郯庐断裂带西山驿岩体构造变形分析
|
摘要
地处肥东岩群西侧的西山驿岩体,由于郯庐断裂带左行平移活动的影响而发生韧性变形。根据野外调查和室内研究,岩体的西侧边界由于受到郯庐断裂带次级剪切带的影响,导致变形强度比岩体内部强烈,岩性上可分为边界糜棱岩带和内部片麻岩带。本文对边界韧性剪切带进行了变形温度估算,剪切类型分析,应力场的方向、差应力大小、应变速率计算。结果显示剪切带糜棱岩的变形温度约为500～600℃,为低角闪岩相变质,内部片麻岩变形温度约为400～530℃,为高绿片岩相到低角闪岩相变质;糜棱岩样品中矿物变斑晶的涡度值介于0.86～0.94之间,剪切类型为简单剪切为主的一般剪切;古应力方向为164°～171°,最低差应力下限值为20.02～23.08MPa,应变速率为1.35×10~(-13)～4.93×10~(-13)s~(-1)。在中、晚侏罗世到早白垩世期间,由于太平洋板块的斜向汇聚作用,郯庐断裂带发生构造活动,而通过上述西山驿岩体的构造变质变形分析结果,反演郯庐断裂带的变形规律,并且希望借此在以后的研究中归纳该时期中国东部的构造演化过程。
Objective: The Tancheng—Lujiang fault( Tanlu fault) belt,as a giant shear zone in eastern China,has been a hot spot among geologists since it was discovered.The Xishanyi pluton,which protolith was monzogranite,located in the west of Feidong group. However,the pluton occurred ductile deformation due to sinistral strike-slip shearing of the Tanlu fault belt.The mylonite with strong deformation is formed on both sides of the pluton,and the gneiss within the pluton is deformed weakly. Due to the serious overburden,only the west side is exposed. In this paper,the structural analysis of mylonite and gneiss are carried out,to investigate the structural deformation characteristics of the Xishanyi pluton.Methods: Detailed field observation,microstructure analysis,estimation of metamorphic—deformation temperature,analysis of tectonic stress field,kinematic vorticity calculation,the fractal dimension of the quartz,and the calculation of differential stress and strain rate of quartz are used to study the Xishanyi pluton.Results: Through the observation and analysis,the dynamic recrystallization type of quartz and feldspar in mylonite is mainly GBM and BLG—SR,respectively. The dynamic recrystallization type of quartz and feldspar in gneiss is SR—GBM and BLG,respectively. In addition,the fractal dimension of the quartz in mylonite is between1.164 ～ 1.173,indicating the metamorphic—deformation temperature of mylonite is between 500 ～ 600℃.However it is 400 ～ 530℃ in gneiss.Through microscopic analysis and measurement,the vorticity value Wkis between 0.86 ～0.94,which is greater than 0.75 and indicates that the shear zone on the west side of the Xishanyi pluton is mainly simple shear,with little component of pure shearing; The results of stress field show that the direction of maximum compressional stress is between 164° ～ 171°. The minimum differential stress is between 20. 02 ～ 23. 08 Mpa,and strain rate of the shear zone is between 1.35×10-13～ 4.93×10-13 s-1.Conclusions: Through detailed field observation and indoor analysis on the Xishanyi pluton,we know the pluton participated in the activities of the Tanlu fault belt as a tectonic lenticles.The pluton and the shear zone on both sides constitute the "S—C"fabric.The pluton recorded the activity characteristics of the Tanlu fault belt.
Objective: The Tancheng—Lujiang fault( Tanlu fault) belt,as a giant shear zone in eastern China,has been a hot spot among geologists since it was discovered.The Xishanyi pluton,which protolith was monzogranite,located in the west of Feidong group. However,the pluton occurred ductile deformation due to sinistral strike-slip shearing of the Tanlu fault belt.The mylonite with strong deformation is formed on both sides of the pluton,and the gneiss within the pluton is deformed weakly. Due to the serious overburden,only the west side is exposed. In this paper,the structural analysis of mylonite and gneiss are carried out,to investigate the structural deformation characteristics of the Xishanyi pluton.Methods: Detailed field observation,microstructure analysis,estimation of metamorphic—deformation temperature,analysis of tectonic stress field,kinematic vorticity calculation,the fractal dimension of the quartz,and the calculation of differential stress and strain rate of quartz are used to study the Xishanyi pluton.Results: Through the observation and analysis,the dynamic recrystallization type of quartz and feldspar in mylonite is mainly GBM and BLG—SR,respectively. The dynamic recrystallization type of quartz and feldspar in gneiss is SR—GBM and BLG,respectively. In addition,the fractal dimension of the quartz in mylonite is between1.164 ～ 1.173,indicating the metamorphic—deformation temperature of mylonite is between 500 ～ 600℃.However it is 400 ～ 530℃ in gneiss.Through microscopic analysis and measurement,the vorticity value Wkis between 0.86 ～0.94,which is greater than 0.75 and indicates that the shear zone on the west side of the Xishanyi pluton is mainly simple shear,with little component of pure shearing; The results of stress field show that the direction of maximum compressional stress is between 164° ～ 171°. The minimum differential stress is between 20. 02 ～ 23. 08 Mpa,and strain rate of the shear zone is between 1.35×10-13～ 4.93×10-13 s-1.Conclusions: Through detailed field observation and indoor analysis on the Xishanyi pluton,we know the pluton participated in the activities of the Tanlu fault belt as a tectonic lenticles.The pluton and the shear zone on both sides constitute the "S—C"fabric.The pluton recorded the activity characteristics of the Tanlu fault belt.
引文
陈宣华,王小凤,张青,陈柏林,陈正乐,Harrison T M,Yin An.2000.郯庐断裂带形成演化的年代学研究.长春科技大学学报,30(3):215～220.
董树文,吴宣志,高锐,卢德源,李英康,何义权,汤加富,曹奋扬,侯明金,黄德志.1998.大别造山带地壳速度结构与动力学.地球物理学报,41(3):349～361.
侯明金,王永敏,Jacques M,Pierre V.2003.郯庐断裂带(安徽部分)动力学演化及其构造意义.地质通报,22(2):105～112.
侯明金,Jacques M,Pierre V,王永敏.2006.郯庐断裂带的两大发展阶段——广义的逆冲推覆断裂带和狭义的平移断裂带.中国地质,33(6):1267～1275.
胡惟,朱光,严乐佳,詹润.2014.郯庐断裂带中段地震活动性与深部地壳电性结构关系的探讨. 地质论评,60(1):80～90.
李建波,郭磊,鲁勇花,曾涛.2017.华北克拉通北缘医巫闾山韧性剪切拆离带的运动学涡度与韧性减薄量.地质论评,63(6):1429～1439.
李曙光,刘德良,陈移之,王松山,裘冀,胡世玲,桑海清.1993.中国中部蓝片岩的形成时代.地质科学,28(1):21～27.
李振生,田晓莉,张文俊,陶冶. 2013.安徽桐城挂车河镇地区东西向韧性剪切带分形特征及其估算应变速率适用性分析.科技导报,31(20):15～19.
刘备,朱光,胡红雷,宋利宏.2015.郯庐断裂带江苏段新构造活动规律分析.地质学报,89(8):1352～1366.
乔秀夫.1981.对郯—庐断裂巨大平移之质疑. 地质论评,27(3):222-224.
宋传中,朱光,刘洋,牛漫兰,刘国生.2003.郯庐断裂带肥东韧性剪切带的变形规律、同位素年龄及其构造意义.地质论评,49(1):10～17.
宋传中,黄文成,Shoufa Lin,任升莲,李加好,涂文传.2010a.长江中下游转换构造结的特征、属性及其研究意义.安徽地质,20(1):14～29.
宋传中,Lin Shoufa,周涛发,闫峻,任升莲,李加好,涂文传,张妍.2010b.长江中下游及其邻区中生代构造体制转换.岩石学报,26(9):2835～2849.
宋传中,张华,任升莲,李加好,Lin Shoufa,涂文传,张妍,王中.2011.长江中下游转换构造结与区域成矿背景分析.地质学报,85(5):778～788.
宋传中,李加好,任升莲,Lin Shoufa,刘欢,黄鹏,王微,杨帆.2014.长江中下游地区中生代陆内构造作用与成因分析.地质科学,49(2):339～354.
汤加富,许卫.2002.郯庐断裂带南段并无巨大平移——来自安徽境内的证据. 地质论评, 48(5):449～456.
汤加富,李怀坤,娄清.2003.郯庐断裂南段研究进展与断裂性质讨论.地质通报,22(6):426～436.
万桂梅,汤良杰,金文正,余一欣.2009.郯庐断裂带研究进展及存在问题探讨.地质论评,55(2):251～259.
万天丰,朱鸿,赵磊,林建平,程捷,陈进.1996.郯庐断裂带的形成与演化:综述.现代地质,10(2):159～168.
王书琴,孙晓猛,杜继宇,王英德,许强伟,田景雄.2012.郯庐断裂带北段构造样式解析.地质论评,58(3):414～425.
王微,宋传中,任升莲,李加好,张妍,汪佩佩,胡达.2016a.郯庐断裂带中桃源韧性剪切带剪切温压条件及锆石U-Pb分析.岩石学报,32(3):787～803.
王微,宋传中,李加好,任升莲,张妍,冯腊梅,李振伟,王阳阳.2016b.郯庐断裂带肥东桃源韧性剪切带构造分析及时限探究.地质科学,51(4):1040～1058.
王小凤.2000.郯庐断裂带.地质出版社.
王新社,郑亚东,杨崇辉,侯贵廷.2001.用动态重结晶石英颗粒的分形确定变形温度及应变速率.岩石矿物学杂志,20(1):36～41.
王勇生,朱光,王道轩,刘国生,宋传中.2004a.大别山东缘郯庐两期走滑剪切带形成的温压条件与造山带折返的关系.大地构造与成矿学,28(3):228～238.
王勇生,朱光.2004b.运动学涡度及其测量方法.合肥工业大学学报,27(11):1480～1484.
王勇生,朱光,王道轩,宋传中,刘国生.2005.地质温度计在郯庐断裂带南段低温糜棱岩中的尝试.中国地质,32(4):625～633.
王勇生,朱光,宋传中,刘国生.2006.郯庐断裂带南段晚期韧性剪切带涡度分析及其构造意义.地质论评,52(5):591～600.
向必伟,朱光,王勇生,谢成龙,胡召齐.2007.糜棱岩化过程中矿物变形温度计.地球科学进展,22(2):126～135.
肖文交,周烑秀,杨振宇,赵西西.2000.大别—郯庐—苏鲁造山带复合旋转拼贴作用.地球科学进展,15(2):147～153.
徐嘉炜. 1980. 郯庐断裂带的平移运动及其地质意义. 见: 国际交流地质学术论文集(1):构造地质,地质力学. 北京: 地质出版社: 129～142.
徐嘉炜.1985.郯庐断裂带北段平移研究的若干进展——答乔秀夫的“对郯庐断裂巨大平移质疑”. 地质论评,31(1):83～86.
徐嘉炜,马国锋.1992.郯庐断裂带研究的十年回顾. 地质论评,38(4):316～324.
徐嘉炜,朱光,吕培基,郑学信,孙世群.1995.郯庐断裂带平移年代学研究的进展.安徽地质,5(1):1～12.
徐树桐,江来利,刘怡灿,张勇.1992.大别山区(安徽部分)的构造格局和演化过程.地质学报,66(1):1～14.
薛德杰,徐先兵,李源,章泽军,楼法生.2014.华南武功山早古生代花岗岩构造变形特征及其形成机制,地质学报,88(7):1236～1246.
严乐佳,朱光,林少泽,赵田.2014.沂沭断裂带新构造活动规律与机制.中国科学(D辑),44(7):1452～1467.
杨文采,于常青. 2001.根据地球物理资料分析大别-苏鲁超高压变质带演化的运动学与动力学.地球物理学报,44(3):346～359.
张波,张进江,郭磊.2006.北喜马拉雅穹隆带然巴韧性剪切带石英动态重结晶颗粒的分维几何分析与主要流变参数的估算.地质科学,41(1):158～169.
张鹏,王良书,钟锴,丁增勇.2007.郯庐断裂带的分段性研究.地质论评,53(5):586～591.
张岳桥,董树文.2008.郯庐断裂带中生代构造演化史:进展与新认识.地质通报,27(9):1371～1390.
赵田,朱光,林少泽,宋利宏.2014a.郯庐断裂带南段张八岭群变质岩的原岩时代及其构造意义.地质论评,60(6):1266～1283.
赵田,朱光,林少泽,严乐佳,姜芹芹.2014b.郯庐断裂带张八岭隆起段变质岩的原岩时代与变形机制.中国科学(D辑),44(10):2112～2129.
赵田,朱光,向必伟,林少泽,顾承串.2016.郯庐断裂带起源机制的探讨.矿物岩石地球化学通报,35(5):1120～1140.
郑亚东,王涛,张进江.2008.运动学涡度的理论与实践.地学前缘,15(3):209～220.
朱光,徐嘉炜,孙世群.1995.郯庐断裂带平移时代的同位素年龄证据.地质论评,41(5):452～456.
朱光,牛漫兰,刘国生,王道轩,宋传中.2002.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件.地质学报,76(3):325～334.
朱光,王道轩,刘国生,牛漫兰,宋传中.2004a.郯庐断裂带的演化及其对西太平洋板块运动的响应.地质科学,39(1):36～49.
朱光,王勇生,牛漫兰,刘国生,谢成龙.2004b.郯庐断裂带的同造山活动.地学前缘,11(3):169～182.
朱光,牛漫兰,刘国生,王勇生,谢成龙,李长城2005.郯庐断裂带肥东段走滑运动的40Ar /39Ar法定年.地质学报,79(3):303～316.
朱光,张力,谢成龙,牛漫兰,王勇生.2009.郯庐断裂带构造演化的同位素年代学制约.地质科学,44(4):1327～1342.
朱光,王薇,顾承串,张帅,刘程.2016.郯庐断裂带晚中生代演化历史及其对华北克拉通破坏过程的指示.岩石学报,32(04):935～949.
Chung Sunlin. 1999.Trace element and isotope characteristics of Cenozoic basalts around the Tanlu Fault with implications for the eastern plate boundary between North and South China.The Journal of Geology,107(3):301～312.
Chen Xuanhua,Wang Xiaofeng,Zhang Qing,Chen Bolin,Chen Zhengle,Harrison T Mark,Yin An.2000&.Gechronologic study on the formation and evolution of Tanlu fault.Journal of Changchun University of Science and Technology,30(3):215～220.
De Paor D G.1983.Orthographic analysis of geologic structures—I.Deformation theory.Journal of Structural Geology,5(3):255～278.
Dong Shuwen,Wu Xuanzhi,Gao Rui,Lu Deyuan,Li Yingkang,He Yiquan,Tang Jiafu,Cao Fenyang,Hou Mingjin,Huang Dezhi.1998&.On the crust velocity levels and dynamics of the Dabieshan orogenic belt.Acta Geophysica Sinica,41(3):349～361.
Hou Mingjin,Wang Yongmin,Jacques M,Pierre V.2003&.Dynamic evolution and tectonic significance of the Tanlu fault zone(Anhui segment).Geological Bulletin of China,22(2):105～112.
Hou Mingjin,Jacques M,Pierre V,Wang Yongmin.2006&.Two development stages of the Tanlu fault zone:the stages of the overthrust fault zone sensu lato and the wrench fault zone sensu stricto.Geology in China,33(6):1267～1275.
Hu Wei, Zhu Guang, Yan Lejia, Zhan Run. 2014&. Analysis of relationship between seismic activity and crust electrical textures for the central segment of the Tan-Lu fault zone. Geological Review,60(1):80～90.
Kruhl J H,Nega M and MillaH E.1995.The fractal shape of grain boundary sutures:reality,modeland application asa geo-thermometer.Book of Abstracts,2nd In.t Con.f on Fractaland.Dynamic Systems in Geosciences,84 Frankfort:31～32.
Kruhl J H,Nega M.1996.The fractal shape of sutured quartz grain boundaries:application as a geothermometer.Geologishe Rundschau,85(1):38～43.
Li Jianbo,Guo Lei,Lu Yonghua,Zeng Tao.2017&.The kinematic vorticity and the ductile thinning of the YiwulüShan ductile shear detachment zone in North China Craton. Geological Review,63(6):1429～1439.
Li Shuguang,Liu Deliang,Chen Yizhi,Wang Songshan,Qiu Ji,Hu Shiling,Sang Haiqing.1993&.Time of the blueschis belt formation in central China.Scientia Geological Sinica,28(1):21～27.
Li Zhensheng,Tian Xiaoli,Zhang Wenjun,Tao Ye.2013&.Fractal analysis of east—west ductile shear zone in Guachehe town area,Tongcheng,Anhui and its applicability of strain-rate estimation.Science & Technology Review,31(20):15～19.
Li Zhengxiang.1994.Collision between the north and south China blocks:A crust-detachment model for suturing in the region east of the Tan-Lu fault.Geology,22(8):739～742.
Liu Bei,Zhu Guang,Hu Honglei,Song Lihong.2015&.Analysis on neotectonic activity of the Jiangsu Part of the Tan-Lu Fault Zone.Acta Geologica Sinica,89(8):1352～1366.
Matthews P E,Bond R A,Vallden Berg J.1974.Analgebraic method of strain analysis using ellipitical markers.Tectonopbysics,24(1～2):31～67.
Means W D,Hobbs B E,Lister G S, Willianms P F.1980.Vorticity and non-coaxialicy in progressive deformation.Journal of Structural Geology,2(3):371～378.
Qiao Xiufu. 1981&. Doubts concerning the great horizontal displacement along the Tancheng—Lujiang fault zone. 1981. Geological Review,27(3):222～224.
Orife T,Lisle R J.2006.Assessing the statistical significance of palaeostress estimates:Simulations using random fault slips. J. Struct. Geol.,28(6):952～956.
Parrish D K,Krivz A L,Carter N L.1976. Finite—element folds of similar geometry.Tectonophysics,32(3～4):183～207.
Passchier C W,Urai J L.1988.Vorticity and strain analysis using Mohrdiagrams.J Struct Geol,10(8):755～763.
Passchier C W,Trouw R A J.1996.Microtectonics. Springer-verlag Berlin Heidelberg:36～45.
Pfiffner O A,Ramsay J G.1982.Constraints on geological strain rates:Arguments from finite strain states of naturally deformed rocks. Journal of Geophysical Research,87(B1):311～321.
Song Chuanzhong,Zhu Guang,Liu Yang,Niu Manlan,Liu Guosheng.2003&.Deformation features and isotopic ages of the Feidong ductile shear belt in the Tanlu fault zone and its tectonic implications.Geological Review,49(1):10～17.
Song Chuanzhong,Huang Wencheng,Shoufa Lin,Ren Shenglian,Li Jiahao,Tu Wenchuan.2010a&.Features,attributes and research implications of transfer structure knots along the middle—lower Yangtze river reaches.Geology of Anhui,20(1):14～29.
Song Chuanzhong,Lin Shoufa,Zhou Taofa,Yan Jun,Ren Shenglian,Li Jiahao,Tu Wenchuan,Zhang Yan.2010b&.Mesozoic tectonic regime transition of the middle and lower reaches of the Yangtze river and its adjacent area.Acta Petrologica Sinica,26(9):2835～2849.
Song Chuanzhong,Zhang Hua,Ren Shenglian,Li Jiahao,Lin Shoufa,Tu Wenchuan,Zhang Yan,Wang Zhong.2011&.Transform Tectonic node of the middle and lower reaches of the Yangtze river and analysis of regional metallogenic settings.Acta Geological Sinica,85(5):778～788.
Song Chuanzhong,Li Jiahao,Ren Shenglian,Lin Shoufa,Liu Huan,Huang Peng,Wang Wei,Yang Fan.2014&.Mesozoic intracontinental tectonism and its genesis analysis of the middle—lower reaches of the Yangtze River.Chinese Journal of Geology,49(2):339～354.
Stipp M,Stunitz H,Heilbronner R, Schmid S M. 2002.The eastern Tonalefault zone:A natural laboratory for crystal plastic deformation ofquartz overa temperature range from 250 to 700℃.Journal of Structural Geology,24(12):1861～1884.
Takahashi M,Nagahama H,Masuda T.1998.Fractal analysis of experimentally,dynamically recrystallized quartz grains and its possible application as a strain rats meter. Journal of Structural Geology,20(2～3):269～275.
Tang Jiafu, Xu Wei. 2002&. No huge strike slip in the southern sector of the Tancheng—Lujiang fault——Tectonic evidence from Anhui Province. Geological Review, 48(5):449～456.
Tang Jiafu,Li Huaikun,Lou Qing.2003&.Progress in the study of the southern segment of the Tanlu Fault and a discussion of the nature of the fault.Geological Bulletin of China,22(6):426～436.
Tikoff B,Fossen H.1995.The limitati ons of three-dimensional kinematic vorticity analysis.Journal of Structural Geology,17(12):1771～1784.
Twiss R J.1977.Theory and application of a recrystallized grainsize paleopiezometer.Pure Applied Geophysics,115(1～2):227～244.
Vissers R L M.1989.Asymmetric quartz c-axis fabrics and flow vorticity:astudy using rotated garnets.Journal of Structural Geology,11(3):231～144.
Wallis S R.1992. Vorticity analysis in a metachert from the Sanbagawabelt,SW Japan.Journal of Structural Geology,14(3):271～280.
Wallis S R. 1995. Vorticity analysis and recognition of ductile extension in Sanbagawa belt,SW Japan.Journal of Structural Geology,17(8):1077～1094.
Wan Guimei,Tang Liangjie,Jin Wenzheng,Yu Yixin.2009&.Progresses and problems in the study of Tancheng—Lujiang Fault Zone. Geological Review,55(2):251～259.
Wan Tianfeng,Zhu Hong,Zhao Lei,Lin Jianping,Cheng Jie,Chen Jin.1996&.Formation and evolution of Tancheng—Lujiang fault zone:A review.Geoscience,10(2):159～168.
Wang Shuqin,Sun Xiaomeng,Du Jiyu,Wang Yingde,Xu Qiangwei,Tian Jingxiong.2012&.Analysis of structural styles in northern segment of Tancheng—Lujiang Fault Zone. Geological Review,58(3):414～425.
Wang Wei,Song Chuanzhong,Ren Shenglian,Li Jiahao,Zhang Yan,Wang Peipei,Hu Da.2016a&.P—T conditions and zircon U-Pb analysis of the Taoyuan ductile shear zone in Tan-Lu fault zone. Acta Petrologica Sinica,3(32):787～803.
Wang Wei,Song Chuanzhong,Li Jiahao,Ren Shenglian,Zhang Yan,Feng Lamei,Li Zhenwei,Wang Yangyang.2016b&.Structural and geochronology characteristics of Taoyuan ductile shear zone in Tanlu fault belt and their significance.Chinese Journal of Geology,51(4):1040～1058.
Wang Xiaofeng.2000#.The Tanlu Fault Zone. Beijing: Geological Publishing House.
Wang Xinshe,Zhang Shangkun,Zhang Fuzhong,Yang Chonghui.2005&.Kinematic vorticities and shear types of the Qingyi ductile shear zone in western Shandong.Acta Geoscientica Sinica,26(5):423～428.
Wang Yongsheng,Zhu Guang,Wang Daoxuan,Liu Guosheng,Song Chuanzhong.2004a&.Relation between P—T contitions of two phases of Tanlu strike-slip shear zones and delamination of the orogenic belts on the eastern margin of the Dabie mountains.Geotectonica et Metallogenia,28(3):228～238.
Wang Yongsheng,Zhu Guang.2004b&.The kinematic vorticity number and its measurement.Journal of Hefei University of Technology,27(11):1480～1484.
Wang Yongsheng,Zhu Guang,Wang Daoxuan,Song Chuanzhong,Liu Guosheng.2005&.An attempt to apply three geothermometers in the interpretation of low-temperature mylonites in the southern segment of the Tanlu fault zone.Geology in China,32(4):625～633.
Wang Yongsheng,Zhu Guang,Song Chuanzhong,Liu Guosheng.2006&.Vorticity analysis of the late ductile shear zone in the southern segment of the Tancheng—Lujiang Fault Zone and its tectonic significances. Geological Review,52(5):591～600.
Xiang Biwei,Zhu Guang,Wang Yongsheng,Xie Chenglong,Hu Zhaoqi.2007&. Mineral deformation thermometer for mylonitization. Advances in Earth Science,22(2):126～135.
Xiao Wenjiao,Zhou Yaoxiu,Yang Zhenyu,Zhao Xixi.2000&.Multiple rotation and amalgamation processes of Dabie—Tanlu—Sulu orogeny.Avdance in Earth Sciences,15(2):147～153.
Xu Jiawei.1980#. Translational movement and geological significance of Tan-Lu fault zone. Academic Papers on International Exchange Geology (1): Structural Geology, Geomechanics. Beijing: Geological Publishing House: 129～142.
Xu Jiawei. 1985&. Some advances in the study of the great horizontal displacement along the northern Tancheng—Lujiang fracture zone. Geological Review, 31(1):83～86.
Xu Jiawei,Wang Ping,Ching Rengao,Ye Zhoujie.1986.Ductile deformation and regional strain field in the southern segment of the Tancheng—Lujiang fault zone,castern China.Pure Applied Geophys,124(1～2):337～364.
Xu Jiawei,Zhu Guang,Tong Weixing,Cui Kerei,Liu Qing.1987.Formation and evolution of the Tancheng—Lujiang wrench fault system:a major shear system to the northwest of the Pacific Ocean.Tectonophysics,134(4):273～310.
Xu Jiawei, Ma Guofeng. 1992&. Review of ten years(1981～1991) of research on the Tancheng—Lujiang fault zone. Geological Review,38(4):316～324.
Xu Jiawei,Zhu Guang,L Peiji,Zheng Xuexin,Sun Shiqun.1995&.Progress in studies on strike-slip chronology of the Tanlu fault zone.Geology of Anhui,5(1):1～12.
Xu Shutong,Jiang Laili,Liu Yican,Zhang Yong.1992&.Tectonic framework and evolution of the Dabie mountains in Anhui,eastern China.Acta Geological Sinica,66(1):1～14.
Xue Dejie,Xu Xianbing,Li Yuan,Zhang Zejun,Lou Fasheng.2014&.Structural characteristics and deformation mechanism of early Paleozoic Granite in the Wugongshan Area,South China.Acta Geological Sinica,88(7):1236～1246.
Yan Lejia,Zhu Guang,LinShaoze,Zhao Tian.2014#.Neotectonic activity and formation mechanism of the Yishu fault zone.Science China(Series D),44(7):1452～1467.
Yang Wencai,Yu Changqing. 2001&. Kinetics and dynamics of development of the Dabie—Sulu UHPM terranes based on geophysical evidences. Chinese Journal of Geophysics,44(3):346～359.
Yin An,Nie Shangyou.1993.An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault system,eastern Asia.Tectonics,12(4):801～813.
Zhang Bo,Zhang Jinjiang,Guo Lei.2006&.Fractal analysis of dynamically recrystallized quartz grains and estimation of mainly rheological parameters of the Ranba ductile shear zone,northern Himalayan dome belt.Chinese Journal of Geology,41(1):158～169.
Zhang Kaijun.1997.North and South China collision along the eastern and southern North China margins.Tectonphysics,270(1～2):145～156.
Zhang Peng,Wang Liangshu,Zhong Kai,Ding Zengyong.2007&.Research on the segmentation of Tancheng—Lujiang Fault Zone. Geological Review,53(5):586～591.
Zhang Yueqiao,Dong Shuwen.2008&.Mesozoic tectonic evolution history of the Tanlu fault zone,China:Advances and new understanding.Geological Bulletin of China,27(9):1371～1390.
Zhao Tian,Zhu Guang,Lin Shaoze,Song lihong.2014a&.Protolith ages of metamorphic rocks of the Zhangbaling group along the southern segment of the Tanlu fault zone and their tectonic implications.Geological Review,60(6):1266～1283.
Zhao Tian,Zhu Guang,Lin Shaoze,Yan Lejia,Jiang Qinqin.2014b#. Protolith ages and deformation mechanism of metamorphic rocks in the Zhangbaling uplift segment of the Tanlu fault zone.Science China(Series D),44(10):2112～2129.
Zhao Tian,Zhu Guang,Xiang Biwei,Lin Shaoze,Gu Chengchuan.2016&.Discussion on initial mechanism of the Tanlu fault zone.Bulletin of Mineralogy,Petrology and Geochemistry,35(6):1120～1140.
Zheng Yadong,Wang Tao,Zhang Jinjiang.2008&.Theory and practice of kinematic vorticity(Wt).Earth Science Frontiers,15(3):209～220.
Zhu Guang,Xu Jiawei, Sun Shiqun.1995&.Isotopic age evidence for the timing of strike-slip movement of the Tan-Lu Fault Zone. Geological Review,41(5):452～456.
Zhu Guang,Niu Manlan,Liu Guosheng,Wang Daoxuan,Song Chuanzhong.2002&.Structural,Magmatic and Sedimentary Events of the Tanlu fault belt during its early cretaceous strike-slip movement.Acta Geologica Sinica,76(3):325～334.
Zhu Guang,Wang Daoxuan,Liu Guosheng,Niu Manlan,Song Chuanzhong.2004a&.Evolution of the Tanlu fault zone and its responses to plate movements in west pacific basin.Chinese Journal of Geology,39(1):36～49.
Zhu Guang,Wang Yongsheng,Niu Manlan,Liu Guosheng,Xie Chenglong.2004b&. Synorogenic movement of the Tanlu Fault Zone. Earth Science Frontiers,11(3):169～182.
Zhu Guang,Hou Mingjin,Wang Yongsheng,Liu Guosheng,Niu Manlan.2004.Thermal evolution of the Tan-Lu fault zone on the eastern margin of the Dabie mountains and Its tectonic implications.Acta Geologica Sinica(English edition),78(4):940～953.
Zhu Guang,Niu Manlan,Liu Guosheng,Wang Yongsheng,Xie Chenglong,Li Changcheng.2005&.40Ar/39Ar dating for the strike-slip movement on the Feidong part of the Tanlu fault belt.Acta Geologica Sinica,79(3):303～316.
Zhu Guang,Zhang Li,Xie Chenglong,Niu Manlan,Wang Yongsheng.2009&.Geochronological constraints on tectonic evolution of the Tanlu fault zone.Chinese Journal of Geology,44(4):1327～1342.
Zhu Guang,Wang Wei,Gu Chengchaun,Zhang Shuai,Liu Cheng.2016&.Late mesozoic evolution history of the Tanlu fault zone and its indication to destruction processes of the north China craton.Acta Petrologica Sinica,32(4):935～949.
董树文,吴宣志,高锐,卢德源,李英康,何义权,汤加富,曹奋扬,侯明金,黄德志.1998.大别造山带地壳速度结构与动力学.地球物理学报,41(3):349～361.
侯明金,王永敏,Jacques M,Pierre V.2003.郯庐断裂带(安徽部分)动力学演化及其构造意义.地质通报,22(2):105～112.
侯明金,Jacques M,Pierre V,王永敏.2006.郯庐断裂带的两大发展阶段——广义的逆冲推覆断裂带和狭义的平移断裂带.中国地质,33(6):1267～1275.
胡惟,朱光,严乐佳,詹润.2014.郯庐断裂带中段地震活动性与深部地壳电性结构关系的探讨. 地质论评,60(1):80～90.
李建波,郭磊,鲁勇花,曾涛.2017.华北克拉通北缘医巫闾山韧性剪切拆离带的运动学涡度与韧性减薄量.地质论评,63(6):1429～1439.
李曙光,刘德良,陈移之,王松山,裘冀,胡世玲,桑海清.1993.中国中部蓝片岩的形成时代.地质科学,28(1):21～27.
李振生,田晓莉,张文俊,陶冶. 2013.安徽桐城挂车河镇地区东西向韧性剪切带分形特征及其估算应变速率适用性分析.科技导报,31(20):15～19.
刘备,朱光,胡红雷,宋利宏.2015.郯庐断裂带江苏段新构造活动规律分析.地质学报,89(8):1352～1366.
乔秀夫.1981.对郯—庐断裂巨大平移之质疑. 地质论评,27(3):222-224.
宋传中,朱光,刘洋,牛漫兰,刘国生.2003.郯庐断裂带肥东韧性剪切带的变形规律、同位素年龄及其构造意义.地质论评,49(1):10～17.
宋传中,黄文成,Shoufa Lin,任升莲,李加好,涂文传.2010a.长江中下游转换构造结的特征、属性及其研究意义.安徽地质,20(1):14～29.
宋传中,Lin Shoufa,周涛发,闫峻,任升莲,李加好,涂文传,张妍.2010b.长江中下游及其邻区中生代构造体制转换.岩石学报,26(9):2835～2849.
宋传中,张华,任升莲,李加好,Lin Shoufa,涂文传,张妍,王中.2011.长江中下游转换构造结与区域成矿背景分析.地质学报,85(5):778～788.
宋传中,李加好,任升莲,Lin Shoufa,刘欢,黄鹏,王微,杨帆.2014.长江中下游地区中生代陆内构造作用与成因分析.地质科学,49(2):339～354.
汤加富,许卫.2002.郯庐断裂带南段并无巨大平移——来自安徽境内的证据. 地质论评, 48(5):449～456.
汤加富,李怀坤,娄清.2003.郯庐断裂南段研究进展与断裂性质讨论.地质通报,22(6):426～436.
万桂梅,汤良杰,金文正,余一欣.2009.郯庐断裂带研究进展及存在问题探讨.地质论评,55(2):251～259.
万天丰,朱鸿,赵磊,林建平,程捷,陈进.1996.郯庐断裂带的形成与演化:综述.现代地质,10(2):159～168.
王书琴,孙晓猛,杜继宇,王英德,许强伟,田景雄.2012.郯庐断裂带北段构造样式解析.地质论评,58(3):414～425.
王微,宋传中,任升莲,李加好,张妍,汪佩佩,胡达.2016a.郯庐断裂带中桃源韧性剪切带剪切温压条件及锆石U-Pb分析.岩石学报,32(3):787～803.
王微,宋传中,李加好,任升莲,张妍,冯腊梅,李振伟,王阳阳.2016b.郯庐断裂带肥东桃源韧性剪切带构造分析及时限探究.地质科学,51(4):1040～1058.
王小凤.2000.郯庐断裂带.地质出版社.
王新社,郑亚东,杨崇辉,侯贵廷.2001.用动态重结晶石英颗粒的分形确定变形温度及应变速率.岩石矿物学杂志,20(1):36～41.
王勇生,朱光,王道轩,刘国生,宋传中.2004a.大别山东缘郯庐两期走滑剪切带形成的温压条件与造山带折返的关系.大地构造与成矿学,28(3):228～238.
王勇生,朱光.2004b.运动学涡度及其测量方法.合肥工业大学学报,27(11):1480～1484.
王勇生,朱光,王道轩,宋传中,刘国生.2005.地质温度计在郯庐断裂带南段低温糜棱岩中的尝试.中国地质,32(4):625～633.
王勇生,朱光,宋传中,刘国生.2006.郯庐断裂带南段晚期韧性剪切带涡度分析及其构造意义.地质论评,52(5):591～600.
向必伟,朱光,王勇生,谢成龙,胡召齐.2007.糜棱岩化过程中矿物变形温度计.地球科学进展,22(2):126～135.
肖文交,周烑秀,杨振宇,赵西西.2000.大别—郯庐—苏鲁造山带复合旋转拼贴作用.地球科学进展,15(2):147～153.
徐嘉炜. 1980. 郯庐断裂带的平移运动及其地质意义. 见: 国际交流地质学术论文集(1):构造地质,地质力学. 北京: 地质出版社: 129～142.
徐嘉炜.1985.郯庐断裂带北段平移研究的若干进展——答乔秀夫的“对郯庐断裂巨大平移质疑”. 地质论评,31(1):83～86.
徐嘉炜,马国锋.1992.郯庐断裂带研究的十年回顾. 地质论评,38(4):316～324.
徐嘉炜,朱光,吕培基,郑学信,孙世群.1995.郯庐断裂带平移年代学研究的进展.安徽地质,5(1):1～12.
徐树桐,江来利,刘怡灿,张勇.1992.大别山区(安徽部分)的构造格局和演化过程.地质学报,66(1):1～14.
薛德杰,徐先兵,李源,章泽军,楼法生.2014.华南武功山早古生代花岗岩构造变形特征及其形成机制,地质学报,88(7):1236～1246.
严乐佳,朱光,林少泽,赵田.2014.沂沭断裂带新构造活动规律与机制.中国科学(D辑),44(7):1452～1467.
杨文采,于常青. 2001.根据地球物理资料分析大别-苏鲁超高压变质带演化的运动学与动力学.地球物理学报,44(3):346～359.
张波,张进江,郭磊.2006.北喜马拉雅穹隆带然巴韧性剪切带石英动态重结晶颗粒的分维几何分析与主要流变参数的估算.地质科学,41(1):158～169.
张鹏,王良书,钟锴,丁增勇.2007.郯庐断裂带的分段性研究.地质论评,53(5):586～591.
张岳桥,董树文.2008.郯庐断裂带中生代构造演化史:进展与新认识.地质通报,27(9):1371～1390.
赵田,朱光,林少泽,宋利宏.2014a.郯庐断裂带南段张八岭群变质岩的原岩时代及其构造意义.地质论评,60(6):1266～1283.
赵田,朱光,林少泽,严乐佳,姜芹芹.2014b.郯庐断裂带张八岭隆起段变质岩的原岩时代与变形机制.中国科学(D辑),44(10):2112～2129.
赵田,朱光,向必伟,林少泽,顾承串.2016.郯庐断裂带起源机制的探讨.矿物岩石地球化学通报,35(5):1120～1140.
郑亚东,王涛,张进江.2008.运动学涡度的理论与实践.地学前缘,15(3):209～220.
朱光,徐嘉炜,孙世群.1995.郯庐断裂带平移时代的同位素年龄证据.地质论评,41(5):452～456.
朱光,牛漫兰,刘国生,王道轩,宋传中.2002.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件.地质学报,76(3):325～334.
朱光,王道轩,刘国生,牛漫兰,宋传中.2004a.郯庐断裂带的演化及其对西太平洋板块运动的响应.地质科学,39(1):36～49.
朱光,王勇生,牛漫兰,刘国生,谢成龙.2004b.郯庐断裂带的同造山活动.地学前缘,11(3):169～182.
朱光,牛漫兰,刘国生,王勇生,谢成龙,李长城2005.郯庐断裂带肥东段走滑运动的40Ar /39Ar法定年.地质学报,79(3):303～316.
朱光,张力,谢成龙,牛漫兰,王勇生.2009.郯庐断裂带构造演化的同位素年代学制约.地质科学,44(4):1327～1342.
朱光,王薇,顾承串,张帅,刘程.2016.郯庐断裂带晚中生代演化历史及其对华北克拉通破坏过程的指示.岩石学报,32(04):935～949.
Chung Sunlin. 1999.Trace element and isotope characteristics of Cenozoic basalts around the Tanlu Fault with implications for the eastern plate boundary between North and South China.The Journal of Geology,107(3):301～312.
Chen Xuanhua,Wang Xiaofeng,Zhang Qing,Chen Bolin,Chen Zhengle,Harrison T Mark,Yin An.2000&.Gechronologic study on the formation and evolution of Tanlu fault.Journal of Changchun University of Science and Technology,30(3):215～220.
De Paor D G.1983.Orthographic analysis of geologic structures—I.Deformation theory.Journal of Structural Geology,5(3):255～278.
Dong Shuwen,Wu Xuanzhi,Gao Rui,Lu Deyuan,Li Yingkang,He Yiquan,Tang Jiafu,Cao Fenyang,Hou Mingjin,Huang Dezhi.1998&.On the crust velocity levels and dynamics of the Dabieshan orogenic belt.Acta Geophysica Sinica,41(3):349～361.
Hou Mingjin,Wang Yongmin,Jacques M,Pierre V.2003&.Dynamic evolution and tectonic significance of the Tanlu fault zone(Anhui segment).Geological Bulletin of China,22(2):105～112.
Hou Mingjin,Jacques M,Pierre V,Wang Yongmin.2006&.Two development stages of the Tanlu fault zone:the stages of the overthrust fault zone sensu lato and the wrench fault zone sensu stricto.Geology in China,33(6):1267～1275.
Hu Wei, Zhu Guang, Yan Lejia, Zhan Run. 2014&. Analysis of relationship between seismic activity and crust electrical textures for the central segment of the Tan-Lu fault zone. Geological Review,60(1):80～90.
Kruhl J H,Nega M and MillaH E.1995.The fractal shape of grain boundary sutures:reality,modeland application asa geo-thermometer.Book of Abstracts,2nd In.t Con.f on Fractaland.Dynamic Systems in Geosciences,84 Frankfort:31～32.
Kruhl J H,Nega M.1996.The fractal shape of sutured quartz grain boundaries:application as a geothermometer.Geologishe Rundschau,85(1):38～43.
Li Jianbo,Guo Lei,Lu Yonghua,Zeng Tao.2017&.The kinematic vorticity and the ductile thinning of the YiwulüShan ductile shear detachment zone in North China Craton. Geological Review,63(6):1429～1439.
Li Shuguang,Liu Deliang,Chen Yizhi,Wang Songshan,Qiu Ji,Hu Shiling,Sang Haiqing.1993&.Time of the blueschis belt formation in central China.Scientia Geological Sinica,28(1):21～27.
Li Zhensheng,Tian Xiaoli,Zhang Wenjun,Tao Ye.2013&.Fractal analysis of east—west ductile shear zone in Guachehe town area,Tongcheng,Anhui and its applicability of strain-rate estimation.Science & Technology Review,31(20):15～19.
Li Zhengxiang.1994.Collision between the north and south China blocks:A crust-detachment model for suturing in the region east of the Tan-Lu fault.Geology,22(8):739～742.
Liu Bei,Zhu Guang,Hu Honglei,Song Lihong.2015&.Analysis on neotectonic activity of the Jiangsu Part of the Tan-Lu Fault Zone.Acta Geologica Sinica,89(8):1352～1366.
Matthews P E,Bond R A,Vallden Berg J.1974.Analgebraic method of strain analysis using ellipitical markers.Tectonopbysics,24(1～2):31～67.
Means W D,Hobbs B E,Lister G S, Willianms P F.1980.Vorticity and non-coaxialicy in progressive deformation.Journal of Structural Geology,2(3):371～378.
Qiao Xiufu. 1981&. Doubts concerning the great horizontal displacement along the Tancheng—Lujiang fault zone. 1981. Geological Review,27(3):222～224.
Orife T,Lisle R J.2006.Assessing the statistical significance of palaeostress estimates:Simulations using random fault slips. J. Struct. Geol.,28(6):952～956.
Parrish D K,Krivz A L,Carter N L.1976. Finite—element folds of similar geometry.Tectonophysics,32(3～4):183～207.
Passchier C W,Urai J L.1988.Vorticity and strain analysis using Mohrdiagrams.J Struct Geol,10(8):755～763.
Passchier C W,Trouw R A J.1996.Microtectonics. Springer-verlag Berlin Heidelberg:36～45.
Pfiffner O A,Ramsay J G.1982.Constraints on geological strain rates:Arguments from finite strain states of naturally deformed rocks. Journal of Geophysical Research,87(B1):311～321.
Song Chuanzhong,Zhu Guang,Liu Yang,Niu Manlan,Liu Guosheng.2003&.Deformation features and isotopic ages of the Feidong ductile shear belt in the Tanlu fault zone and its tectonic implications.Geological Review,49(1):10～17.
Song Chuanzhong,Huang Wencheng,Shoufa Lin,Ren Shenglian,Li Jiahao,Tu Wenchuan.2010a&.Features,attributes and research implications of transfer structure knots along the middle—lower Yangtze river reaches.Geology of Anhui,20(1):14～29.
Song Chuanzhong,Lin Shoufa,Zhou Taofa,Yan Jun,Ren Shenglian,Li Jiahao,Tu Wenchuan,Zhang Yan.2010b&.Mesozoic tectonic regime transition of the middle and lower reaches of the Yangtze river and its adjacent area.Acta Petrologica Sinica,26(9):2835～2849.
Song Chuanzhong,Zhang Hua,Ren Shenglian,Li Jiahao,Lin Shoufa,Tu Wenchuan,Zhang Yan,Wang Zhong.2011&.Transform Tectonic node of the middle and lower reaches of the Yangtze river and analysis of regional metallogenic settings.Acta Geological Sinica,85(5):778～788.
Song Chuanzhong,Li Jiahao,Ren Shenglian,Lin Shoufa,Liu Huan,Huang Peng,Wang Wei,Yang Fan.2014&.Mesozoic intracontinental tectonism and its genesis analysis of the middle—lower reaches of the Yangtze River.Chinese Journal of Geology,49(2):339～354.
Stipp M,Stunitz H,Heilbronner R, Schmid S M. 2002.The eastern Tonalefault zone:A natural laboratory for crystal plastic deformation ofquartz overa temperature range from 250 to 700℃.Journal of Structural Geology,24(12):1861～1884.
Takahashi M,Nagahama H,Masuda T.1998.Fractal analysis of experimentally,dynamically recrystallized quartz grains and its possible application as a strain rats meter. Journal of Structural Geology,20(2～3):269～275.
Tang Jiafu, Xu Wei. 2002&. No huge strike slip in the southern sector of the Tancheng—Lujiang fault——Tectonic evidence from Anhui Province. Geological Review, 48(5):449～456.
Tang Jiafu,Li Huaikun,Lou Qing.2003&.Progress in the study of the southern segment of the Tanlu Fault and a discussion of the nature of the fault.Geological Bulletin of China,22(6):426～436.
Tikoff B,Fossen H.1995.The limitati ons of three-dimensional kinematic vorticity analysis.Journal of Structural Geology,17(12):1771～1784.
Twiss R J.1977.Theory and application of a recrystallized grainsize paleopiezometer.Pure Applied Geophysics,115(1～2):227～244.
Vissers R L M.1989.Asymmetric quartz c-axis fabrics and flow vorticity:astudy using rotated garnets.Journal of Structural Geology,11(3):231～144.
Wallis S R.1992. Vorticity analysis in a metachert from the Sanbagawabelt,SW Japan.Journal of Structural Geology,14(3):271～280.
Wallis S R. 1995. Vorticity analysis and recognition of ductile extension in Sanbagawa belt,SW Japan.Journal of Structural Geology,17(8):1077～1094.
Wan Guimei,Tang Liangjie,Jin Wenzheng,Yu Yixin.2009&.Progresses and problems in the study of Tancheng—Lujiang Fault Zone. Geological Review,55(2):251～259.
Wan Tianfeng,Zhu Hong,Zhao Lei,Lin Jianping,Cheng Jie,Chen Jin.1996&.Formation and evolution of Tancheng—Lujiang fault zone:A review.Geoscience,10(2):159～168.
Wang Shuqin,Sun Xiaomeng,Du Jiyu,Wang Yingde,Xu Qiangwei,Tian Jingxiong.2012&.Analysis of structural styles in northern segment of Tancheng—Lujiang Fault Zone. Geological Review,58(3):414～425.
Wang Wei,Song Chuanzhong,Ren Shenglian,Li Jiahao,Zhang Yan,Wang Peipei,Hu Da.2016a&.P—T conditions and zircon U-Pb analysis of the Taoyuan ductile shear zone in Tan-Lu fault zone. Acta Petrologica Sinica,3(32):787～803.
Wang Wei,Song Chuanzhong,Li Jiahao,Ren Shenglian,Zhang Yan,Feng Lamei,Li Zhenwei,Wang Yangyang.2016b&.Structural and geochronology characteristics of Taoyuan ductile shear zone in Tanlu fault belt and their significance.Chinese Journal of Geology,51(4):1040～1058.
Wang Xiaofeng.2000#.The Tanlu Fault Zone. Beijing: Geological Publishing House.
Wang Xinshe,Zhang Shangkun,Zhang Fuzhong,Yang Chonghui.2005&.Kinematic vorticities and shear types of the Qingyi ductile shear zone in western Shandong.Acta Geoscientica Sinica,26(5):423～428.
Wang Yongsheng,Zhu Guang,Wang Daoxuan,Liu Guosheng,Song Chuanzhong.2004a&.Relation between P—T contitions of two phases of Tanlu strike-slip shear zones and delamination of the orogenic belts on the eastern margin of the Dabie mountains.Geotectonica et Metallogenia,28(3):228～238.
Wang Yongsheng,Zhu Guang.2004b&.The kinematic vorticity number and its measurement.Journal of Hefei University of Technology,27(11):1480～1484.
Wang Yongsheng,Zhu Guang,Wang Daoxuan,Song Chuanzhong,Liu Guosheng.2005&.An attempt to apply three geothermometers in the interpretation of low-temperature mylonites in the southern segment of the Tanlu fault zone.Geology in China,32(4):625～633.
Wang Yongsheng,Zhu Guang,Song Chuanzhong,Liu Guosheng.2006&.Vorticity analysis of the late ductile shear zone in the southern segment of the Tancheng—Lujiang Fault Zone and its tectonic significances. Geological Review,52(5):591～600.
Xiang Biwei,Zhu Guang,Wang Yongsheng,Xie Chenglong,Hu Zhaoqi.2007&. Mineral deformation thermometer for mylonitization. Advances in Earth Science,22(2):126～135.
Xiao Wenjiao,Zhou Yaoxiu,Yang Zhenyu,Zhao Xixi.2000&.Multiple rotation and amalgamation processes of Dabie—Tanlu—Sulu orogeny.Avdance in Earth Sciences,15(2):147～153.
Xu Jiawei.1980#. Translational movement and geological significance of Tan-Lu fault zone. Academic Papers on International Exchange Geology (1): Structural Geology, Geomechanics. Beijing: Geological Publishing House: 129～142.
Xu Jiawei. 1985&. Some advances in the study of the great horizontal displacement along the northern Tancheng—Lujiang fracture zone. Geological Review, 31(1):83～86.
Xu Jiawei,Wang Ping,Ching Rengao,Ye Zhoujie.1986.Ductile deformation and regional strain field in the southern segment of the Tancheng—Lujiang fault zone,castern China.Pure Applied Geophys,124(1～2):337～364.
Xu Jiawei,Zhu Guang,Tong Weixing,Cui Kerei,Liu Qing.1987.Formation and evolution of the Tancheng—Lujiang wrench fault system:a major shear system to the northwest of the Pacific Ocean.Tectonophysics,134(4):273～310.
Xu Jiawei, Ma Guofeng. 1992&. Review of ten years(1981～1991) of research on the Tancheng—Lujiang fault zone. Geological Review,38(4):316～324.
Xu Jiawei,Zhu Guang,L Peiji,Zheng Xuexin,Sun Shiqun.1995&.Progress in studies on strike-slip chronology of the Tanlu fault zone.Geology of Anhui,5(1):1～12.
Xu Shutong,Jiang Laili,Liu Yican,Zhang Yong.1992&.Tectonic framework and evolution of the Dabie mountains in Anhui,eastern China.Acta Geological Sinica,66(1):1～14.
Xue Dejie,Xu Xianbing,Li Yuan,Zhang Zejun,Lou Fasheng.2014&.Structural characteristics and deformation mechanism of early Paleozoic Granite in the Wugongshan Area,South China.Acta Geological Sinica,88(7):1236～1246.
Yan Lejia,Zhu Guang,LinShaoze,Zhao Tian.2014#.Neotectonic activity and formation mechanism of the Yishu fault zone.Science China(Series D),44(7):1452～1467.
Yang Wencai,Yu Changqing. 2001&. Kinetics and dynamics of development of the Dabie—Sulu UHPM terranes based on geophysical evidences. Chinese Journal of Geophysics,44(3):346～359.
Yin An,Nie Shangyou.1993.An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault system,eastern Asia.Tectonics,12(4):801～813.
Zhang Bo,Zhang Jinjiang,Guo Lei.2006&.Fractal analysis of dynamically recrystallized quartz grains and estimation of mainly rheological parameters of the Ranba ductile shear zone,northern Himalayan dome belt.Chinese Journal of Geology,41(1):158～169.
Zhang Kaijun.1997.North and South China collision along the eastern and southern North China margins.Tectonphysics,270(1～2):145～156.
Zhang Peng,Wang Liangshu,Zhong Kai,Ding Zengyong.2007&.Research on the segmentation of Tancheng—Lujiang Fault Zone. Geological Review,53(5):586～591.
Zhang Yueqiao,Dong Shuwen.2008&.Mesozoic tectonic evolution history of the Tanlu fault zone,China:Advances and new understanding.Geological Bulletin of China,27(9):1371～1390.
Zhao Tian,Zhu Guang,Lin Shaoze,Song lihong.2014a&.Protolith ages of metamorphic rocks of the Zhangbaling group along the southern segment of the Tanlu fault zone and their tectonic implications.Geological Review,60(6):1266～1283.
Zhao Tian,Zhu Guang,Lin Shaoze,Yan Lejia,Jiang Qinqin.2014b#. Protolith ages and deformation mechanism of metamorphic rocks in the Zhangbaling uplift segment of the Tanlu fault zone.Science China(Series D),44(10):2112～2129.
Zhao Tian,Zhu Guang,Xiang Biwei,Lin Shaoze,Gu Chengchuan.2016&.Discussion on initial mechanism of the Tanlu fault zone.Bulletin of Mineralogy,Petrology and Geochemistry,35(6):1120～1140.
Zheng Yadong,Wang Tao,Zhang Jinjiang.2008&.Theory and practice of kinematic vorticity(Wt).Earth Science Frontiers,15(3):209～220.
Zhu Guang,Xu Jiawei, Sun Shiqun.1995&.Isotopic age evidence for the timing of strike-slip movement of the Tan-Lu Fault Zone. Geological Review,41(5):452～456.
Zhu Guang,Niu Manlan,Liu Guosheng,Wang Daoxuan,Song Chuanzhong.2002&.Structural,Magmatic and Sedimentary Events of the Tanlu fault belt during its early cretaceous strike-slip movement.Acta Geologica Sinica,76(3):325～334.
Zhu Guang,Wang Daoxuan,Liu Guosheng,Niu Manlan,Song Chuanzhong.2004a&.Evolution of the Tanlu fault zone and its responses to plate movements in west pacific basin.Chinese Journal of Geology,39(1):36～49.
Zhu Guang,Wang Yongsheng,Niu Manlan,Liu Guosheng,Xie Chenglong.2004b&. Synorogenic movement of the Tanlu Fault Zone. Earth Science Frontiers,11(3):169～182.
Zhu Guang,Hou Mingjin,Wang Yongsheng,Liu Guosheng,Niu Manlan.2004.Thermal evolution of the Tan-Lu fault zone on the eastern margin of the Dabie mountains and Its tectonic implications.Acta Geologica Sinica(English edition),78(4):940～953.
Zhu Guang,Niu Manlan,Liu Guosheng,Wang Yongsheng,Xie Chenglong,Li Changcheng.2005&.40Ar/39Ar dating for the strike-slip movement on the Feidong part of the Tanlu fault belt.Acta Geologica Sinica,79(3):303～316.
Zhu Guang,Zhang Li,Xie Chenglong,Niu Manlan,Wang Yongsheng.2009&.Geochronological constraints on tectonic evolution of the Tanlu fault zone.Chinese Journal of Geology,44(4):1327～1342.
Zhu Guang,Wang Wei,Gu Chengchaun,Zhang Shuai,Liu Cheng.2016&.Late mesozoic evolution history of the Tanlu fault zone and its indication to destruction processes of the north China craton.Acta Petrologica Sinica,32(4):935～949.