Bear J, Verruijt A. 1987. Modelling Groundwater Flow and Pollution. Boston: D. Reidel.
[2]
Jia C, Yuan F, Zhang M M, et al. 2014. Numerical simulation of the process of deposit formation in Baixiangshan iron deposit, Ningwu Basin. Acta Petrologica Sinica (in Chinese), 30(4): 1031-1040.
[3]
Jiang S D, Qin D X, Deng M G. 2006. Geochemical characteristics and their ore finding significance of Lutangba ore district in Gejiu tin mine. Mineral Resources and Geology (in Chinese), 20(6): 677-681.
[4]
Jiang Z W, Oliver N H S, Barr T D, et al. 1997. Numerical modeling of fault-controlled fluid flow in the genesis of Tin deposits of the Malage ore field, Gejiu mining district, China. Economic Geology, 92(2): 228-247.
[5]
Lü Q T,Dong S W,Shi D N, et al.2014.Lithosphere architecture and geodynamic model of Middle and Lower Reaches of Yangtze Metallogenic Belt:A review from SinoProbe.Acta Petrologica Sinica,30(4):889-906.
[6]
Lü Q T,Yan J Y,Shi D N, et al.2013.Reflection seismic imaging of the Lujiang-Zongyang volcanic basin,Yangtze Metallogenic Belt:An insight into the crustal structure and geodynamics of an ore district.Tectonophysics,606:60-77,doi:10.1016/j.tecto.2013.04.006.
[7]
Ma D Y, Gao Z M, Tao Y, et al. 2004. The characteristics of ore-controlling structures of the interbedded cassiterite-sulfide deposit, Gaosong ore field, Gejiu, Yunnan. Acta Mineralogica Sinica (in Chinese), 24(2): 153-156.
[8]
Meng W J, Chen Z A, Bai W M. 2015. Numerical simulation on process of the plume-lithosphere interaction. Chinese J. Geophys. (in Chinese), 58(2): 495-503, doi: 10.6038/cjg20150213.
[9]
Nield D A, Bejan A. 1992. Convection in Porous Media. New York: Spring-Verlag, 408 pp.
[10]
Ord A. 1991. Deformation of rock: a pressure-sensitive, dilatant material. Pure and Applied Geophysics, 137(4): 337-366.
[11]
Ord A, Oliver N H S. 1997. Mechanical controls on fluid flow during regional metamorphism: some numerical models. Journal of Metamorphic Geology, 15(3): 345-359.
[12]
Ramberg H. 1970. Folding of laterally compressed multilayers in the field of gravity, I. Phys. Earth Planet. Inter., 2(4): 203-232.
[13]
Ramsay J G, Huber M I. 1987. The Techniques of Modern Structural Geology. Vol. 2: Fold and Fractures. London: Academic Press.
Chen J Y, Yang X S, Shi Y L. 2009. A coupled thermal-fluid-solid approach for modeling the lithosphere-asthenosphere interactions. Chinese J. Geophys. (in Chinese), 52(4): 939-949, doi: 10.3969/j.issn.0001-5733.2009.04.010.
[22]
Cheng Y B, Mao J W, Xie G Q, et al. 2009. Zircon U-Pb dating of granites in Gejiu superlarge tin polymetallic orefield and its significance. Mineral Deposits (in Chinese), 28(3): 297-312.
[23]
Cundall P A, Board M. 1988. A microcomputer program for modelling large-strain plasticity problems.// Swoboda G Ed. Proceedings of the Sixth International Conference on Numerical Methods in Geomechanics. Numerical Methods in Geomechanics, 6: 2101-2108.
[24]
Currie J B, Patnode H W, Trump R P. 1962. Development of folds in sedimentary strata. Geol. Soc. Am. Bull., 73(6): 655-674.
[25]
Deng J, Yang L Q, Zhai Y S, et al. 2000. Theoretical framework and methodological system of tectonics-fluids-mineralization system and dynamics. Earth Science—Journal of China University of Geosciences (in Chinese), 25(1): 71-78.
[26]
Deng J, Wang Q F, Huang D H, et al. 2004. Structural control of ore-forming fluid activities in shallow crust of Tongling ore concentration area in Yanshanian Period. Mineral Deposits (in Chinese), 23(3): 399-404.
[27]
Fang W X, Hu R Z, Xie G Q, et al. 2002. Tectonolithostratigraphic units of the Ailaoshan area in Yunnan, China and their implications of tectonic evolution. Geotectonica et Metallogenia (in Chinese), 26(1): 28-36.
[28]
Fyfe W S, Kerrich R. 1985. Fluids and thrusting. Chem. Geol., 49(1-3): 353-362.
[29]
Gao J G, Nian H L, Chen S Y. 2004. Spatial distribution characteristics of mineralized fracture zone and metallogenetic elements in the south of Gejiu ore district, Yunnan province—Take Longshujiao fault as an example. Contributions to Geology and Mineral Resources Research (in Chinese), 19(4): 238-242.
[30]
Gao Y, Zhang S T. 2007. Study on vertical zoning of orefield structures in Laochang Tin orefield in Gejiu area, Yunnan province. Geotectonica et Metallogenia (in Chinese), 31(3): 335-341.
[31]
Gessner K. 2009. Coupled models of brittle-plastic deformation and fluid flow: approaches, methods, and application to Mesoproterozoic Mineralisation at Mount Isa, Australia. Surv. Geophys., 30(3): 211-232.
[32]
Han D M, Tan M. 2014. Rock and ore control feature of EW fault in E Gejiu area. Yunnan Geology (in Chinese), 33(1): 71-75.
[33]
Hobbs B E, Zhang Y, Ord A, et al. 2000. Application of coupled deformation, fluid flow, thermal and chemical modeling to Predictive mineral exploration. Journal of Geochemical Exploration, 69-70: 505-509.
[34]
Hu S Z, Fu L Y, Pei Z L. 2009. A boundary element method for the 2-D wave equation in fluid-saturated porous media. Chinese J. Geophys. (in Chinese), 52(9): 2364-2369, doi: 10.3969/j.issn.0001-5733.2009.09.022.
Jaeger J C, Cook N G W. 1979. Fundamentals of Rock Mechanics, 3rd rd. London: Chapman and Hall.
[37]
Li B L, Mao J W, Mo G P, et al. 2012. An analysis and measurement of joints developed in typical orefields of the Gejiu tin-copper polymetallic ore concentration area, Yunnan Province. Geology in China (in Chinese), 39(6): 1657-1669.
[38]
Lin G, Zhang Y, Guo F. 2005. Numerical modelling of lithosphere evolution in the North China Block: Thermal versus tectonic thinning. Journal of Geodynamics, 40(1): 92-103.
[39]
Liu L M, Zhao Y L, Sun T. 2012. 3D computational shape- and cooling process-modeling of magmatic intrusion and its implication for genesis and exploration of intrusion-related ore deposits: An example from the Yueshan intrusion in Anqing, China. Tectonophysics, 526-529: 110-123.
[40]
Lü B S. 2005. A new round of mineral prospecting and prospecting targets in Gejiu, Yunnan province. Geological Review (in Chinese), 51(6): 640-648.
[41]
Shang B C, Chen J P, Zheng X, et al. 2013. Three dimensional quantitative characteristics of fault structures in Gaosong Ore Field, Gejiu. Journal of Jilin University (Earth Science Edition) (in Chinese), 43(5): 1448-1456.
[42]
Sun J C, Jiang Z W, Zhou D P. 1988. Dynamic evolution of tectonic stress field and feature of control of ore deposits in Malage Orefield of Gejiu, Yunan. Journal of Kunming Institute of Technology (in Chinese), 13(3): 177-190.
[43]
Sun S Y. 2004. Study on the multi-episodic activity of faults in the Gaosong field of Gejiu Tin deposits. Acta Mineralogica Sinica (in Chinese), 24(2): 124-128.
[44]
Vermeer P A, de Borst R. 1984. Non-associated plasticity for soils, concrete and rock. Heron, 29(3): 1-62.
[45]
Yu C W, Tang Y J, Shi P F, et al. 1988. The Dynamic System of Endogenic Ore Formation in Gejiu Tin-Polimetallic Metallogenic Area, Yunnan Province (in Chinese). Wuhan: China University of Geosciences Press.
[46]
Zhai Y S. 1996. Problems in the study of structure-fluid-ore-forming processes. Earth Science Frontiers (in Chinese), 3(3-4): 230-236.
[47]
Zhang Y H, Lin G, Roberts P, et al. 2007. Numerical modelling of deformation and fluid flow in the Shuikoushan district, Hunan Province, South China. Ore Geology Reviews, 31(1-4): 261-278.
[48]
Zhang Y H, Robinson J, Schaubs P M. 2011. Numerical modelling of structural controls on fluid flow and mineralization. Geoscience Frontiers, 2(3): 449-461.
[49]
Zhao J J, Fang W X, Guo Y Q, et al. 2011. Study on Xinshan granite emplacement mechanism and metaliogenic relationship of Kafang ore field in Gejiu, Yunnan. Mineral Resources and Geology (in Chinese), 25(1): 53-58.
[50]
Zhou B, Sun F, Yan C H, et al. 2014. 3D-poreelastic finite element numerical simulation of Longtan reservoir-induced seismicity. Chinese J. Geophys. (in Chinese), 57(9): 2846-2868, doi: 10.6038/cjg20140911.
[51]
Zhuang Y Q, Wang R Z, Yang S P, et al. 1996. Gejiu Tin (Cu) Polymetallic Ore Deposits in Yunnan (in Chinese). Beijing: Seismological Press.
