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地质学报  2009 

富金斑岩铜矿床研究进展

, PP. 1997-2017

Keywords: 富金斑岩型铜矿,大地构造背景,高钾钙碱性岩浆,富金机制

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Abstract:

富金斑岩型铜矿床作为斑岩型矿床的一类,自20世纪70年代起逐渐引起了人们的重视。近年来又取得了很多重要进展,主要体现在以下5个方面:①富金斑岩型铜矿不仅在全世界范围内大量发现,而且部分矿床规模巨大;②绝大多数富金斑岩型矿床集中在新生代和中生代产出,尤以第三纪最为普遍;③富金斑岩型铜矿床不仅仅发育于汇聚板块边缘的岩浆弧环境,在大陆碰撞带甚至是陆内环境也发现了大量此类矿床;④含矿斑岩绝大多数为钙碱性岩浆系列,但部分矿床与高钾钙碱性(甚至钾玄质)岩浆密切相关;⑤富金斑岩型矿床金的富集,与大地构造背景、成矿时代、含矿斑岩性质、围岩性质、蚀变与矿化类型等因素关系不大,而主要受地幔岩浆过程、岩浆热液过程及热液过程控制。

References

[1]  Gustafson L B,Hunt J P,The porphyry copper deposit at El Salvador,Chile,Economic Geology,1975.
[2]  Halter W E,Pettke T,Heinrich C A,The origin of Cu/Au ratios in porphyry-type ore deposits,Science,2002.
[3]  Harris A C,Kamenetsky V S,White N C,Achterbergh E V Ryan C G,Melt inclusions in veins:linking magmas and porphyry Cu deposits,Science,2003.
[4]  Misra K C,Understanding mineral deposits,Kluwer Academic Publishers,2000.
[5]  Mpodozis C,Kay S M,Cornejo P,Tittler A,La Franja de Maricunga:s ntesis de la evoluci n del frente volc nico Oligoceno-Mioceno de la zona sur de los Andes Centrales,Revista Geol gica de Chile,1995.
[6]  Muntean J L,Einaudi M T,Porphyry gold deposits of the Refugio district,Maricunga belt,northern Chile,Economic Geology,2000.
[7]  Mustard R,Ulrich T,Kamenetsky V S,Mernagh T,Gold and metal enrichment in natural granitic melts during fractional crystallization,Geology,2006.
[8]  Sillitoe R H,Special Paper:Major gold deposits and belts of the North and South American cordillera:distribution,tectonomagmatic settings,and metallogenic considerations,Economic Geology,2008.
[9]  Singer D A,Cox D P,Grade and tonnage model of porphyry Cu-Au,US Geological Survey Bulletin,1986.
[10]  Singer D A,World class base and precious metal deposits:a quantitative analysis,Economic Geology,1995.
[11]  Singer D A,Berger V I,Menzie W D,Berger B R,Porphyry copper deposit density,Economic Geology,2005.
[12]  Tosdal R M,Richards J P,Magmatic and structural controls on the development of porphyry Cu±Mo±Au deposits,2001.
[13]  Ulrich T,Günther D,Heinrich C A,Gold concentrations of magmatic brines and the metal budget of porphyry copper deposits,Nature,1999.
[14]  Ulrich T,Heinrich C A,Geology and alteration geochemistry of the porphyry Cu-Au deposit at Bajo de la Alumbrera Argentina,Economic Geology,2001.
[15]  Ulrich T,Guünthur D,Heinrich C A,The evolution of a poprphyry Cu-Au deposit,based on LA-ICP-MS analysis of fluid inclusions:Bajo de la Alumbrera,Argentina,Economic Geology,2002.
[16]  van Dongen M,Weinberg R F,Tomkins A G,Armstrong R A,Woodhead J D,Recycling of Proterozoic crust in Pleistocene juvenile magma and rapid formation of the Ok Tedi porphyry Cu-Au deposit,Papua New Guinea,Lithos,2009.
[17]  Vila T,Sillitoe R H,Gold-rich porphyry systems in the Maricunga belt,northern Chile,Economic Geology,1991.
[18]  Vila T,Sillitoe R H,Betzhold J,Viteri E,The porphyry gold deposits at Marte,northern Chile,Economic Geology,1991.
[19]  Weiland R J,Cloos M,Pliocene-Pleistocene asymmetric unroofing of the Irian fold belt,Irian Jaya,Indonesia:apatite fission-track thermochronology,Geological Society of America Bulletin,1995.
[20]  Williams-Jones A E,Heinrich C A,Vapor transport of metals and the formation of magmatic-hydrothermal ore deposits,Economic Geology,2005.
[21]  Wilson A J,Cooke D R,Harper B J,Deyell C L,Sulfur isotopic zonation in the Cadia district,southeastern Australia:exploration significance and implications for the genesis of alkalic porphyry gold copper deposits,Mineralium Deposita,2007.
[22]  Yigit O,Gold in Turkey-a missing link in Tethyan metallogeny,Ore Geology Reviews,2006(2).
[23]  Yilmaz H,Exploration at the Kuscayiri Au(Cu) prospect and its implications for porphyry-relates mineralization in western Turkey,Journal of Geochemical Exploration,2003(2-3).
[24]  侯增谦.潘小菲.杨志明.曲晓明 初论大陆环境斑岩铜矿 [J].-现代地质2007(2)
[25]  孙凤兴,吴国学,杨鹏,团结沟金矿床地质模型,吉林地质,1996(2).
[26]  王奖臻.李朝阳.胡瑞忠 斑岩铜矿研究的若干进展 [J].-地球科学进展2001(4)
[27]  王奖臻.胡瑞忠.孙燕.陆彦.李泽琴 西范坪斑岩铜矿钾硅酸盐化作用的地球化学研究 [J].-矿物岩石2002(1)
[28]  徐兴旺.蔡新平.宋保昌.张宝林.应汉龙.肖骑彬.王杰 滇西北衙金矿区碱性斑岩岩石学、年代学和地球化学特征及其成因机制 [J].-岩石学报2006(3)
[29]  杨志明,西藏驱龙超大型斑岩铜矿床--岩浆作用及矿床成因,北京:中国地质科学院,2008.
[30]  曾普胜.侯增谦.高永峰.杜安道 印度-亚洲碰撞带东段喜马拉雅期铜-钼-金矿床Re-Os年龄及成矿作用 [J].-地质论评2006(1)
[31]  朱永峰 俯冲带中H2O和K的深循环:对碰撞后富钾岩浆成因研究的启示 [J].-地学前缘2003(3)
[32]  朱永峰.何国琦.安芳 中亚成矿域核心地区地质演化与成矿规律 [J].-地质通报2007(9)
[33]  Baldwin J T,Swain H D,Clark G H,Geology and grade distribution of the Panguna Porphyry copper deposit,Bougainville,Papua New Guinea,Economic Geology,1978.
[34]  Campbell I H,Naldrett A J,The influence of silicate:sulfide ratios on the geochemistry of magmatic sulfides,Economic Geology and the Bulletin of the Society of Economic Geologists,1979.
[35]  Candela P A,A review of shallow,ore-related granites:textures,volatiles and ore metals,Journal of Petrolgoy,1997.
[36]  Candela P A,Controls on ore metal ratios in granite-related ore systems:an experimental and computational approach,Transactions of the Royal Society of Edinburgh:Earth Sciences,1992.
[37]  Candela P A,Holland H D,The partitioning of copper and molybdenum between melts and aqueous fluids,Geochimica et Cosmochimica Acta,1984.
[38]  Cannell J,Cooke D R,Walshe J L,Stein Holly,Geology,mineralization,alteration,and structural evolution of the El Teniente porphyry Cu-Mo deposit,Economic Geology,2005.
[39]  Carroll M R,Rutherford M J,Sulfide and sulfate saturation in hydrous silicate melts,1985.
[40]  Chou I C,Phase relations in the system NaCl-KCl-H_2O:III,solubilities of halite in vapor-saturated liquids above 445 degrees C and redetermination of phase equilibrium properties in the system NaCl-H_2O to 1000 degrees C and 1500 bars,Geochimica et Cosmochimica Acta,1987.
[41]  Clark A H,Arancibia O N,Occurrence paragenesis and implications of magnetite-rich alteration-mineralization in calc-alkaline porphyry copper deposits,Kingston,QminEx Associates and Queen\'s University,1995.
[42]  Clark G H,Panguna copper-gold deposit,Australasian Institute of Mining and Metallurgy Monograph,1990.
[43]  Cline J,Bodnar R J,Can economic porphyry copper mineralization be generated by a typical calc-alkaline melt?,Journal of Geophysical Research,1991.
[44]  Cuddy A S,Kesler S E,Gold in the Granisle and Bell copper porphyry copper deposit,British Columbia,Rexdale,Ontario,Associatin of Exploration Geochemists,1982.
[45]  Esperance S,Grisci G M,de Rosa R,The role of the crust in the magmatic evolution of the island of Lipari (Aeolian Islands,Italy),Contributions to Mineralogy & Petrology,1992.
[46]  Frank M R,Candela P A,Piccoli P M,Glascock M D,Gold solubility,speciation,and partitioning as a function of HCl in the brine-silicate melt-metallic gold system at 800℃ and 100 MPa,Geochimica et Cosmochimica Acta,2002.
[47]  Fournier R O,Conceptual models of brine evolution in magmatic-hydrothermal systems,US Geological Survey Professional Paper,1987.
[48]  Gammons C H,Williams-Jones A E,Chemical mobility of gold in the porphyry-epithermal environment,Economic Geology,1997.
[49]  Garrett S,The geology and mineralisation of the dinkidi porphyry related Au-Cu deposit in porphyry related copper and gold deposits of the Asia Pacific region,AMF,Adelaide,1996.
[50]  Gill I,Orogenic Undesites and Plate Tectonics,Springer-verlag,1982.
[51]  Guilbert J M,Geology,alteration,mineralization,and genesis of the Bajo de la Alumbrera porphyry copper-gold deposit,Catamarca province,Argentina,Arizona Geological Society Digest,1995.
[52]  Gursoy H,Tatar O,Piper J D A,Heimann A,Kocbulut F,Mesci B L,Palaeomagnetic study of Tertiary volcanic domains in Southern Turkey and Neogene anticlockwise rotation of the Arabian Plate,Tectonophysics,2008.
[53]  常成.孙景贵 斑岩型多金属矿床成矿规律及成矿条件研究--以吉林省东部小西南岔金铜矿床为例 [J].-长春工程学院学报(自然科学版)2007(3)
[54]  迟效国.董春艳.马瑞 富钾贫钙岩浆的成因探讨--来自岩石失水熔融实验分析[J].矿物岩石地球化学通报2007(z1)
[55]  邓晋福.苏尚国.赵国春.刘翠 华北燕山造山带结构要素组合 [J].-高校地质学报2004(3)
[56]  杜琦,多宝山斑岩铜矿床,北京:地质出版社,1988.
[57]  葛良胜.郭晓东.邹依林.杨嘉禾.李玉静 云南姚安与富碱岩浆活动有关的金矿床地质及成因 [J].-地质与资源2002(1)
[58]  葛良胜.郭晓东.邹依林.李振华.张晓辉 云南北衙金矿床地质特征及成因研究 [J].-地质找矿论丛2002(1)
[59]  葛良胜,卿敏,袁士松,唐明国,邢俊兵,内蒙古毕力赫大型金矿勘查突破过程及启示意义,矿床地质,2009(4).
[60]  郭春影,高帮飞,刘学飞,张瑞忠,云南金平长安金矿床稀土元素特征及其地质意义,黄金地质,2009(1).
[61]  侯增谦 斑岩Cu-Mo-Au矿床:新认识与新进展 [J].-地学前缘2004(1)
[62]  侯增谦.钟大赉.邓万明 青藏高原东缘斑岩铜钼金成矿带的构造模式 [J].-中国地质2004(1)
[63]  侯增谦.潘桂棠.王安建.莫宣学.田世洪.孙晓明.丁林.王二七.高永丰.谢玉玲.曾普胜.秦克章.许继峰.曲晓明.杨志明.杨竹森.费红彩.孟祥金.李振清 青藏高原碰撞造山带:Ⅱ.晚碰撞转换成矿作用 [J].-矿床地质2006(5)
[64]  侯增谦.王二七 印度-亚洲大陆碰撞成矿作用主要研究进展 [J].-地球学报2008(3)
[65]  侯增谦,王二七,莫宣学,青藏高原碰撞造山与成矿作用,北京:地质出版社,2008.
[66]  侯增谦,杨志明,中国大陆环境斑岩型矿床:基本地质特征、岩浆-热液系统与成矿概念模型,地质学报,2009(12).
[67]  李成范,刘新三,团结沟斑岩金矿的成矿作用,北京:冶金工业出版社,1992.
[68]  李光明.李金祥.秦克章.张天平.肖波 西藏班公湖带多不杂超大型富金斑岩铜矿的高温高盐高氧化成矿流体:流体包裹体证据 [J].-岩石学报2007(5)
[69]  李金祥.秦克章.李光明 富金斑岩型铜矿床的基本特征、成矿物质来源与成矿高氧化岩浆-流体演化 [J].-岩石学报2006(3)
[70]  李颖.兰翔.刘连登 斑岩型金矿分类探讨 [J].-地质与勘探1999(6)
[71]  莫宣学,路风香,沈上越,三江特提斯火山作用与成矿,北京:地质出版社,1993.
[72]  聂风军.张洪涛.孙浩 内蒙古哈达庙金矿床地质特征及矿床成因探讨 [J].-矿床地质1989
[73]  聂风军,张洪涛,孙浩,樊建廷,内蒙古哈达庙含金隐爆角砾岩带地质特征及成因探讨,中国地质科学院院报,1991.
[74]  曲晓明.侯增谦.黄卫 冈底斯斑岩铜矿(化)带:西藏第二条“玉龙”铜矿带? [J].-矿床地质2001(4)
[75]  曲晓明.辛洪波 藏西班公湖斑岩铜矿带的形成时代与成矿构造环境 [J].-地质通报2006(7)
[76]  芮宗瑶,张洪涛,王龙生,吉林延边地区斑岩型-浅成低温型金铜矿床,矿床地质,1995(2).
[77]  芮宗瑶.张立生.陈振宇.王龙生.刘玉琳.王义天 斑岩铜矿的源岩或源区探讨 [J].-岩石学报2004(2)
[78]  Arif J,Baker T,Gold paragenesis and chemistry at Batu Hijau,Indonesia:implications for gold-rich porphyry copper deposits,Mineralium Deposita,2004.
[79]  Audétat A,Pettke T,Heinrich C A,Bodnar R J,The composition of magmatic-hydrothermal fluids in barren and mineralized intrusions,Economic Geology,2008.
[80]  Babcock R C,Ballantyne G H,Phillips C H,Summary of the geology of the Bingham District,Utah,Arizona Geological Society Digest,1995.
[81]  Bodnar R J,Burnham C W,Sterner S M,Synthetic fluid inclusions in natural quartz;III,determination of phase equilibrium properties in the system H_2O-NaCl to 1000 degrees C and 1500 bars,Geochimica et Cosmochimica Acta,1985(9).
[82]  Burnham C W,Magmas and hydrothermal fluids,New York:wiley,1979.
[83]  Caira N M,Findlay A,Delong C,Rebagliad C M,Fish Lake porphyry copper-gold deposite,central British Columbia,Canadian Institute of Mining Metallurgy and Petroleum Sepcial,1995.
[84]  Cooke D R,Hollings P,Walshe J L,Giant porphyry deposits:characteristics,distribution,and tectonic controls,Economic Geology,2005.
[85]  Corbett G J,Leach T M,Southwest Pacific Rim gold-copper systems.Structure,alteration and mineralization,Society of Economic Geologists Special Publication,1998.
[86]  Cox D P,Singer D A,Distribution of gold in porphyry copper deposits,1988.
[87]  Cunningham C G,Austin G W,Naeser C W,Formation of a paleothermal anomaly and disseminated gold deposits associated with the Bingham canyon porphyry Cu-Au-Mo system,Utah,Economic Geology,2004.
[88]  de Hoog J C M,Mason P R D,van Bergen M J,Sulfur and chalcophile elements in subduction zones:constraints from a laser ablation ICP-MS study of melt inclusions from Galunggung volcano,Indonesia,Geochimica et Cosmochimica Acta,2001.
[89]  Edwards C M H,Menzies M A,Thirlwall M F,Evidence from Murian,Indonesia,for the interplay of supra-subduction zone and intraplarte processes in the genesis of potassic alkaline magmas,Journal of Petrology,1991.
[90]  Emmons W H,Relations of disseminated copper ores in porphyry to igneous intrusions,Am Inst Mining Metall Eng Trans,1927.
[91]  Hayashi K,Ohmoto H,Solubility of gold in NaCl and H_ 2S bearing aqueous solutions at 250~350℃,Geochimica et Cosmochimica Acta,1991.
[92]  Hedenquist J W,Lowenstern J B,The role of magmas in the formation of hydrothermal of deposits,Nature,1994.
[93]  Hedenquist J W,ArribasA J R,Reynolds T J,Evolution of an intrusion-centere hdydrothermal system:far Southeast-Lepanto porphyry and epithermal Cu-Au deposits,Philippines,Economic Geology,1997.
[94]  Hedenquist J W,Arriba A J,Reynolds T J,Evolution of an intrusion-centered hydrothermal system:Far Southeast-Lepanto porphtyry and epithermal Cu-Au deposits,Philippines,Economic Geology,1998.
[95]  Heinrich C A,The physical and chemical evolution of low-salinity magmatic fluids at the porphyry to epithermal transition:a thermodynamic study,Mineralium Deposita,2005.
[96]  Heinrich C A,Ryan C G,Mernagh T P,Eadington P J,Segregation of ore metals between magmatic brine and vapor,Economic Geology,1992.
[97]  Heinrich C A,Gunther D,Audetat A,Ulrich T Frischknecht R,Metal fractionation between magmatic brine and vapor,determined by microanalysis of fluid inclusions,Geology,1999.
[98]  Henley R W,McNabb A,Magmatic vapor plumes and ground-water interatction in porphyry copper emplacement,Economic Geology,1978.
[99]  Hildreth W,Moorbath S,Crustal contributions to arc magmatism in the Andes of central Chile,Contributions to Mineralogy & Petrology,1988.
[100]  Holiday J R,Wilson A J,Blevin P L,Tedder I J Dunham P D Pfitzner M,Porphyry gold copper mineralisation in the Cadia district,eastern Lachlan Fold Belt,New South Wales,and its relationship to shoshonitic magmatism,Mineralium Deposita,2002.
[101]  Holland H D,Granites,solutions,and base metal deposits,Economic Geology,1972.
[102]  Hou Z Q,Gao Y F,Qu X M,Origin of adakitic intrusives generated during mid-Miocene east-west extension southern Tibet,Earth and Planetary Science Letters,2003.
[103]  Hou Z Q,Cook N,Metallogenesis of the Tibetan Collisional orogen.areview and introduction to the special issue,Ore Geology Reviews,2009.
[104]  Ishihara S,The granitoid series and mineralization,Economic Geology,1981.
[105]  Jones B K,Application of metal zoning to gold exploration in porphyry copper systems,Journal of Geochemical Exploration,1992(2).
[106]  Jugo P J,Candela P A,Piccoli P M,Linearly independent conditions of chemical equilibrium for the partitioning of ore metals in melt-crystal-volatile phase systems:applications to mineral exploration,Salvador,Brazil.Lithos,1999.
[107]  Jugo P J,Luth R W,Richards J P,Experimental determination of sulfur solubility in basaltic melts at sulfide vs.sulfate saturation:possible implications for ore formation,EOS(Transactions of the American Geophysical Union),2001.
[108]  Jugo P J,Luth R W,Richards J P,Generation of sulfur-rich,sulfur-undersaturated basaltic melts in oxidized arc sources,2003.
[109]  Kamenetsky V S,Wolfe R C,Eggins S M,Mernagh T P Bastrakov E,Volatile exsolution at the Dinkidi Cu-Au porphyry deposit,Philippines:a melt-inclusion record of the initial ore-forming process,Geology,1999.
[110]  Kay S M,Mpodozis C,Central Andean ore deposits linked to evolved shallow subduction systems and thickening crust,GSA Today,2001.
[111]  Kay S M,Mpodozis C,Coira B,Neogene magmatism,tectonism,and mineral deposits of the Central Andes(22 to 33 S Latitude),Society of Economic Geologists Special Publication,1999.
[112]  Kay S M,Mpodozis C,Magmatism as a probe to the Neogene shallowing of the Nazca plate beneath the modern Chilean flat-slab,Journal of South American Earth Sciences,2002.
[113]  Kay S M,Mpodozis C,Tittler A,Cornejo P,Tertiary magmatic evolution of the Maricunga mineral belt in Chile,International Geology Review,1994.
[114]  Kerrich R,Goldfarb R,Groves D,Garwin S,The geodynamics of world-class gold deposits:characteristics,space-time distributions,and origins,Reviews in Economic Geology,2000.
[115]  Kesler S E,Chryssoulis S L,Simon G,Gold in porphyry copper deposits:its abundance and fate,Ore Geology Reviews,2002.
[116]  Khashgerel B E,Rye R O,Hedenquist J W,Kavalieris I,Geology and reconnaissance stable isotope study of the Oyu Tolgoi porphyry Cu-Au system,South Gobi,Mongolia,Economic Geology,2006.
[117]  Kirkham R V,Sinclair W D,Porphyry copper,gold,molybdenum,tungsten,tin,silver,Geological Survey of Canada Geology of Canada,1995.
[118]  Kosaka H,Wakita K,Some geologic features of the Mamut porphyry copper deposit,Sabah,Malaysia,Economic Geology,1978.
[119]  Lang J R,Stanley C R,Thompson J F H,Dunne K P E,Na-K-Ca magmatic hydrothermal alteration in alkalic porphyry Cu-Au deposits,British Columbia,Mineral Assoc Can Short Course Ser,1995.
[120]  Lickfold V,Cooke D R,Smith S G,Ullrich T D,Endeavour copper-gold porphyry deposits,Northparkes,New South Wales:intrusive history and fluid evolution,Economic Geology,2003.
[121]  Liegeois J P,Navez J,Hertogen J,Contrasting origin of post-collisional high-K calc-alkaline and shoshonitic versus alkaline and pevalkaline granitoids.The use of sliding normalization,Lithos,1998.
[122]  Loucks R R,Mavvogenes J A,Gold solubility in supercritical hydrothermal brines measured in synthetic fluid inclusions,Science,1999.
[123]  Lowell J D,Guilbert J M,Lateral and vertical alteration-mineralization zoning in porphyry ore deposits,Economic Geology,1970.
[124]  Lowenstern J B,Mahood G A,Rivers M I,Sutton S R,Evidence for extreme partitioning of copper into a magmatic vapor phase,Science,1991.
[125]  MacDoanld G D,Arnold L C,Geological and geochemical zoning of the Grasberg Igneous Complex,Irian Jaya,Indonesia,Journal of Geochemical Exploration,1994.
[126]  Massonne H J,Evidence for low temperature ultrapotassic siliceous fluids in subduction zone environments from experiments in the system K_2O-MgO-Al_2O_3-SiO_2-H_2O(KMASH),Lithos,1991.
[127]  McInnes B,Cameron E M,Carbonated,alkaline hybridizing melts from a sub-arc environment:mantle wedge samples from the Tabar-Lihir-Tanga-Feni arc,Papua New Guinea,Earth and Planetary Science Letters,1994.
[128]  McKee E H,Robinson A C,Rytuba J J,Cuitino L Moscoso R D,Age and Sr isotopic composition of volcanic rocks in the Maricunga Belt,Chile:implications for magma sources,Journal of South American Earth Sciences,1994.
[129]  Meldrum S J,Aquino R S,Gonzales R I,Burke R J Suyadi A Irianto B ClarkeD S,The Batu Hijau porphyry copper-gold deposit,Sumbawa Island,Indonesia,Journal of Geochemical Exploration,1994.
[130]  Nagaseki H,Hayashi K,Experimental study of the behavior of copper and zinc in a boiling hydrothermal system,Geology,2008.
[131]  O′brien H,Irving A J,Mccallum I S,Strontium,neodymium,and lead isotopic evidence for the interaction of post-2subduction asthenospheric potassic mafic magmas of the Highwood Mountains,Montana,USA,with ancient Wyoming craton lithospheric mantle,Geochimica et Cosmochimica Acta,1995.
[132]  Padilla Grrza R A,Titley S R,Francisco Pimentel B,Geology of the Escondida Porphyry copper deposit,Antofagasta Region,Chile Economic Geology,2001(2).
[133]  Palacios C,Herail G,Townley B,The composition of gold in the cerro casale gold-rich porphyry deposit,Maricunga belt,Northern Chile,The Canadian Mineralogist,2001.
[134]  Parry W T,Jasumback J,Wilson P N,Clay mineralogy of phyllic and intermediate argillic alteration at Bingham,Utah,Economic Geology,2002.
[135]  Peach C L,Mathez E A,Keays R R,Sulfi de melt silicate melt distribution coefficients for noble metals and other chalcophile elements as deduced from MORB:implications for partial melting,Geochimica et Cosmochimica Acta,1990.
[136]  Perello J,Cox D,Garamjav D,Oyu Tolgoi,Mongolia:Siluro-Devonian porphyry Cu-Au-(Mo) and high-sulfidation Cu Mineralization with a Cretaceous Chalcocite Blanket,Economic Geology,2001.
[137]  Perello J,Razione A,Schloderer J,Asad-UR-Rehman,The Chagai porphyry copper belt,Baluchistan Province,Pakistan,Economic Geology,2008.
[138]  Petford N,Atherton M P,Cretaccous-Tertiary volcanism and syn-subduction crutal extension in northern central Peru,Geological Society(London) Special Publication,1994.
[139]  Pokrovski G,Roux J,Harrichoury J-C,Fluid density control on vapour-liquid partitioning of metals in hydrothermal systems,Geology,2005.
[140]  Pollard J P,Roger G T,Peters L,Ages of intrusion,alteration,and mineralization at the Grasberg Cu-Au deposit,Papua,Indonesia,Economic Geology,2005.
[141]  Proffett J M,Geology of the Bajo de la Alumbrera porphyry copper-gold deposit,Argentina,Economic Geology,2003.
[142]  Richards J P,Petrology and geochemistry of alkalic intrusives at the Porgera gold deposit,Papua New Guinea,1990.
[143]  Richards J P,Tectono-magmatic precursors for porphyry Cu-(Mo-Au) deposit formation,Economic Geology,2003.
[144]  Richards J P,Cumulative factors in the generation of giant calc-alkaline porphyry Cu deposits,PGC Publishing,Adelaide,2005.
[145]  Richards J P,Postsubduction porphyry Cu-Au and epithermal Au deposits:products of remelting of subduction-modified lithosphere,Geology,2009.
[146]  Richards J P,McCulloch M T,Chappell B W,Kerrich R,Sources of metals in the Porgera gold deposit,Papua New Guinea:evidence from alteration,isotope,and noble metal geochemistry,Geochimica et Cosmochimica Acta,1991.
[147]  Roedder E,Fluid inclusions,Reviews in Mineralogy,1984.
[148]  Roedder E,Fluid inclusion evidence for immisciblility in magmatic differentiation,Geochimica et Cosmochimica Acta,1992(1).
[149]  Rush S M,Seegera H J,Ok Tedi copper-gold deposits,Australasian Institute of Mining and Metallurgy Monograph,1990.
[150]  Sengor A M C,Ozeren M S,Keskin M,Sakinc M Ozbakir A D Kayan I,Eastern Turkish high plateau as a small Terkic-type orogen:implication for post-collisional crust-forming processes in Turkic-type orogens,Earth-Science Reviews,2008.
[151]  Serafica V S,Baluda R P,Geology of the Philex Sto.TomasII ore body:symposium on mineral resources development,Baguio City,Philippines,1977.
[152]  Seward T M,The hydrothermal geochemistry of gold,Glasgow,Blackie,1991.
[153]  Shinohara H,Exsolution of immiscible vapor and liquid phases from a crystallizing silicate melt; implications for chlorine and metal transport,Geochimica et Cosmochimica Acta,1994(23).
[154]  Shinohara H,Kazahaya K,Lowenstern J B,Volatile transport in a convecting magma column:implication for porphyry Mo mineralization,Geology,1995.
[155]  Shinohara H,Hedenquist J W,Constraints on magma degassing beneath the Far Southeast porphyry Cu-Au deposit,Philippines,Journal of Petrology,1997.
[156]  Sillitoe R H,Some thoughts on gold-rich porphyry copper deposits,Mineralium Deposita,1979.
[157]  Sillitoe R H,Characteristics and controls of the largest porphyry copper-gold and epithermal gold deposits in the circum-Pacific region,Australian Journal of Earth Sciences,1997.
[158]  Sillitoe R H,Gold-rich porphyry deposits:descriptive and genetic models and their role in exploration and discovery,Reviews in Economic Geology,2000.
[159]  Sillitoe R H,Some metallogenic features of gold and copper deposits related to alkaline rocks and consequences for exploration,Mineralium Deposita,2002.
[160]  Solomon M,Subduction,arc reversal and the origin of porphyry copper-gold deposits in island arcs,Geology,1990.
[161]  Sourirajan S,Kennedy G C,The system NaCl-H_2O at elevated temperatures and pressures,American Journal of Science,1962.
[162]  Sun Weidong,Richard J Arculus,Vadim S Kamenetsky,Raymond A Binns,Release of gold-bearing fluids in convergent margin magmas prompted by magnetite crystallization,Nature(London),2004(7011).
[163]  Tapponnier P,Xu Z Q,Roger F,Meyer B Arnaud N Wittlinger G Yang J S,Oblique stepwise rise and growth of the Tibet plateau,Science,2001.
[164]  Tarkian M,Koopmann G,Platinum-group minerals in the Santo Tomas II(Phylex) porphyry copper gold deposit,Luzon Island,Philippines,Mineralium Deposita,1995.
[165]  Thompson J F H,Exploration and research related to porphyry deposits,Canadian Institute of Mining,Metallurgy and Petroleum Special,1995.
[166]  Thompson J F H,Lang J R,Mortensen J K,Cassidy K F,Cu-Au metallogeny of alkalic arc magmatism:examples from the Mesozoic arc terranes of the northern Canadian Cordillera and comparison to the Tabar-Feni arc,PNG,Queen\'s University,Kingston,Ontario,1995.
[167]  Thorpe R S,Francis P W,O′Callaghan L,Relative roles of source composition,fractional crystallization and crustal contamination in the petrogenesis of Andean volcanic rock,Philosophical Transactions of the Royal Society of London,1984.
[168]  Tobey E,Schneider A,Alegria A,Olcay L,Perantonis G,Quiroga J,Glenside,South Australia,Australian Mineral Foundation,1998.
[169]  Yilmaz H,Geochemical exploration for gold in western Turkey:success and failure,Journal of Geochemical Exploration,2003.
[170]  Cooke D R,斑岩型矿床分类、分布和动力学背景,云南省地质调查局,2008.

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