[1] 洪德全, 王行舟, 倪红玉, 等. 多种方法研究2012年7月20日江苏高邮MS4.9地震震源机制和震源深度[J]. 地球物理进展, 2013, 28(4): 1757-1765. (Hong Dequan, Wang Xingzhou, Ni Hongyu, et al. Focal mechanism and focal depth of July 20, 2012 JiangSu Gaoyou MS4.9 earthquake[J]. Progress in Geophysics, 2013, 28(4): 1757-1765. (in Chinese))
[2] 王俊, 缪发军, 詹小艳, 等. 利sPn震相精确测定江苏高邮、宝应交界M4.9地震震源深度[J]. 防震减灾工程学报, 2013, 33(3): 354-360. (Wang Jun, Miao Fajun, Zhan Xiaoyan, et al. Precise Determination of the Focal Depth of Jiangsu Gaoyou-Baoying M4.9 Earthquake by sPn Phase[J]. Journal of Disaster Prevention and Mitigation Engineering, 2013, 33(3): 354-360. (in Chinese))
[3] 康清清, 缪发军, 刘红桂, 等.利用矩张量反演法研究江苏-高邮M_S 4.9地震震源机制和震源深度[J]. 地球物理学报, 2015, 58(1): 204-215. (Kang Qingqing, Miao Fajun, Liu Honggui, et al. Focal mechanism and focal depth of the Gaoyou-Baoying, Jiangsu, china M_S4.9 earthquake on 20 July 2012 derived from moment tensorinversion[J]. Chinese Journal of Geophysics, 2015, 58(1): 204-215. (in Chinese))
[4] 郭斌, 张鹏, 王俊, 等. 2012年7月20日高邮M4.9级地震发震构造探讨[J].华北地震科学, 2015, 33(4): 24-29,36. (Guo Bin, Zhang Peng, Wang Jun, et al. Discussion on Seismogenic Structure of Gaoyou M4.9 Earthquake on July 20, 2012[J]. North China Earthquake Sciences, 2015, 33(4): 24-29,36. (in Chinese))
[5] 赵启光, 孙业君, 黄耘. 等. 高邮—宝应M_s4.9地震的发震构造[J]. 地震地质, 2021, 43(3): 630-646. (Zhao Qiguang, Sun Yejun, Huang Yun, et al. A Study On The Seismogenic Structure Of Gaoyou-Baoying MS4.9 Earthquake[J]. Seismology and Geology, 2021, 43(3): 630-646. (in Chinese))
[6] 倪红玉, 郑海刚, 刘泽民, 等. 2012年江苏高邮、宝应交界M4.9地震发震断层参数测定[J]. 地震工程学报, 2015, 37(1): 260-265. (Ni Hongyu, Zheng Haigang, Liu Zemin, et al. Determination of Fault Plane Parameters of the 2012 Gaoyou-Baoying MS4.9 Earthquake in Jiangsu Province [J]. China Earthquake Engineering Journal, 2015, 37(1): 260-265. (in Chinese))
[7] 孙业君, 王俊, 黄耘. 2012年7月20日江苏省高邮—宝应M4.9地震震源机制[J]. 防震减灾工程学报, 2012, 32(4): 521-522. (Sun Yejun, Wang Jun, Huang Yun. Focal Mechanism Solution of M4.9 Earthquake for 20 July 2012 Gaoyou-Baoying, Jiangsu Province[J]. Journal of Disaster Prevention and Mitigation Endineering, 2012, 32(4): 521-522. (in Chinese))
[8] 何斌, 王恒知, 张元生. 基于视出射角与到时参数联合定位方法对高邮、宝应交界M4.9地震序列的定位研究[J]. 地震工程学报, 2014, 36(4): 1081-1086. (He Bin, Wang Hengzhi, Zhang Yuansheng. Location of the Gaoyou-Baoying M4.9 Earthquake Using Apparent Emergence Angle and Seismic Arrival Times[J]. China Earthquake Engineering Journal, 2014, 36(4): 1081-1086. (in Chinese))
[9] 刘建达, 杨伟林, 李丽梅, 等. 江苏高邮—宝应交界4.9级地震震害分析[J]. 中国地震, 2012, 28(4): 402-414. (Liu Jianda, Yamg Weilin, Li Limei, et al. Damage survey and analysis on earthquake (MS= 4.9) at the boundary zone of Gaoyou and Baoying, Jiangsu Province[J]. Earthquake Research in China, 2012, 28(4): 402-414. (in Chinese))
[10] Marshall, T.S, Cooke, et al.Interseismic deformation associated with three-dimensional faults in the greater Los Angeles region, California[J]. Journal of Geophysical Research, 2009, 114(12): 1-17.
[11] Wang Q,Qiao X J, Lan Q G, et al. Rupture of deep faults in the 2008 Wenchuan earthquake and uplift of the Longmeng Shan[J]. Nature Geoscience, 2001, 4(9): 634-640.
[12] Shi Z, Day S M.Ruputure dynamics and ground motion from 3-D rough-fault simulations[J]. Journal of Geophysical Research: Soild Earth, 2013, 108(B3). doi: 10.1029/2001JB001628.
[13] Herbert J W, Cooke M L, Marshall S T, et al. Influence of fault connectivity on slip rates in southern California: Potential impact on discrepancies between geodetic derived and geologic slip rates[J]. Journal of Geophysical Research: Solid Earth, 2014, 119(3): 2342-2361.
[14] Thompson J,Philibosian B, Chupik C, et al. Evidence of Previous Faulting along the 2019 Ridgecrest, California, Earthquake Ruptures[J]. Bulletin of the Seismological Society of America, 2020, 110(4): 1427-1456.
[15] Hubbard J, Almeida R, Foster A, et al. Structural segmentation controlled the 2015 MW7.8Gorkha earthquake rupture in Nepal[J]. Geology, 2016, 44(8): 639-642.
[16] Lozos J C, Harris R A, Murray R J, et al. Dynamic rupture models of earthquakes on the Bartlett Springs Fault, Northern California[J]. Geophysical Research Letters, 2015, 42(11): 4343-4349.
[17] Hamling I J, Hreinsdóttir S, Clark K, et al. Complex multifault rupture during the 2016 Mw7.8 Kaikōura earthquake, New Zealand[J]. Science, 2017, 356(6334): 7194.
[18] Lu R Q,Xu X W, He D F, et al. Seismotectonics of the 2013 Lushan Mw6.7 earthquake: Inversion tectonics in the eastern margin of the Tibetan plateau[J]. Geophysical Research Letters, 2017, 44(16): 8236-8243.
[19] Lu R Q, Zhao C P, Zhang J Y, et al. 3D fault model andseismotectonics indicate the potential seismic risk in the Daliang Mountains, southeastern Tibetan Plateau[J]. Journal of the Geological Society, 2024, 181(2): 2023-136.
[20] Riesner M, Durand-Riard P, Hubbard J, et al. Building objective 3D fault representations in active tectonic settings[J]. Seismological Research Letters, 2017, 88(3): 831-839.
[21] Plesch A, Shaw J H, Ross Z E, et al. Detailed 3D fault representations for the 2019 Ridgecrest, California, earthquake sequence[J]. Bulletin of the Seismological Society of America, 2020, 110(4): 1818-1831.
[22] 鲁人齐, 房立华, 郭志, 等. 2022年6月1日四川芦山M_s6.1强震构造精细特征[J]. 地球物理学报, 2022, 65(11): 4299-4310. (Lu Renqi, Fang Lihua, Guo Zhi, et al. Detailed structural characteristics of the 1 June 2022 MS6.1 Sichuan Lushan strong earthquake[J]. Chinese Journal of Geophysics, 2022, 65(11): 4299-4310. (in Chinese))
[23] Caumon G, Tertois A L, Zhang L. Elements for stochastic structural perturbation of stratigraphic modeis [A]// EAGE conference on petroleum geostatistics. Cascais, Portugal. European Association of Geoscientists & Engineers[C]. 2007: cp-32-00002.
[24] 陈友飞, 严钦尚, 许世远.苏北盆地沉积环境演变及其构造背景[J]. 地质科学, 1993, 28(2): 151-160. (Chen Youfei, Yan Qinshang, Xu Shiyuan. Depository Environment Evolution and Its Structural Background of the Subei Basin[J]. Scientia Geologica Sinica, 1993, 28(2): 151-160. (in Chinese))
[25] 毛凤鸣, 陈安定, 严元峰, 等. 苏北盆地复杂小断块油气成藏特征及地震识别技术[J]. 石油与天然地质, 2006, 27(6): 827-840. (Mao Fengming, Chen Anding, Yan Yuanfeng, et al. Hydrocarbon pooling features and seisnic recognizing technologies of small complex fault blocks in Subei basin[J]. Oil ＆ Gas Geology, 2006, 27(6): 827-840. (in Chinese))
[26] 刘寅, 陈清华, 胡凯, 等.渤海湾盆地-南黄海盆地构造特征和成因对比[J]. 大地构造与成矿学, 2014, 38(1): 38-51. (Liu Yin, Chen Qinghua, Hu Kai, et al. Comparison of the Bohai Bay Basin and Subei-South Yellow Sea Basinin the Structural characteristics and Forming Mechanism[J]. Geotectonica et Metallogenia, 2014, 38(1): 38-51. (in Chinese))
[27] 王玺, 陈清华, 朱文斌, 等. 苏北盆地高邮凹陷边界断裂带构造特征及成因[J]. 大地构造与成矿学, 2013, 37(1):20-28. (Wang Xi, Chen Qinghua, Zhu Wenbin, et al. Structural Characteristics and Origin of Boundary Fault Belts of the Gaoyou Sag in the Subei Basin[J]. Geotectonica et Metallogenia, 2013, 37(1): 20-28. (in Chinese))
[28] 陈安定. 苏北盆地构造特征及箕状断陷形成机理[J].石油与天然气地质, 2012, 31(2):140-15. (Chen Anding. Tectonic features of the Subei Basin and the forming mechanism of its dustpan-shaped fault depression[J]. Oil ＆Gas Geology, 2010, 31(2): 140-15. (in Chinese))
[29] 梁兵.高邮凹陷断层—岩性油气藏勘探技术与实践[J]. 中国石油勘探, 2013, 18(4): 36-39. (Liang Bing. Fault-Lithologic Reservoir Exploration Technology and Practice in Gaoyou Sag[J]. China Petroleum Exploration, 2013, 18(4): 36-49. (in Chinese))
[30] 朱光, 姜芹芹, 朴学峰, 等.基底断层在断陷盆地断层系统发育中的作用:以苏北盆地南部高邮凹陷为例[J]. 地质学报, 2013, 87(4): 441-451. (Zhu Guang, Jiang Qinqin, Pu Xuefeng, et al. Role of Basement Faults in Faulting System Development of A RiftBasin: An Example from the Gaoyou Sag in Southern Subei Basin[J]. Acta Geologica Sinica, 2013, 87(4): 441-451. (in Chinese))
[31] 胡红雷, 朱光. 苏北地区前陆变形特征与形成机制[J].大地构造与成矿学, 2013, 37(3): 366-376. (Hu Honglei, Zhu Guang. Characteristics and Formation Mechanism of the Foreland Deformation in the Subei Region[J]. Geotectonica et Metallogenia, 2013, 37(3): 366-376. (in Chinese))
[32] 吴健生. 江苏北部G262线大地电磁测探(MT)区域勘探与综合研究成果报告[R]. 1996. (WU Jiansheng. Report on regional exploration and comprehensive research results of magnetotelluric sounding (MT) along G262 line in northern Jiangsu Province[R]. 1996. (in Chinese))
[33] 曾萍. G78区域大剖面综合解释与苏北盆地构造特征[J]. 石油天然气学报, 2007, 29(3): 82-86. (Zeng Ping. G78 regional profiles interpretation and Subei Basin tectonic characteristics[J]. Journal of Oil and Gas Technology, 2007, 29(3): 82-86. (in Chinese))
[34] 江苏省地质调查院. 江苏省干热岩资源调查评价报告[R]. 2017. (Geological Survery of JiangSu Province. 2017. Investigation and evaluation of dry-hot rock resources in Jiangsu province [R]. 2017. (in Chinese))
[35] 江苏石油勘探局. 江苏北部G262线大地电磁探测(MT)区域勘探与综合研究成果报告[R]. 1996. (Jiangsu Oil-field Engineering Institute. Report on regional exploration and comprehensive research results of G262 Line magnetotelluric exploration (MT) in northern Jiangsu Province[R]. 1996. (in Chinese))
[36] 陈沪生.下扬子及邻区岩石圈结构构造特征与油气资源评价[M]. 北京:地质出版社, 1999. (Chen Husheng. Structural characteristics and hydrocarbon resource evaluation of lithosphere in Lower Yangtze and adjacent areas[M]. Beijing: Geology Press, 1999. (in Chinese))
[37] 郭彤楼, 李国雄, 曾庆立. 江汉盆地当阳复向斜当深3井热史恢复及其油气勘探意义[J]. 地质科学, 2005(4): 122-130. (Guo Tonglou, Li G X, Zeng Q L. Thermal History Reconstruction For Well Dangshen 3 In The Dangyang Synclinorium, Jianghan Basin And Itsexploration Implications[J]. Chinese Journal of Geology, 2005(4): 122-130. (in Chinese))
[38] 黄耘, 李清河, 张元生, 等. 江苏及邻区地震重新定位和构造特征分析[J]. 地球物理学报, 2008(1): 175-185. (Huang Yun, Li Qinghe, Zhang Yuansheng, et al. Relocation of earthguakes in Jiangsu and neighboring areas,China andanalysis of structural features[J]. Chinese Journal of Geophysics, 2008(1): 175-185. (in Chinese))
