTIVITIES IN PAN YANGTZE RIVER DELTA REGION
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摘要: 在系统收集整理前人成果资料基础上，结合基础地质和遥感解译，对泛长三角地区的主要活动断裂及其活动性进行了全面梳理和分析，并根据区域主要断裂的活动性与历史地震活动特征，进一步分析指出了该区需要特别关注的潜在震源区和地壳稳定性相对较差的区域。研究结果表明，该区主要发育38条活动性相对显著的活动断裂带，并以北东和北西走向两组活动断裂为主，前者以右旋走滑活动为主，后者以左旋走滑活动为主；其次为近东西走向，活动性较弱。进一步结合历史地震活动信息分析发现，其中的北东/北北东向断裂是区域上主要的控震构造和发震断层，其次是北西向断裂，这两组不同走向断裂带的交汇部位常常是地震发生部位，其中最显著的控震断裂是北东向的郯庐断裂与北西向的无锡-宿迁断裂。Abstract: On the basis of systematically collecting and sorting the data of predecessors' achievements, and combination of basic geology and remote sensing interpretation, we comprehensively analyzed and sorted out the main active faults and their activity in Pan-Yangtze River Delta region. According to the main regional faults and the activity of historical earthquakes, this paper further analyzed, and pointed out the potential focal region that needs special attention and region of relatively poor crustal stability in this area. The research results show that, there are 38 active faults with relatively strong activity, mainly being in the directions of northeast and northwest. The former mainly on right lateral strike slip activity, the later mainly on left lateral strike slip activity. Then east-west faults with poor activity followed. Furthermore, combining the information of historical earthquake activity, we find that the convergence position of the two groups of fault zone with different directions are often the sites of earthquake occurrence. The most prominent controlled earthquake faults are northeast-orientational Tanlu fault and northwest-orientational Wuxi-Suqian fault.
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图 1 研究区位置与地质环境条件
Figure 1. Location and geological environmental conditions of the study area
图 2 泛长三角地区主要活动断裂与地震分布
F1—郯庐断裂；F2-1—陈家堡-小海断裂；F2-2—茅山断裂；F2-3—金坛-南渡断裂；F2-4—江南断裂；F2-5—葛公断裂；F3-1—奉贤-南汇断裂；F3-2—马金-乌镇断裂；F3-3—萧山-球川断裂；F3-4—江山-绍兴断裂；F4-1—镇海-温州断裂；F4-2—丽水-余姚断裂；F5-1—无锡-宿迁断裂；F5-2—南通-嘉宁断裂；F6-1—涡河断裂；F6-2—南京-湖熟断裂；F7-1—颖上-定远断裂；F7-2—肥中断裂；F8-1—青山-晓天断裂；F8-2—梅山-龙河口断裂；F9-1—幕府山-焦山断裂；F9-2—栟茶河断裂；F9-3—昌化-普陀断裂；F10-1—宿北断裂；F10-2—太河-五河断裂；F10-3—临泉-刘府断裂；F10-4—六安-合肥断裂；F10-5—肥西-韩摆渡断裂；F10-6—滁河断裂；F10-7—乌江-罗昌河断裂；F10-8—六合-马鞍山断裂；F10-9—南陵-小丹阳断裂；F10-10—淮阴-响水断裂；F10-11—洪泽-流均沟断裂；F10-12—盐城断裂；F10-13—王老人集断裂；F10-14—固镇-怀远断裂；F10-15—落儿岭-土地岭断裂
(地震资料来源于中国地震台网数据；震源机制来源于文献[35, 37]；断裂资料来源于地质志及地震监测志[1~6])Figure 2. Distributions of the main active faults and earthquakes in the Pan-Yangtze River Delta region
图 3 泛长三角地区1300年以来M≥5.0级地震强度-时间分布图(M-T图)
Figure 3. Intensity-time map of earthquakes with M≥5.0 in Pan-Yangtze River Delta region
表 1 泛长三角地区主要断裂带及其特征一览表
Table 1. Main active faults and their activities in the Pan-Yangtze River Delta region
断裂带名称及编号 断裂
编号断裂基本属性 活动性 最新活动时代 断裂名称 长度/km 走向 运动性质 郯庐断裂带(F1) F1 郯庐断裂 570 NNE 右旋逆冲 强烈 晚更新世 扬州—南京—江南
断裂带(F2)F2-1 陈家堡—小海断裂 100 NE 正断层 弱 全新世 F2-2 茅山断裂 97 NE 右旋走滑 中等 晚更新世 F2-3 金坛—南渡断裂 80 NNE 右旋走滑 中等 晚更新世 F2-4 江南断裂 260 NE 右旋断层 中等 晚更新世 F2-5 葛公断裂 90 NNE 左旋走滑 弱 上海—杭州断裂带(F3) F3-1 奉贤—南汇断裂 150 NE 右旋走滑 弱 早更新世 F3-2 马金—乌镇断裂 弱 F3-3 萧山—球川断裂 164 NE 右旋走滑 弱 中更新世 F3-4 江山—绍兴断裂 380 NE 右旋走滑 弱 晚更新世 镇海—温州断裂带(F4) F4-1 镇海—温州断裂 270 NE 右旋逆冲 弱 中更新世 F4-2 丽水—余姚断裂 325 NE 右旋走滑 弱 晚更新世 苏州—徐州北西向
断裂带(F5)F5-1 无锡—宿迁断裂 300 NE 左旋走滑 中等 F5-2 南通—嘉宁断裂 189 NW 左旋走滑 弱 中更新世 杭州—南京—亳州
断裂带(F6)F6-1 涡河断裂 150 NW 左旋走滑 弱 晚更新世 F6-2 南京—湖熟断裂 NW 左旋走滑 弱 晚更新世 肥中断裂带(F7) F7-1 颖上—定远断裂 160 NWW 左旋走滑 弱 全新世 F7-2 肥中断裂 300 NWW 左旋走滑 弱 全新世 霍山断裂带(F8) F8-1 青山—晓天断裂 NW 左旋走滑 弱 全新世 F8-2 梅山—龙河口断裂 NWW 左旋走滑 弱 近东西向断裂系(F9) F9-1 幕府山—焦山断裂 EW 弱 全新世 F9-2 栟茶河断裂 EW 正断层 弱 全新世 F9-3 昌化—普陀断裂 290 EW 弱 更新世 其他断裂(F10) F10-1 宿北断裂 EW 弱 F10-2 太河—五河断裂 EW 弱 F10-3 临泉—刘府断裂 NWW 弱 F10-4 六安—合肥断裂 EW 弱 F10-5 肥西—韩摆渡断裂 NWW 弱 F10-6 滁河断裂 NE 弱 F10-7 乌江—罗昌河断裂 弱 F10-8 六合—马鞍山断裂 65 NNE 右旋走滑 不明显 更新世 F10-9 南陵—小丹阳断裂 NE 右旋走滑 弱 F10-10 淮阴—响水断裂 214 NE 弱 更新世 F10-11 洪泽—流均沟断裂 230 EW 正断层 弱 更新世 F10-12 盐城断裂 F10-13 王老人集断裂 340 NNE 中等 F10-14 固镇—怀远断裂 F10-15 落儿岭—土地岭断裂 NE 注：断裂资料来源于地质志及地震监测志[1~6] 
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表 2 泛长三角地区5.0级以上地震及其特征一览表
Table 2. Earthquakes with M≥5 and their characteristics in the Pan-Yangtze River Delta region
地震名称 时间 震级 宏观震中 最大烈度 等震线长轴方向 相关断裂 安徽寿县地震 294-07 5½ 安徽寿县 Ⅶ 颍上—定远断裂 江苏徐州地震 925-11-18 5¾ 江苏徐州西北 江苏常州地震 999-10 5½ 江苏常州 Ⅶ 安徽霍山地震 1336-01-20 5¼ 安徽霍山西南 NE 梅山-龙河口断裂和落儿岭-土地岭断裂 安徽六安地震 1425-03-16 5¾ 安徽六安 Ⅶ NE(?) 韩摆渡—肥西断裂西侧 安徽毫州地震 1481-03-18 6.0 安徽毫州 NW 涡河断裂 安徽天长地震 1491-09-23 5.0 安徽天长 江苏苏州地震 1524-03-29 5½ 江苏苏州西 安徽凤阳地震 1525-10-12 5.5 安徽凤阳西北 Ⅶ NW(?) 临泉—刘府断裂 安徽灵璧地震 1537-05-23 5½ 安徽灵璧 Ⅶ 宿北断裂 江苏邳县寨山地震 1546-09-29 5.5 江苏邳县 Ⅶ 安徽巢县地震 1585-03-06 5¾ 安徽巢县南 Ⅶ NE 枞阳—当涂断裂与汤沟一高淳断裂 江苏南通狼山地震 1615-03-01 5.0 江苏南通狼山镇 Ⅵ NW 南通-嘉定断裂 江苏扬州地震 1624-02-10 6.0 江苏扬州苏南 Ⅷ NE 陈家堡—小海断裂或茅东断裂北段(？) 江苏盱眙地震 1642-11-20 5.0 江苏盱眙 Ⅵ 安徽凤阳地震 1644-02-08 5.5 安徽凤阳 Ⅶ 安徽霍山地震 1652-02-10 5.5 安徽霍山 安徽霍山地震 1652-03-23 6.0 霍山东北 Ⅷ NW 梅山—龙河口断裂和落儿岭—土地岭断 安徽庐江地震 1654-02-17 5¼ 安徽庐江东南 安徽合肥地震 1673-03-29 5.0 安徽合肥 Ⅵ 合肥—六安断裂 江苏溧阳地震 1679-12-26 5¼ 江苏溧阳 Ⅶ 江苏仪征地震 1712-12-22 5.0 江苏仪征 江苏昆山南地震 1731-11 5.0 江苏昆山南 Ⅵ 安徽泾县地震 1743-06-30 5.0 江苏泾县 Ⅵ—Ⅶ 江南断裂与青弋江断裂交汇 安徽霍山地震 1770-01-16 5¾ 安徽霍山 NW(?) 安徽凤台地震 1831-09-28 6¼ 安徽凤台 Ⅷ NW 固镇一风台和临泉一刘府断裂交汇 江苏宜兴地震 1839-10-12 5.0 江苏宜兴 Ⅵ 安徽定远地震 1868-10-30 5.5 安徽定远 江苏太湖地震 1872-09-21 5.5 江苏太湖 江苏镇江地震 1913-04-03 5.5 江苏镇江 Ⅶ 安徽霍山地震 1917-01-24 6¼ 安徽霍山 Ⅷ NNE 桐柏-磨子潭断裂与落儿岭-土地岭断裂 安徽霍山地震 1917-02-22 5.5 安徽霍山 江苏镇江地震 1930-01-03 5.5 江苏镇江 Ⅶ 安徽霍山地震 1934-03-18 5.0 安徽霍山 安徽合肥地震 1954-06-17 5½ 安徽合肥 江苏溧阳地震 1974-04-22 5.5 江苏溧阳 Ⅶ NE 茅东断裂或金坛南渡断裂 江苏溧阳地震 1979-07-09 6.0 江苏溧阳 Ⅷ NE 茅东断裂或金坛—南渡断裂 江苏常熟地震 1990-02-10 5.1 江苏太仓 Ⅵ NE 注：地震资料来源于中国地震台网数据
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表 3 地震活动期划分简表
Table 3. Division of seismic activity periods
活动期 地震活动期 起止年份 时间间隔/a 地震次数 最大震级Ms Ⅰ
(1300—1679)平静期
活跃期1300—1480
1481—1679180
1982
165.0
6.0Ⅱ
(1680—2000)平静期
活跃期1680—1803
1804—2000123
1964
135.0
6¼
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[1] 安徽省地质矿产局.安徽省区域地质志[M].北京:地质出版社, 1987Bureau of Geology and Mineral Resources of Anhui Province. Regional geology of Anhui province[M]. Beijing:Geological Publishing House, 1987. [2] 江苏地质矿产局.江苏省及上海市区域地质志[M].北京:地质出版社, 1984:1~10Bureau of Geology and Mineral Resources of Jiangsu Province. Regional geology of Jiangsu Province and Shanghai City[M]. Beijing:Geological Publishing House, 1984:1~10. [3] 浙江省地质矿产局.浙江省区域地质志[M].北京:地质出版社, 1989Bureau of Geology and Mineral Resources of Zhejiang Pprovince. Regional geology of Zhejiang Province[M]. Beijing:Geological Publishing House, 1989. [4] 朱煌武.安徽省地震监测志[M].合肥:安徽大学出版社, 2004ZHU Huang-wu. Anhui earthquake monitoring[M]. Hefei:Anhui University Press, 2004. [5] 江苏省地震局.江苏省地震监测志[M].南京:河海大学出版社, 2008Series of Seismological Bureau of Jiangsu Province. Seismological monitoring of Jiangsu Province[M]. Nanjing:Publishing House of Hehai University, 2008. [6] 陈学庭.浙江省地震监测志[M].北京:地震出版社, 2004CHEN Xue-ting. Seismological monitoring of Zhejiang Province[M]. Beijing:Seismological Press, 2004. [7] 王斌, 梁雪萍, 周健.江苏及其周边地区断裂活动性与地震关系的分析[J].高原地震, 2008, 20(1):38~43 http://www.cnki.com.cn/Article/CJFDTOTAL-GYDZ200801007.htmWANG Bin, LIANG Xue-ping, ZHOU Jian. Analysis on relationship between fault activity and earthquakes in Jiangsu Province and its adjacent area[J]. Plathau Earthquake Research, 2008, 20(1):38~43. http://www.cnki.com.cn/Article/CJFDTOTAL-GYDZ200801007.htm [8] 方良好, 童远林, 赵朋, 等.安徽北部涡河断裂第四纪活动特征及地震危险性初步研究[J].防灾科技学院学报, 2015, (1):19~25 http://www.cnki.com.cn/Article/CJFDTOTAL-FZJS201501004.htmFANG Liang-hao, TONG Yuan-lin, ZHAO Peng, et al. Preliminary study on characteristics of Quaternary tectonic activity and seismic hazard of Guohe fault in northern part of Anhui Province[J]. Journal of Institute of Disater Prevention, 2015, (1):19~25. http://www.cnki.com.cn/Article/CJFDTOTAL-FZJS201501004.htm [9] 陈安国, 刘东旺, 郑海刚.安徽地区历史及现代地震活动与断裂活动性关系研究[J].华北地震科学, 2009, 27(4):16~21 http://www.cnki.com.cn/Article/CJFDTOTAL-HDKD200904004.htmCHEN An-guo, LIU Dong-wang, ZHENG Hai-gang. Study on historical and modern seismicity and fault tectonic in Anhui area[J]. North China Earthquake Sciences, 2009, 27(4):16~21. http://www.cnki.com.cn/Article/CJFDTOTAL-HDKD200904004.htm [10] 姚大全, 张杰, 沈小七.安徽霍山地区断层活动习性研究的新进展[J].地球物理学进展, 2006, 21(3):776~782 http://www.cnki.com.cn/Article/CJFDTOTAL-DQWJ200603013.htmYAO Da-quan, ZHANG Jie, SHEN Xiao-qi. New progress in the study of fault activity in the Huoshan area, Anhui[J]. Progress in Geophysics, 2006, 21(3):776~782. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWJ200603013.htm [11] 郑颖平, 翟洪涛, 李光, 等.安徽南部葛公镇断裂活动性初探[J].西部探矿工程, 2012, 24(11):111~114 doi: 10.3969/j.issn.1004~5716.2012.11.036ZHENG Ying-ping, ZHAI Hong-tao, LI Guang, et al. Gegongzhen fault activity in Southern Anhui[J]. West China Exploration Engineering, 2012, 24(11):111~114. doi: 10.3969/j.issn.1004~5716.2012.11.036 [12] 余钦范, 王晓青.安徽省及其邻区航磁异常特征与地震活动性[J].中国地震, 1987, 3(3)51~59:. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD198703008.htmYU Qin-fan, WANG Xiao-qing. The characteristics of aeromagnetic anomalies and the relation to the earthquake activities in Anhui Province and its vicinity[J]. Earthquake Research in China, 1987, 3(3):51~59. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD198703008.htm [13] 郑颖平, 翟洪涛, 李光, 等.安徽省未来中强震活动背景分析[J].内陆地震, 2010, 24(4):340~344 http://www.cnki.com.cn/Article/CJFDTOTAL-LLDZ201004006.htmZHENG Ying-ping, ZHAI Hong-tao, LI Guang, et al. The background analysis of future moderate-strong earthquake activity in Anhui Province[J]. Inland Earthquake, 2010, 24(4):340~344. http://www.cnki.com.cn/Article/CJFDTOTAL-LLDZ201004006.htm [14] 侯康明, 熊振, 李丽梅.对江苏省溧阳2次破坏性地震发震构造的新认识[J].地震地质, 2012, 34(2):303~312 http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201202010.htmHOU Kang-ming, XIONG Zhen, LI Li-mei. New insights into the seismogenic structures of the two destructive earthquakes in Liyang[J]. Seismology and Geology, 2012, 34(2):303~312. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201202010.htm [15] 梅岩辉, 张微, 吴建勇.多元信息在断裂空间展布调查中的应用——以马金-乌镇断裂为例[J].科技通报, 2013, 29(1):110~113 http://www.cnki.com.cn/Article/CJFDTOTAL-KJTB201301023.htmMEI Yan-hui, ZHANG Wei, Wu Jian-yong. An application of multivariate information in the investigation of the spatial distribution of faults:A case study of the Majin-Wuzhen fault[J]. Bulletin of Science and Technology, 2013, 29(1):110~113. http://www.cnki.com.cn/Article/CJFDTOTAL-KJTB201301023.htm [16] 吴中海, 赵希涛, 范桃园, 等.泛亚铁路滇西大理至瑞丽沿线主要活动断裂与地震地质特征[J].地质通报, 2012, 31(2):191~217 http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2012Z1001.htmWU Zhong-hai, ZHAO Xi-tao, FAN Tao-yuan, et al. Active faults and seismologic characteristics along the Dali-Ruili railway in western Yunnan Province[J]. Geological Bulletin of China, 2012, 31(2):191~217. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2012Z1001.htm [17] 闫素萍, 陈宇卫, 李敏莉, 等.华东地区Ms≥5.0地震持续平静的意义[J].地震地磁观测与研究, 2005, 26(6):1~8 http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzgj200506001&dbname=CJFD&dbcode=CJFQYAN Su-ping, CHEN Yu-wei, LI Min-li, et al. The meaning of Ms≥5.0 earthquake keep silence in East China[J]. Seismological and Geomagnetic Observation and Research, 2005, 26(6):1~8. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzgj200506001&dbname=CJFD&dbcode=CJFQ [18] 陈宇卫, 凌学书, 余华扬, 等.华东地区强震活动的特点及其应用[J].中国地震, 1999, 15(2):167~177 http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD902.007.htmCHEN Yu-wei, LING Xue-shu, YU Hua-yang, et al. Characteristics and application of strong earthquake activity in East China[J]. Earthquake Research in China, 1999, 15(2):167~177. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD902.007.htm [19] 翟文建, 齐小兵, 章泽军.江南断裂构造属性及成生环境初探[J].大地构造与成矿学, 2009, 33(3):372~380 http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200903009.htmZHAI Wen-jian, QI Xiao-bing, ZHANG Ze-jun. A preliminary study of tectonic attribute and formation environment of Jiangnan Fault[J]. Geotectonica et Metallogenia, 2009, 33(3):372~380. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200903009.htm [20] 方良好, 童远林, 赵朋, 等.安徽北部涡河断裂第四纪活动特征及地震危险性初步研究[J].防灾科技学院学报, 2015, 17(1):19~25 http://www.cnki.com.cn/Article/CJFDTOTAL-FZJS201501004.htmFANG Liang-Hao, TONG Yuan-Lin, ZHAO Peng, et al. Study on the Quaternary active features and seismic hazard of the vortex River in the north of Anhui[J]. Journal of Institute of Disaster Prevention, 2015, (1):19~25. http://www.cnki.com.cn/Article/CJFDTOTAL-FZJS201501004.htm [21] 王一宽. 江苏中强地震与活动断裂关系的初步探讨[C]//长三角科技论坛防震减灾学术分论坛. 2007 http://industry.wanfangdata.com.cn/dl/Column/Paper?q=%E6%B1%9F%E8%8B%8F%E5%A4%A7%E5%AD%A6%20%E7%BC%96%E7%BA%82%2F%E5%87%BA%E7%89%88%E5%8D%95%E4%BD%8D%3A%E5%8C%97%E4%BA%AC%E9%82%AE%E7%94%B5%E5%A4%A7%E5%AD%A6%E5%87%BA%E7%89%88%E7%A4%BE%20%E9%A2%81%E5%B8%83%E6%97%A5%E6%9C%9F%3A2007~2007%20%E6%95%88%E5%8A%9B%E7%BA%A7%E5%88%AB%3A%E9%83%A8%E9%97%A8%E8%A7%84%E8%8C%83%E6%80%A7%E6%96%87%E4%BB%B6%20DBID%3AWF_HY%20%E5%88%86%E7%B1%BB%E5%8F%B7%3A%22P3*%22&f=subjectCatagoryWANG Yi-kuan. Preliminary study of Jiangsu strong earthquakes and active faults[C]//The Yangtze River Delta Forum on science and technology in earthquake prevention and disaster reduction academic forum. 2007. http://industry.wanfangdata.com.cn/dl/Column/Paper?q=%E6%B1%9F%E8%8B%8F%E5%A4%A7%E5%AD%A6%20%E7%BC%96%E7%BA%82%2F%E5%87%BA%E7%89%88%E5%8D%95%E4%BD%8D%3A%E5%8C%97%E4%BA%AC%E9%82%AE%E7%94%B5%E5%A4%A7%E5%AD%A6%E5%87%BA%E7%89%88%E7%A4%BE%20%E9%A2%81%E5%B8%83%E6%97%A5%E6%9C%9F%3A2007~2007%20%E6%95%88%E5%8A%9B%E7%BA%A7%E5%88%AB%3A%E9%83%A8%E9%97%A8%E8%A7%84%E8%8C%83%E6%80%A7%E6%96%87%E4%BB%B6%20DBID%3AWF_HY%20%E5%88%86%E7%B1%BB%E5%8F%B7%3A%22P3*%22&f=subjectCatagory [22] 葛炳生.上海及邻近地区地震活动的特征[J].上海国土资源, 1981, (4):16~24 http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD198104001.htmGE Bing-sheng. The characteristics of seismic activity in Shanghai and its neighboring areas[J]. Shanghai Land and Resources, 1981, (4):16~24. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD198104001.htm [23] 朱积安, 朱履熹, 刘宜栋, 等.上海及邻区的地质构造与地震活动[J].华东师范大学学报:自然科学版, 1984, (4):81~90 http://www.cnki.com.cn/Article/CJFDTOTAL-HDSZ198404013.htmZHU Ji-an, ZHU Lü-xi, LIU Yi-dong, et al. Geological structure and seismic activity in Shanghai and its vicinity[J]. Journal of China Normal University:Natural Science Edition, 1984, (4):81~90. http://www.cnki.com.cn/Article/CJFDTOTAL-HDSZ198404013.htm [24] 朱履熹.上海及邻区新构造应力场初步探讨[J].上海国土资源, 1990, (1):45~55 http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199001003.htmZHU Lü-xi. A preliminary study of the neotectonic stress field in Shanghai and its vicinity[J]. Shanghai Land and Resources, 1990, (1):45~55. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199001003.htm [25] 段光贤, 刘昌森.上海及其邻近地区地震地质特征及上海基本地震烈度的初步认识[J].上海国土资源, 1987, (1):1~9 http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD198701000.htmDUAN Guang-xian, LIU Chang-sen. Preliminary understanding of the seismic geological characteristics of Shanghai and its adjacent areas and the basic seismic intensity of Shanghai[J]. Shanghai Land and Resources, 1987, (1):1~9. http://www.cnki.com.cn/Article/CJFDTOTAL-SHAD198701000.htm [26] 刘东旺, 夏瑞良, 沈小七, 等. 郯庐断裂带安徽段现代地震活动及应力场特征研究[C]//中生代以来中国大陆板块作用过程学术研讨会论文集. 2005 http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGEM198409001074.htmLIU Dong-wang, XIA Rui-liang, SHEN Xiao-qi, et al. The modern seismic activity and stress field characteristics of Tanlu faults zone in Anhui section[C]//The academic seminar on the role of the plate in China since the Mesozoic Era. 2005. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGEM198409001074.htm [27] 虞永林.温州-镇海复式断裂带全新世构造运动及地震的地质构造标志[J].浙江地质, 1992, 8(1):30~37 http://www.cnki.com.cn/Article/CJFDTOTAL-ZJDZ199201005.htmYU Yong-lin. The Holocene tectonic movement of Wenzhou-Zhenghai Multiple Belt and the geo-structural mark of earthquake[J]. Geology of Zhejiang, 1992, 8(1):30~37. http://www.cnki.com.cn/Article/CJFDTOTAL-ZJDZ199201005.htm [28] 陶夏新.我国新的地震区划编图和中国地震烈度区划图(1990)[J].自然灾害学报, 1992, 1(1):99~109 http://www.cnki.com.cn/Article/CJFDTOTAL-ZRZH199201020.htmTAO Xia-xin. The new national seismic zonation and the seismic intensity zoning map of China (1990)[J]. Journal of Natural Disasters, 1992, (1):99~109. http://www.cnki.com.cn/Article/CJFDTOTAL-ZRZH199201020.htm [29] 傅建武. 长三角城市群(浙江)地震科技发展规划[C]//长三角科技论坛防震减灾学术分论坛. 2007 http://c.wanfangdata.com.cn/ConferenceMeeting.aspx?Class=PFU Jian-wu. The earthquake science and technology development planning of the Yangtze River Delta city group (Zhejiang)[C]//Yangtze River Delta Forum on science and technology forum for earthquake prevention and disaster reduction. 2007. http://c.wanfangdata.com.cn/ConferenceMeeting.aspx?Class=P [30] 姚琪, 陈汉林, 张微, 等.浙江杭州地区孝丰-三门湾断裂晚第四纪活动性研究[J].高校地质学报, 2008, 14(4):601~609 http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200804016.htmYAO Qi, CHEN Han-lin, ZHANG Wei, et al. Zhejiang Hangzhou Xiaofeng-Sanmen Bay late Quaternary fault activity[J]. Geological Journal of China Uuniversities, 2008, 14(4):601~609. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200804016.htm [31] 陈立峰. 浙江省沿海北东向断裂活动性研究[D]. 杭州: 浙江大学, 2010 http://www.cnki.com.cn/Article/CJFDTotal-DDYJ200901001.htmCHEN Li-feng. Study on the activity of the faults in the east coast of Zhejiang province[D]. Hangzhou:Zhejiang University, 2010. http://www.cnki.com.cn/Article/CJFDTotal-DDYJ200901001.htm [32] 竺国强, 姜继双, 陈梓军, 等.浙西北江山-绍兴断裂带构造演化特征[J].浙江地质, 1997, 13(2):6~10 http://www.cnki.com.cn/Article/CJFDTOTAL-ZJDZ199702001.htmZHU Guo-qiang, JIANG Ji-shuang, CHEN Zi-jun, et al. Tectonic evolution and deformational features of Jiangshan-Shaoxing fracture zone in northwestern Zhejiang[J]. Geology of Zhejiang, 1997, 13(2):6~10. http://www.cnki.com.cn/Article/CJFDTOTAL-ZJDZ199702001.htm [33] 鄢家全, 贾素娟.中强地震潜在震源区划分原则和方法的研究进展[J].国际地震动态, 1997, (2):1~7 http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD199602007.htmYAN Jia-quan, JIA Su-juan. Moderate strong earthquake potential source division principles and methods of research progress[J]. Recent Developments in World Seismology, 1997, (2):1~7. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD199602007.htm [34] 黄汲清.按大地构造观点进行中国地震地质区划的尝试[J].中国地质科学院院报, 1979, 1(1):18~30 http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB197900001.htmHUANG Ji-qing. An attempt to the seismological regionalization of China according to the tectonic point of view[J]. Journal of China Academy of Geological Sciences, 1979, 1(1):18~30. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB197900001.htm [35] 高维明, 郑朗荪, 李家灵, 等.1668年郯城8.5级地震的发震构造[J].中国地震, 1988, 4(3):9~15 http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD198803002.htmGAO Wei-ming, ZHENG Lang-sun, LI Jia-ling, et al. The earthquake of 8.5 magnitude earthquake in Tancheng in 1668[J]. Earthquake Research in China, 1988, 4(3):9~15. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD198803002.htm [36] 张志中, 张征宇, 吴健, 等.皖南地区历史地震略考[J].震灾防御技术, 2013, 8(3):292~302 doi: 10.11899/zzfy20130308ZHANG Zhi-zhong, ZHANG Zheng-yu, WU Jian, et al. Historical earthquakes in southern Anhui Province[J]. Earthquake Disaster Prevention Technology, 2013, 8(3):292~302. doi: 10.11899/zzfy20130308 [37] 郑月军, 张世民, 崔效锋, 等.地震震源机制解在华南及邻区潜源区长轴方向判定中的应用[J].中国地震, 2006, 22(1):24~33 http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD200601002.htmZHENG Yue-jun, ZHANG Shi-min, CUI Xiao-feng, et al. Application of the seismic source mechanism in the determination of the long axis of the potential source region of Southern China and its adjacent area[J]. China Earthquake, 2006, 22(1):24~33. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD200601002.htm -
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