参考文献/References:
[1] YIN A, NIE S Y. An indentation model for the north and south China collision and the development of the Tan-Lu and Honame fault systems,Eastern Asia[J]. Tectonics, 1993,12(4):801-813.
[2] XU J, ZHU G. Tectonic Models of the Tan-Lu Fault Zone, Eastern China[J]. International Geology Review, 1994,36(8): 771-784.
[3] GILDER S A, LELOUP P H, COURTILLOT V.Tectonic evolution of the Tancheng-Lujiang(Tan-Lu)fault via Middle Triassic to Early Cenozoic paleomagnetic data[J]. Journal of Geophysical Research, 1999, 104(15): 365-375.
[4] ZHU G, LIU G S, NIU M L, et al. Syn-collisional transform faulting of the Tan-Lu fault zone, East China[J]. International Journal of Earth Sciences, 2009, 98(1): 135-155.
[5] 秦元喜,张良筹,严开健.赣榆—太湖断裂与郯庐断裂带的关系及其构造特征的初步探讨[J].中国地质科学院南京地质矿产研究所所刊,1985(1):66-71.
[6] 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.
[7] 晁洪太,王志才,刘西林.郯庐断裂带下辽河—莱州湾段与潍坊—嘉山段地震构造和地震活动特征对比[J]. 华北地震科学,1999,17(2):36-42.
[8] 李康,徐锡伟,魏雷鸣,等. 1668年郯城地震断层的长发震间隔与低速率证据[J]. 科学通报,2019,64(11): 1168-1178.
[9] 蒋功成,李才生,滕寿玉.从下草湾化石群看洪泽湖地区中新世时期的生物多样性[J]. 地质学刊,2013,37(2):169-172.
[10] 张玉兰,王开发,蒋辉.江苏泗洪地区峰山组的孢粉组合及其地质时代[J]. 地层学杂志,1982,6(2):107-111.
[11] 胡存礼.苏北—南黄海盆地西部边缘泗洪地区早中新世峰山组孢粉组合[G]//中国地质科学院地层古生物论文集编委会.地层古生物论文集:第十六辑.北京:地质出版社,1986:212-221.
[12] DENG Y, FAN W, ZHANG Z, et al. Geophysical evidence on segmentation of the Tancheng-Lujiang fault and its implications on the lithosphere evolution in East China[J]. Journal of Asian Earth Sciences, 2013, 78:263-276.
[13] SCHMID R, RYBERG T, RATSCHBACHER L, et al. Crustal structure of the eastern Dabie Shan interpreted from deep reflection and shallow tomographic data[J].Tectonophysics,2001, 333(3/4):347-359.
[14] ZHANG J, HAO T, DONG S, et al. The structural and tectonic relationships of the major fault systems of the Tan-Lu fault zone, with a focus on the segments within the North China region[J]. Journal of Asian Earth Sciences, 2015,110(1):85-100.
[15] ZHANG J, YANG X, SUN W, et al. New data on the evolution of the Tan-Lu fault belt: constraints from geological-geophysical surveys in the southern segment[J].International Geology Review, 2012, 54:1562-1578.
[16] GRIMMER J C, JONCKHEERE R, ENKELMANN E, et al. Cretaceous-Cenozoic history of the southern Tan-Lu fault zone: apatite fission-track and structural constraints from the Dabie Shan(eastern China)[J]. Tectonophysics, 2002,359(3/4):225-253.
[17] HACKER B R, RATSCHBACHER L, WEBB L,et al. Exhumation of ultrahigh-pressure continental crust in east central China:Late Triassic-Early Jurassic tectonic unroofing[J]. Journal of Geophysical Research, 2000,105:13339-13364.
[18] WANG Y. The onset of the Tan-Lu fault movement in eastern China: constraints from zircon(SHRIMP)and 40Ar/39Ar dating[J]. Terra Nova, 2006, 18:423-431.
[19] WANG Y, ZHOU S. 40Ar/39Ar dating constraints on the high-angle normal faulting along the southern segment of the Tan-Lu fault system: An implication for the onset of eastern China rift-systems[J]. Journal of Asian Earth Sciences, 2009, 34(1):51-60.
[20] ZHAO T, ZHU G, LIN S Z, et al. Indentation-induced tearing of a subducting continent: Evidence from the Tan-Lu Fault Zone, East China[J]. Earth-Science Reviews, 2016,152:14-36.
[21] ZHU G, LIU G, DUNLAP W J, et al.40Ar/39Ar geochronological constraints on syn-orogenic strike-slip movement of Tan-Lu fault zone[J]. Chinese Science Bulletin, 2004,49(5):499.
[22] 周济元.安徽张八岭地区构造演化及动力学[J].火山地质与矿产,1995(4):17-24.
[23] 董茂兴,张德宝,郭坤一.张八岭地区地质构造特征[J].火山地质与矿产,1995(4):45-52.
[24] 沈小七,姚大全,郑海刚,等.郯庐断裂带重岗山—迁段晚更新世以来的活动习性[J].地震地质, 2015,37(1):139-148.
[25] 姚大全,汤有标,沈小七,等.郯庐断裂带赤山段中晚更新世之交的史前地震遗迹[J].地震地质,2012,34(1):93-99.
[26] 曹筠,冉勇康,许汉刚,等.宿迁城市活动断层探测多方法技术运用的典型案例[J]. 地震地质,2015,37(1):430-439.
[27] LIU B, ZHU G, ZHAI M J, et al.Quaternary faulting of the Jiangsu part of the Tan-Lu Fault Zone, East China: Evidence from field investigations and OSL dating[J]. Journal of Asian Earth Sciences, 2015, 114:89-102.
[28] JIANG R, CAO K, ZENG J W,et al.Late Cenozoic tectonic evolution of the southern segment of the Tan-Lu fault zone, Eastern China [J]. Journal of Asian Earth Sciences, 2019, 182.
[29] 李传夔.江苏泗洪中新世长臂猿类化石[J].古脊椎动物与古人类,1978,16(3):187-193.
[30] 林水龙.淮河下游地区中新统的划分及其时代讨论[J].地层学杂志,1980,4(2):136-144.
[31] 顾玉珉,林一璞.记江苏泗洪首次发现森林古猿类化石[J].人类学学报,1983,2(4):305-315.
[32] 邱铸鼎.江苏泗洪下草湾中中新世脊—山河狸科(哺乳纲,啮齿目)[J]. 古脊椎动物与古人类,1987,25(4):283-296.
[33] QIU Z D. Cricetid rodents from the early Miocene Xiacaowan formation,Sihong,Jiangsu[J]. Vertebrata Palasiatica, 2010,48(1):27-47.
[34] LI C B, JIANG R, YU J J, et al. Deep structures underneath the Sihong Segment of the Tan-Lu Fault Zone, Eastern China:Interpretations of gravity anomaly and seismic profiles[J]. Journal of Asian Earth Sciences,2019,176: 229-243.
[35] QIAN M P, ZOU S M, LI S, et al. The Discovery of A Late Pleistocene Palaeoloxodon huaihoensis from Sihong County northern Jiangsu Province,China[J]. Journal of Geology, 2016,40(4):545-551.
[36] 蒋仁,钱迈平,曾剑威,等.苏北泗洪晚更新世淮河古菱齿象化石年代学研究及其意义[J].地层学杂志, 2019,43(1):96-100.
[37] 钱迈平,高天山,蒋仁,等.江苏泗洪晚更新世淮河古菱齿象化石层位和古环境[J].地层学杂志,2017,41(2):173-178.
[38] 凌申.全新世以来里下河地区古地理演变[J].地理科学,2001,21(5):474-479.