解国爱 , 王宗秀 , 张庆龙 , 吕赟珊 , 邹旭 . 江西永平铜矿区古构造应力场与构造演化[J]. 地球科学进展, 2013 , 28(5) : 608 -617 . DOI: 10.11867/j.issn.1001-8166.2013.05.0608

[1]Carey E. Recherche des directions principales de contraintes associees au jeu d’une population de failles[J]. Revue de Géographie  Physique et  Gédogie Dynamique，1979，21：57-66.

[2]Fry N. A robust approach to the calculation of paleostress fields from fault plane data: Discussion[J]. Journal of Structural Geology，1992，14：635-637.

[3]Zhang Y Q, Dong S W, Shi W. Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province,eastern China[J]. Tectonophysics，2003，363: 243-258.

[4]Shan J, Suen H, Lin G. Separation of polyphase fault/slip data: An objective-function algorithm based on hard division[J]. Journal of Structural Geology，2003，25：829-840.

[5]Cao Daiyong, Zhan Wenfeng, Zhang Jun, et al. Study on the palaeotectonic stress fields and tectonic evolution in Handan-Fengfeng Coal Mining area[J]. Coal Geology of China, 2005, 17(5):1-3.[曹代勇，占文峰，张军，等. 邯峰矿区古构造应力场与构造演化[J].中国煤田地质，2005,17（5）：1-3.]

[6]Yamaji A. The multiple inverse method:A new technique to separate stresses from heterogeneous faultslip data[J].Journal of Structural Geology, 2000，22: 441-452.

[7]Yamaji A. Multiple inverse method applied to mesoscale faults in mid Quaternary sed-iments near the triple trench junction offcentral Japan[J]. Journal of Structural Geology, 2000，22(4)： 429-440.

[8]Yamaji A . Are the solutions of stress inversion correct? Visualization of their reliability and the separation of stresses from heterogeneous fault-slip data[J].Journal of Structural Geology，2003，25：241-252.

[9]Chan L S， Shen W L，Pubellier M. Polyphase rifting of greater Pearl River Delta region (South China): Evidence for possible rapid changes in regional stress con figuration[J]. Journal of Structural Geology，2010，32：746-754.

[10]Li Xiaofeng, Yasushi Watanabe, Qu Wenjun. Textures and geochemical characteristics of granitic rocks in the Yongping climaxtype Cu-Mo deposit,Jiangxi,southeastern China,and their alteration,mineralization and tectonic regime[J].Acta Petrlogica Sinica, 2007,23(10):2 353-2 365.[李晓峰，Yasushi Watanabe，屈文俊. 江西永平铜矿花岗质岩石的岩石结构、地球化学特征及其成矿意义[J]. 岩石学报，2007,23(10)：2 353-2 365.]

[11]Zhu Bi, Jiang Shaoyong, Ding Xin, et al. Hydrothermal alteration and petrogenesis of granites in the Yongping Copper Dposit,Jiangxi Province:Constraints from mineral chemistry,element geochemistry,and Sr-Nd-Hf isotopes[J]. Acta Petrlogica Sinica,2008,24(8):1 900-1 916.[朱碧，蒋少涌，丁昕，等. 江西永平铜矿区花岗岩热液蚀变与岩石成因：矿物化学、元素地球化学和Sr-Nd-Hf同位素制约[J]. 岩石学报，2008，24(8)：1 900-1 916.]

[12]Liu Xun, Huang Zhen. Tectono-geochemistry in the Yongping Copper Ore Field, Jiangxi[J]. Geological Review, 1992,38(4)：302-310.[刘迅，黄震. 江西永平铜矿田构造地球化学[J]. 地质论评，1992，38(4)：302-310.]

[13]Zhao Changsheng. The feature of syngenetic plume-sedimentation in Yongpin Copper Deposit, Jiangxi[J]. Copper Engineering, 2001,3:48-50.[赵常胜. 江西永平铜矿床以喷流成矿为主体的成因特征[J]. 铜业工程，2001，3：48-50.]

[14]Liao Zongting, Liu Jinshui. Evidences of submarine volcanic hydrothermal sedimentmineralization in Yongping Copper Deposit[J]. Copper Engineering, 2003, 1:31-35.[廖宗廷，刘金水. 永平铜矿海底火山热液沉积成矿作用的依据[J]. 铜业工程，2003，1：31-35.]

[15]Du Lingtong. Sources of ore-forming material and genesis analysis of Yongping Copper Deposit, Jiangxi[J]. Resources Environment and Engineering, 2005, 19(1)：4-11.[杜灵通. 江西永平铜矿成矿物质来源及矿床成因分析[J]. 资源环境与工程，2005，19(1)：4-11.]

[16]Tian Jinghui, Ni Pei, Fan Jianguo. Ore-forming fluid characteristics research of Yongping Copper Deposit[J]. Contributions to Geology and Mineral Resources Research,2001,16(1)：24-27.[田京辉，倪培，范建国. 永平铜矿成矿流体特征研究[J]. 地质找矿论丛，2001，16(1)：24-27.]

[17]Ni Pei, Tian Jinghui, Zhu Xiaoting, et al. Fluid inclusion studies on footwall stringer system  mineralization of Yongping Massive Copper Deposit, Jiangxi Province, China[J].Acta Petrologica Sinica, 2005,21(5)：1 139-1 146.[倪培，田京辉，朱筱婷，等. 江西永平铜矿下盘网脉状矿化的流体包裹体研究[J]. 岩石学报，2005，21(5)：1 139-1 146.]

[18]Ding Xin, Jiang Shaoyong, Ni Pei, et al. Zircon SIMS U-Pb geochronology of host granitoids in Wushan and Yongping Copper Deposits, Jiangxi Province[J]. Geological Journal of China Universities, 2005，11（3）：383-389.[丁昕，蒋少涌，倪培，等. 江西武山和永平铜矿含矿花岗质岩体锆石SIMS U-Pb年代学[J]. 高校地质学报，2005，11（3）：383-389.]

[19]Angelier J. Determination of the mean principal directions of stresses for a given fault population[J]. Tectonophysics,1979，56 (3/4)：17-26.

[20]Angelier J. Tectonic analysis of fault slip data sets[J].Journal of Geophysical Research, 1984，89: 5 835-5 848.

[21]Gephart J W, Forsyth D W. Animproved method for determining the regional stress tensor using earthquake focal mechanism data: Application to the San Fernando earthquake sequence[J]. Journal of Geophysical Research,1984, 89: 9 305-9 320.

[22]Ishii E, Yasue K, Takenobu T, et al. Three-dimensional distribution and hydrogeological properties of the Omagari Fault in the Horonobe area, northern Hokkaido Japan[J].Journal of the Geological Society of Japan, 2006,112: 301-314.

[23]Ishii E, Fukushima T. A case study of analysis of faul: Ts in Neogene siliceous rocks[J]. Journal of the Japan Society of Engineering Geology, 2006, 47: 280-291.

[24]Kuniyasu M, Yamada Y. Structural analysis of deep zones in southern central Hokkaido, northern Japan[J]. Journal of the Japanese Association for Petroleum Technology, 2004, 69: 131-144.

[25]Kusuhashi N，Yamaji A. Miocene tectonics of SW Japan as inferred from the Kuma Group, Shikoku[J]. Journal of the Geological Society of Japan, 2001, 107: 25-40.

[26]Eliassi M, Ahmadian S. Determination of the geometrical configuration of σ1 trajectory in KanKaraj area (Central Alborz) using Multiple Inverse Method[J]. Geosciences, 2007, 67: 140-149.

[27]Eliassi M, Mohajjel M，Mesbahi F. Paleostress analysis of horizontal Plio-Quaternary deposits in the NW of Zanjan[J]. Journal of Earth and Space Physics, 2008, 34: 27-42.

[28]Lunina O V, Gladkov A S. Active faults and crustal stress in the northeastern flank of the Baikal rift system[J]. Russian Geology and Geophysics, 2008, 49: 113-123.

[29]Lunina O X, Gladkov A S, Novikov I S, et al. Geometry of the fault zone of the 2003 Ms=7.5 Chuya earthquake and associated stress fields, Gorny Altai[J]. Tectonophysics, 2008, 453: 276-294.

[30]Haví[AKrˇ] J, Gilíkov H. Results of the structural study of the Culm sediments near Suchdol and Odrou[J]. Geological Research in Moravia and Silesia, 2007, 14:52-55.

[31]Sippel J, Scheck-Wenderoth M, Reicherter K, et al. Paleostress states at the south-western margin of the Central European Basin System—Application of fault-slip analysis to unravel a polyphase deformation pattern[J]. Tectonophysics, 2009, 470: 129-146.

[32]Viola G, Venvik Ganerd G, Wahlgren C H. Unraveling 1.5 Ga of brittle deformation history in the Laxemar-Simpevarp area, southeastern Sweden: A contribution to the Swedish site investigation study for the disposal of highly radioactive nuclear waste[J].Tectonics,2009,28: TC5007.

[33]Veloso E E, Anma R, Yamaji A. Ophiolite emplacement and the effects of the subduction of the active Chile Ridge System: Heterogeneous paleostress regimes recorded on the Taitao Ophiolite (southern Chile)[J]. Andean Geology, 2009, 36: 3-16.

[34]Yang Minggui, Huang Shuibao, Lou Fasheng, et al. Lithospheric structure and large-scale metallogenic process in Southeast China continental area[J]. Geology in China, 2009, 36(3):528-543.[杨明桂，黄水保，楼法生，等．中国东南陆区岩石圈结构与大规模成矿作用[J]．中国地质，2009，36(3)：528-543.]

[35]Mao Jingwen, Chen Maohong, Yuan Shunda, et al. Geological characteristics of the Qinhang (or Shihang) metallogenic belt in South China and spatial-temporal distribution regularity of mineral deposits[J]. Acta Geologica Sinica, 2011,85(5):636-658.[毛景文，陈懋弘，袁顺达，等. 华南地区钦杭成矿带地质特征和矿床时空分布规律[J]. 地质学报，2011,85（5）：636-658.]

[36]Shu Liangshu. Predevonian tectonic evolution of South China: From cathaysian block to caledonian period folded orogenic belt[J]. Geological Journal of China Universities, 2006, 12(4): 418-431.[舒良树．华南前泥盆纪构造演化：从华夏地块到加里东期造山带[J]．高校地质学报，2006, 12(4)：418-431.]

[37]Hu Zhaorong, Deng Guohui. Tectonic characteristics of the Qinzhou-Hangzhou joint belt[J]. Journal of East China Institute of Technology (Natural Science), 2009, 32(2): 114-122.[胡肇荣，邓国辉. 钦—杭接合带之构造特征[J]. 东华理工大学学报:自然科学版，2009, 32（2）：114-122.]

[38]Dong Shuwen, Zhang Yueqiao, Long Changxing, et al. Jurassic Tectonic revolution in China and new interpretation of the Yanshan movement[J]. Acta Geologica Sinica, 2007, 81(11): 1 449-1 461.[董树文，张岳桥，龙长兴，等.中国侏罗纪构造变革与燕山运动新诠释[J]．地质学报，2007,81(11)：1 449-1 461.]

[39]Zhang Yueqiao, Xu Xianbing, Jia Dong, et al. Deformation record of the change from Indosinian collision-related tectonic system to Yanshanian subduction-related tectonic system in South China during the Early Mesozoic[J]. Earth Science Frontiers, 2009,16(1): 234-247.[张岳桥，徐先兵，贾东，等．华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的变形记录[J]．地学前缘，2009, 16(1)：234-247.]

[40]Mao Jingwen, Xie Guiqing, Guo Chunli, et al. Spatial-temporal distribution of Mesozoic Ore deposits in South China and their metallogenic settings[J]. Geological Journal of China Universities,2008, 14(4): 510-526.[毛景文，谢桂青，郭春丽，等．华南地区中生代主要金属矿床时空分布规律和成矿环境[J]．高校地质学报，2008, 14(4)：510-526.]