[1]Deng Jun(邓军), Lü Guxian(吕古贤), Yang Liqiang(杨立强), et al.The transformation of tectonic stress field and interfacial metallogensis[J].Acta Geosicentia Sinica(地球学报), 1998,19(3): 244-250(in Chinese). [2]Deng Jun(邓军), Sun Zhongshi(孙忠实), Wang Jianping(王建平), et al.Dynamic system transformation and gold ore-forming process[J]. Mineral Deposits(矿床地质), 2001,20(1): 71-77(in Chinese). [3]Zhai Yusheng(翟裕生), Lü Guxian(吕古贤). Transition of tectonic and dynamic regime and mineralization[J]. Acta Geosicentia Sinica(地球学报),2002,23(2):97-102(in Chinese). [4]Sibon R H. Tectonic controls on maximum sustainable overpressure fluid redistribution from stress transition[J]. Journal of Geochemical Exploration, 2000,69~70:471-475. [5]Zhai Yusheng(翟裕生), Zhang Hu(张湖), Song Honglin(宋鸿林), et al.Macroscopic Structures and Superlarge Ore Deposits[M]. Beijing: Geological Publishing House, 1997. 150-151(in Chinese). [6]Zhai Yusheng(翟裕生), Deng Jun(邓军),Li Xiaobo(李晓波). Regional Metallogeny[M].Beijing: Geological Publishing House,1999.287(in Chinese). [7]Xu Jiuhua(徐九华), Xie Yuling(谢玉玲), Shen Shiliang(申世亮). Tectonic environment of hydrothermal gold deposits[J]. Acta Geosicentia Sinica(地球学报),1998,1 (2): 204-209(in Chinese). [8]Yang Weiran(杨巍然), Zhang Wenhuai(张文淮). Tectonic fluids—A new research domain[J]. Earth Science Frontiers(地学前缘), 1996, 21(3): 286-290(in Chinese). [9]Hubbert M K,Rubey W W. Roles of fluid pressure in mechanics of overthrust faulting[J]. AAPG Bulletin,1959,70 :167-206. [10]Bryant D G. Intrusive breccias associated with ore,warren (Bisbee) mining district,Arizona[J].Economic Geology,1968,63(1):1-12. [11]Norton D L,Cathles L M. Breccia pipes,products of exsolved vapor from magmas[J]. Economic Geology,1973,68(3):540-546. [12]Paul D Bons. The formation of large quartz veins by rapid ascent of fluids in mobile hydrofractures[J].Tectonophysics, 2001,336:1-17. [13]Tobin H,Vannucchil P,Meschede M.Structure, inferred mechanical properties, and implications for fluid transport in the decollement zone, Costa Rica Convergent Margin[J]. Geology,2001,29(10):907-910. [14]Liu Junlai(刘俊来), Ma Lijie(马立杰), Cui Yingchun(崔迎春), et al. Fluid flow and brittle to ductile transition of limestone under crustal conditions[J]. Earth Science Frontiers(地学前缘), 2001,8(3):171-176(in Chinese). [15]Wintsch R P,Christoffersen R,Kronenberg A K. Fluid-rock reaction weakening of fault zone[J].Journal of Geophysical Reaserch,1995,100(7):13 021-13 032. [16]Wawrzyniec T,Selverstone J,Axen G J. Correlations between fluid composition and deep-seated structural style in the footwall of the simplon low-angle normal fault, Switzerland[J].Geology,1999,27(8):715-718. [17]Read J J,Meinert L D. Goldbearing quartz vein mineralization atthe Big Hurrah Mine,Seward Peninsula,Alaska[J].Economic Geology,1986,81:1 760-1 764. [18]Robert E,Kelly W C. Ore-forming fluids in Archean gold-bearing quartz veins at the Sigma Mine,Abitibi Green-stone belt,Quebec,Canada[J]. Economic Geology,1987,82:1 464-1 482. [19]Walsh J F,Kesler S E. Fluid inclusion geochemistry of high-grade,vein-hosted gold ore at the Pamour Mine,Porcu-pire Camp,Ontario[J]. Economic Geology,1988,83:1 347-1 367. [20]Craw D. Fluid evolution, fluid immiscibility and gold deposition during Cretaceous-Recenttectonics and uplift of the Otago and Alpine Schist,New Zealand[J]. Chemical Geology,1992,82:221-236. [21]Guha J,Lu H Z,Dube B, et al. Fluid Characteristics of vein and altered wall rock in Archean mesothermal gold deposits[J]. Economic Geology,1991,86:667-684. [22]Craw D,Teagle D A H,Belocky R. Fluid immiscibility in late-Alpine gold-bearing veins,eastern and northwestern European Alps[J]. Mineralium Deposita,1993,28:28-36. [23]Bower T S. The deposition of gold and other metals: Press-induced fluid immiscibility and associated stable signatures[J]. Geochimica et Cosmochimica Acta, 1991, 55:2 417-2 434. [24]De-Bremond-d-Ars-Jean, Arndt-Nicholas-T, Hallot-Erwan. Analog experimental insights into the formation of magmatic sulfide deposits[J]. Earth and Planetary Science Letters, 2001,186(3~4): 371-381. [25]Tang Zhongli(汤中立), Li Wenyuan(李文渊). Metallogeny study and prospect of the nickel sulfide deposits in China[J] . Mineral Deposits(矿床地质), 1991,10 (3) : 193-203(in Chinese). [26]Rui Zongyao(芮宗瑶), Li Yinqing(李荫清), Wang Longsheng(王龙生), et al. Preliminary discussion on ore-forming fluids and enrichment systems of metallic minerals[J] .Mineral Deposits(矿床地质),2002,21(1):83-90(in Chinese). [27]Chen Bangguo(陈邦国), Jiang Zhangping(姜章平), Zhang Weiping(张卫平).Study on altered fluids of diplogenetic stratified copper hydrothermal solution in Dongguashan, Anhui province[J] . Jiangsu Geology(江苏地质), 2002, 26(2):65-69(in Chinese). [28]Snow D T. Anisotropic permeability of fractured media[J]. Water Resources Research, 1969, 5(6): 1 273-1 289. [29]Long J C S,Remer J S, Wilson C R, et al. Porous media equivalents for net-works of discontinuous fractures[J]. Water Resouces Research,1982,18(3):645-658. [30]Oda M. An equivalent continuum model for coupled stress and fluid flow analysis in jointed rock masses[J]. Water Resources Research,1986,22(13):1 845-1 856. [31]Yang Jianven, Latythev K, Edwards R N.Numerical computation of hydrothermal fluid circulation in fractured Earth structures[J]. Geophysical Journal International, 1998,135(2):627-649. [32]Sibson R H. Structural permeability of fluid-driven fault-fracture meshes[J].Journal of Structural Geology, 1996,18(8):1 031-1 042. [33]Rouleau A,Gale J E. Statistical characterization of the fracture system in the Stripa Granite, Sweden[J]. International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, 1985,22(6):353-367. [34]Odling N E, Webman I.A “conductance” mesh approach to the permeability of natural and simulated fracture patterns[J]. Water Resources Research, 1991, 27(10):2 633-2 643. [35]Deng Jun, Fang Yun, Yang Liqiang, et al. Numerical modelling of ore-forming dynamics of fractal dispersive fluid systems[J]. Acta Geologica Sinica, 2001,75(2):220-232. [36]Tang Y W. The effect of tortuosity on fluid flow through a single fracture[J].Water Resources Research,1984,20(9):1 209-1 215. [37]Zhang Youtuan, Liu Zhong. Hydraulic behavior of rock fractures analyzed by using fractal[A]. In: Liu Huaiheng, ed. Proceedings of International Symposium on Application of Computer Method in Rock Mechanics and Engineering[C]. Xi’an: Shaanxi Science and Technology Press,1993.427-434. [38]Warren J E, Root P J. The behavior of naturally fractured reservoirs[J]. Journal of Society Petroleum Engineering,1963,(3):245-255. [39]Bibby R. Mass transport of solutes in dual-porosity media[J]. Water Resources Research, 1981, 17(4):1 075-1 081. [40]Neretnieks I, Rasmuson A. Diffusion in the rock matrix: An important factor in radionudide retardation[J].Journal of Geophysical Research, 1980, 85(B8): 4 379-4 397. [41]Zimmerman R W, Chen G, Hadgu Tekluetal. A numerical dual-porosity model with asemi-analytical treatment of fracture/matrix flow[J]. Water Resources Research, 1993, 29(7): 2 127-2 137. [42]Robinson J W,Gale J E. A laboratory and numerical investigation of solute transport in discontinuous fracture systems[J].Ground Water,1990,28(1):25-36. [43]Neuman S P. Generalized scaling of permeabilities: Validation and effect of support scale[J].Geopysical Research letters, 1994, 1:349-352. [44]Neuman S P. Univeral scaling of hydraulic conductivities and dispersivities in geological media[J]. Water Resources Research,1990,26:1 749-1 758. [45]Gavrilenko P, Gueguen Y F. Flow in fractured medi: A modified renormalization method[J]. Water Resources Research,1998,34(2):177-191. [46]Walsh J B, Brace W F. The effect of pressure on porosity and the transport properties of rock[J]. Journal of Geophysical Research,1984,89:9 425-9 431. [47]Jiang Z W, Nicholas H S, Terence D, et al. Numerical modeling of fault-controlled fluid flow in the genesis of tin deposits of the Malage ore field, Gejiu mining district, China[J]. Economic Geology, 1997,92:228-247. [48]Itasca Consulting Group Inc. Universal distinct element code: Minneapolis, Minnesota, Itasca Consulting Group, Technical Manual, 1993. [49]Harper T R, Last N C. Response of fractal rock subject to fluid injection, Part 2: Characteristic behavior[J]. Tectonophysics, 1990,172:33-51. [50]Harper T R, Last N C. Response of fractal rock subject to fluid injection, Part 3: Practical application[J]. Tectonophysics, 1990,172:53-65. [51]Zhang X, Sanderson D J. Numerical modeling of the effects of fault slip on fluid flow around extensional faults[J]. Journal of Structural Geology,1996,18:109-119. [52]Huang Dinghua(黄定华),Xiang Shuyuan(向树元),Zhu Yunhai(朱云海). Cryptoexplosive mechanics and its significance for mechanism of mineralization[J]. Geological Science and Technology Information(地质科技情报), 1997, 16(1): 77-80(in Chinese). [53]Jügen E Streit, Stephen F Cox. Evolution of fracture networks in shear zones: Insights from see-through experiments on biphenyl aggregates[J].Journal of Structural Geology,2002,24:107-122. [54]Jean De Bremond d’Ars, Nicholas T Arndt, Erwan Hallot. Analog experimental insights into the formation of magmatic sulfide deposits[J]. Earth and Planery Science Letters, 2001,186:371-381. [55]Deng Jun(邓军),Yang Liqiang(杨立强),Zhai Yusheng(翟裕生),et al. Theoretical framework and methodological system of tectonics-fluid-mineralization system and dynamics[J].Earth Science—Journal of China University of Geosciences(地球科学——中国地质大学学报),2000,25(1): 71-78(in Chinese). |