全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
地质学报  2009 

中国大陆环境斑岩型矿床:基本地质特征、岩浆热液系统和成矿概念模型

, PP. 1779-1817

Keywords: 斑岩矿床,含矿斑岩,岩浆起源,动力学机制,成矿模型,大陆环境

Full-Text   Cite this paper   Add to My Lib

Abstract:

中国大陆环境斑岩型矿床包括斑岩型Cu(Mo、Au)、斑岩型Mo、斑岩型Au和斑岩型PbZn等矿床类型,主要产出于青藏高原大陆碰撞带、东秦岭大陆碰撞带和中国东中部燕山期陆内环境,在地球动力学背景、深部作用过程、岩浆起源演化、流体与金属来源等方面与岩浆弧环境斑岩型矿床存在重要差异。在大洋板块俯冲形成的岩浆弧,主要发育斑岩CuAu矿床或富金斑岩Cu矿(岛弧)和斑岩CuMo及斑岩Mo矿床(陆缘弧)。相比,在大陆碰撞带,晚碰撞构造转换环境发育斑岩Cu、CuMo和CuAu矿床,矿床受斜交碰撞带的走滑断裂系统控制,后碰撞地壳伸展环境则主要发育斑岩CuMo矿床,矿床受垂直于碰撞带的正断层系统控制;在陆内造山环境,早期发育斑岩CuAu矿床,晚期发育斑岩PbZn矿床,它们主要沿古老的但再活化的岩石圈不连续带分布,受网格状断裂系统控制;在后造山(或非造山)伸展环境,则大量发育斑岩Mo矿和斑岩Au矿,它们则主要围绕大陆基底―克拉通(或地块)边缘分布,受再活化的岩石圈不连续带控制。大陆环境斑岩Cu(Mo,Au)矿床的含矿斑岩多为高钾钙碱性和钾玄质,以高钾为特征,显示埃达克岩地球化学特性。岩浆通常起源于加厚的新生镁铁质下地壳或拆沉的古老下地壳。上地幔通过三种可能的方式向岩浆系统供给金属Cu(和Au):①提供大批量的幔源岩浆并底垫于加厚下地壳底部,构成含Cu岩浆的源岩;②提供小批量的软流圈熔体交代和改造下地壳,并诱发其熔融;③与拆沉的下地壳岩浆熔体发生反应。大陆环境含Mo岩浆系统高SiO??2?、高K??2?O,岩相以花岗斑岩为主,花岗闪长斑岩次之,既不同于Climax型,又有别于石英二长斑岩型Mo矿床,岩浆起源于古老的下地壳。金属Mo主要为就地熔出,部分萃取于上部地壳。大陆环境含PbZn花岗斑岩多属铝过饱和型,与S型花岗岩相当,以高δ??18?O(>10‰)和高放射性Pb为特征,SrNdPb同位素组成反映其来源于中下地壳的深熔作用,金属PbZn主要来源于深融的壳层。大陆环境含Au岩浆系统以富B花岗闪长斑岩为主,常与矿前闪长岩密切共生。SrNdPb同位素显示,含Au岩浆主要来源于上部地壳,但曾与幔源岩浆发生相互作用。金属Au部分来源于上地壳,部分来源于地幔岩浆。大陆环境斑岩型矿床显示各具特色的蚀变类型和蚀变分带,其中,斑岩型Cu(Mo,Au)矿热液蚀变遵循LowellandGuilbert模式;斑岩型Mo矿主要发育钙硅酸盐化、钾硅酸盐化和石英绢云母化;斑岩型PbZn矿主要发育绿泥石绢云母化和绢云母碳酸盐化,缺乏钾硅酸盐化;斑岩型Au矿强烈发育中度泥化。斑岩型矿床的成矿流体初始为高温、高?f?O??2?、高S、富金属的岩浆水,由浅成侵位的长英质岩浆房在应力松弛环境下出溶而来,晚期有天水不同程度地混入。Cu、Mo、PbZn通常沉淀于流体分相和流体沸腾过程中,而Au则主要沉淀于岩浆热液过渡阶段。

References

[1]  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)
[2]  邓晋福.赵国春.赵海玲.罗照华.戴圣潜.李凯明 中国东部燕山期火成岩构造组合与造山-深部过程 [J].-地质论评2000(1)
[3]  邓晋福.吴宗絮.赵国春.赵海玲.罗照华.莫宣学 华北地台前寒武花岗岩类、陆壳演化与克拉通形成 [J].-岩石学报1999(2)
[4]  邓万明,黄萱,钟大赉,滇西新生代富碱斑岩的岩石特征与成因,地质科学,1998(2).
[5]  丁道桂.刘光祥.吕俊祥.潘文蕾 扬子板块海相中古生界盆地的递进变形改造 [J].-地质通报2007(9)
[6]  高晓峰.郭锋.范蔚茗.李超文.李晓勇 南兴安岭晚中生代中酸性火山岩的岩石成因 [J].-岩石学报2005(3)
[7]  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).
[8]  郭晓东,云南马厂箐斑岩型铜钼(金)矿床地质特征与矿床成因,地质学报,2009(12).
[9]  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)
[10]  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)
[11]  李永峰.毛景文.白凤军.李俊平.和志军 东秦岭南泥湖钼(钨)矿田 Re-Os同位素年龄及其地质意义 [J].-地质论评2003(6)
[12]  李永峰.毛景文.胡华斌.郭保健.白凤军 东秦岭钼矿类型、特征、成矿时代及其地球动力学背景 [J].-矿床地质2005(3)
[13]  李兆鼐,权恒,李之彤,中国东部中新生代火成岩及其深部过程,北京:地质出版社,2003.
[14]  卢欣祥.于在平.冯有利.王义天.马维峰.崔海峰 东秦岭深源浅成型花岗岩的成矿作用及地质构造背景 [J].-矿床地质2002(2)
[15]  罗建安 城门山铜矿床表生变化及次生富集作用的研究 [J].-江西有色金属2003(4)
[16]  罗铭玖,林潜龙,卢欣祥,陈铁华,东秦岭含相花岗岩的地质特征,河南地质,1993(11).
[17]  马鸿文,论藏东玉东铜矿带花岗斑岩类的成因类别,成都理工大学学报(自然科学版),1990.
[18]  毛景文.王志良 中国东部大规模成矿时限及其动力学背景的初步探讨 [J].-矿床地质2000(4)
[19]  毛景文.张作衡.余金杰.王义天.牛宝贵 华北及邻区中生代大规模成矿的地球动力学背景: 从金属矿床年龄精测得到启示 [J].-中国科学D辑2003(4)
[20]  孟庆任,胡健民,胡健民,袁选俊,靳久强.中蒙边界地区晚中生代伸展盆地的结构、演化和成因,地质通报,2002.
[21]  聂凤军,张洪涛,内蒙古哈达庙含金侵入杂岩体稀土元素地球化学研究,地质找矿论丛,1989.
[22]  潘小菲,宋玉财,李振清,杨志明,侯增谦,德兴铜厂斑岩型铜金矿床热液演化过程,地质学报,2009(12).
[23]  齐进英 江西冷水坑斑岩类型及其矿化特征 [J].-岩石学报1987(1)
[24]  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)
[25]  任启江.吴俞斌.武耀成.周会群.徐兆文 陕西金堆城斑岩钼矿含矿裂隙分布规律与成因 [J].-矿床地质1987(3)
[26]  芮宗瑶,黄崇轲,齐国明,中国斑岩铜(钼)矿床,北京:地质出版社,1984.
[27]  芮宗瑶.李光明.张立生.王龙生 西藏斑岩铜矿对重大地质事件的响应 [J].-地学前缘2004(1)
[28]  孙晓明,刘孝善,东秦岭钼矿带中皱纹岩的成因及找矿意义,陕西地质,1993(11).
[29]  唐仁鲤,罗怀松,李荫清,西藏玉龙斑岩铜(钼)矿带地质,北京:地质出版社,1995.
[30]  王建.李建平.王江海 滇西大理-剑川地区钾玄质岩浆作用:后碰撞走滑拉伸环境岛弧型岩浆作用的地球化学研究[J].岩石学报2003(1)
[31]  王立本,季克俭,陈东,安基山和铜山铜 (钼) 矿床中辉钼矿的铼-锇同位素年龄及其意义,岩石矿物学杂志,1997(2).
[32]  王强.赵振华.熊小林.许继锋 底侵玄武质下地壳的熔融:来自安徽沙溪adakite质富钠石英闪长玢岩的证据 [J].-地球化学2001(4)
[33]  王强.赵振华.许继峰.白正华.王建新.刘成新 鄂东南铜山口、殷祖埃达克质(adakitic)侵入岩的地球化学特征对比:(拆沉)下地壳熔融与斑岩铜矿的成因 [J].-岩石学报2004(2)
[34]  王强.许继峰.赵振华.资锋.唐功建.贾小辉.姜子琦 中国埃达克岩或埃达克质岩及相关金属成矿作用 [J].-矿物岩石地球化学通报2007(4)
[35]  王强.赵振华.简平.许继峰.包志伟.马金龙 德兴花岗闪长斑岩SHRIMP锆石Upb年代学和Nd-Sr同位素地球化学 [J].-岩石学报2004(2)
[36]  吴福元.葛文春.孙德有.郭春丽 中国东部岩石圈减薄研究中的几个问题 [J].-地学前缘2003(3)
[37]  肖波,秦克章,李光明,李金祥,夏代祥,陈雷,赵俊兴,西藏驱龙巨型斑岩Cu-Mo矿床的富S、高氧化性含矿岩浆--来自岩浆成因硬石膏的证据,地质学报,2009(12).
[38]  谢桂青.毛景文.李瑞玲.张祖送.赵维超.屈文俊.赵财胜.魏世昆 鄂东南地区Cu-Au-Mo-(W)矿床的成矿时代及其成矿地球动力学背景探讨:辉钼矿Re-Os同位素年龄 [J].-矿床地质2006(1)
[39]  谢?,徐夕生,邹海波,蒋少涌,张明,邱检生,中国东南部晚中生代大规模岩浆作用序幕:J_2 早期玄武岩,中国科学d辑,2005.
[40]  谢玉玲,李应羽,David Cooke,白劲松,刘云飞,李光明,张丽,西藏恰功铁矿岩浆演化序列及斑岩出溶流体特征,地质学报,2009(12).
[41]  许继峰.王强.徐义刚.赵振华.熊小林 宁镇地区中生代安基山中酸性侵入岩的地球化学:亏损重稀土和钇的岩浆产生的限制 [J].-岩石学报2001(4)
[42]  杨明桂.王发宁.曾勇 赣东北地区的成矿环境与成矿作用 [J].-资源调查与环境2002(2)
[43]  杨志明,侯增谦,杨竹森,王淑贤,王贵仁,田世洪,温德银,王召林,刘英超,青海纳日贡玛斑岩铜(钼)矿床:岩石成因及构造控制,岩石学报,2008.
[44]  张正伟.朱炳泉.常向阳.强立志.温明星 东秦岭钼矿带成岩成矿背景及时空统-性 [J].-高校地质学报2001(3)
[45]  祝向平,云南哈播斑岩型铜(-钼-金)地质与成矿背景研究,地质学报,2009(12).
[46]  Bornhorst T J,Rose W I,Partitioning of gold in young calc-alkaline volcanic rocks form Guatemala,Journal of Geology,1986.
[47]  Hedenquist J W,Richards J P,The influence of geochemical techniques on the development of genetic models for porphyry copper deposits,Reviews in Economic Geology,1998.
[48]  Hou Zengqian,Zhong Dalai,Deng Wanming,Khin Zaw,A tectonic model for porphyry copper-molybdenum-gold deposits in the eastern Indo-Asian collision zone,PGC Publishing,Adelaide,2005.
[49]  Hou Z Q,Gao Y F,Qu X M,Rui Z Y Mo X X,Origin of adakitic intrusives generated during mid-Miocene east-west extension in southern Tibet,Earth and Planetary Science Letters,2004.
[50]  Owen T J,Zandt G,Implications of crustal property variations for models of Tibetan plateau evolution,Nature,1997.
[51]  Pagnant U,Spencer D A,First record of eclogites from the Himalayan belt,Kaghan valley,Northern Pakistan,European Journal of Mineralogy,1991.
[52]  Proffett J M,Geology of the Bajo de la Alumbrera porphyry copper-gold deposit,Argentina,Economic Geology,2003.
[53]  Qu X M,Hou Z Q,Khin Zaw,Li Y G,Characteristics and genesis of Gangdese porphyry copper deposits in the southern Tibetan Plateau:Preliminary geochemical and geochronological results,Ore Geology Reviews,2007.
[54]  Rapp R P,Watson E B,Dehydration melting of metabasalts at 8-32 kbar:implications for continental growth and crust-mantle recycling,Journal of Petrology,1995.
[55]  Richards J P,Alkalic-type epithermal gold deposits-a review,Mineralogical Association of Canada Short Course Series,1995.
[56]  Skarmeta J,McClay K,Bertens A,Structural controls on porphyry copper deposits in northern Chile:New models and implications for Cu-Mo mineralization in subduction orogens \[abs.\]:D cimo Congreso Geologico Chileno,Concepci n,2003,2003.
[57]  Sourirajan S,Kennedy G C,The system H_2O-NaCl at elevated temperatures and pressures,American Journal of Science,1962.
[58]  Stein H J,Markey R J,Morgan J W,Du A Sun Y,Highly precise and accurate Re-Os ages for molybdenite from the East Qinling molybdenum belt,Shaanxi Province,China,Economic Geology,1997(7-8).
[59]  Tatsumi Y,Hamilton D L,Nesbitt R W,Chemical characteristics of fluid phase released from a subducted lithosphere and the origin of arc magmas:Evidence from high pressure experiments and natural rocks,Journal of Volcanology and Geothermal Research,1986.
[60]  Titley S R,Beane R E,Porphyry copper deposit:Part I.Geologic settings,petrology,and tectonogenesis,1981.
[61]  Ulrich T,G nther D,Heinrich C A,Gold concentrations of magmatic brines and the metal budget of porphyry copper deposits,Nature,1999.
[62]  Wang Q,Xu J F,Jian P,Bao Z W Zhao Z H Li C F Xiong X L Ma J L,Petrogenesis of adakitic porphyries in an extensional tectonic setting,Dexing,South China:Implications for the genesis of porphyry copper mineralization,Journal of Petrology,2006(1).
[63]  White W H,Bookstrom A A,Kamilli R J,Ganster M W,Smith R P,Ranta D E,Steininger R C,Character and origin of Climax-type molybdenum deposits,1981.
[64]  Whitney J A,Vapor Generation in a quartz monzonite magma,a synthetic model with application to porphyry ore deposits,Economic Geology,1975.
[65]  Ulrich T,Heinrich C A,Geology and alteration geochemistry of the porphyry Cu-Au deposit at Bajo de la Alumbrera,Argentina,Economic Geology,2001.
[66]  常印佛,刘湘培,吴言昌,长江中下游成矿带,北京:地质出版社,1991.
[67]  陈建平,唐菊兴,丛源,董庆吉,郝金华,藏东玉龙斑岩铜矿地质特征及成矿模型,地质学报,2009(12).
[68]  邓晋福,罗照华,苏尚国,莫宣学,于炳松,赖兴运,谌宏伟,岩石成因、构造环境与成矿作用,北京:地质出版社,2004.
[69]  邓晋福,莫宣学,罗照华,汪洋,赵海玲,赵志丹,苏尚国,喻学惠,青藏高原岩石圈不均-性及其动力学意义,中国科学d辑,2001.
[70]  侯增谦.莫宣学.杨志明.王安建.潘桂棠.曲晓明.聂凤军 青藏高原碰撞造山带成矿作用:构造背景、时空分布和主要类型 [J].-中国地质2006(2)
[71]  侯增谦.杨竹森.徐文艺.莫宣学.丁林.高永丰.董方浏.李光明.曲晓明.李光明.赵志丹.江思宏.孟祥金.李振清.秦克章.杨志明 青藏高原碰撞造山带:Ⅰ.主碰撞造山成矿作用 [J].-矿床地质2006(4)
[72]  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)
[73]  侯增谦.曲晓明.杨竹森.孟祥金.李振清.杨志明.郑绵平.郑有业.聂凤军.高永丰.江思宏.李光明 青藏高原碰撞造山带:Ⅲ. 后碰撞伸展成矿作用 [J].-矿床地质2006(6)
[74]  侯增谦.赵志丹.高永丰.杨志明.江万 印度大陆板片前缘撕裂与分段俯冲:来自冈底斯新生代火山-岩浆作用证据 [J].-岩石学报2006(4)
[75]  侯增谦.孟祥金.曲晓明.高永丰 西藏冈底斯斑岩铜矿带埃达克质斑岩含矿性:源岩相变及深部过程约束 [J].-矿床地质2005(2)
[76]  侯增谦.高永丰.孟祥金.曲晓明.黄卫 西藏冈底斯中新世斑岩铜矿带:埃达克质斑岩成因与构造控制 [J].-岩石学报2004(2)
[77]  侯增谦,曲晓明,王淑贤,高永丰,杜安道,黄卫,西藏冈底斯斑岩铜矿带辉钼矿Re-Os 年龄:成矿作用时限与动力学背景应用,中国科学A辑,2003.
[78]  侯增谦.莫宣学.高永丰.曲晓明.孟祥金 埃达克岩:斑岩铜矿的一种可能的重要含矿母岩――以西藏和智利斑岩铜矿为例 [J].-矿床地质2003(1)
[79]  侯增谦.曲晓明.黄卫.高永丰 冈底斯斑岩铜矿成矿带有望成为西藏第二条“玉龙”铜矿带 [J].-中国地质2001(10)
[80]  华仁民.李晓峰.陆建军.陈培荣.邱德同.王果 德兴大型铜金矿集区构造环境和成矿流体研究进展 [J].-地球科学进展2000(5)
[81]  Candela P A,Physics of aqueous phase evolution in plutionic environments,American Mineralogist,1991.
[82]  Candela P A,A review of shallow,ore-related granites:Textures,volatiles and ore metals,Journal of Petrolgoy,1997.
[83]  Candela P A,Controls on ore metal ratios in granite-related ore systems;an experimental and computational approach,Geological Society of America,1992.
[84]  Chappell B W,White A J R,Two contrasting granite types,Pacific Geology,1974.
[85]  Chen P R,Hua R M,Zhang B T,Lu J J Fan C F,Early Yanshanian post-orogenic granitoids in the Nanling region:petrological constraintand geodynamic settings,Science in China(Series D),2002.
[86]  Chung S L,Liu D,Ji J,Chu M F Lee H Y Wen D J Lo C H Lee T Y Qian Q Zhang Q,Adakites from continental collision zones:melting of thickened lower crust beneath southern Tibet,Geology,2003.
[87]  Cline J S,Genesis of porphyry copper deposits:the behavior of water,chloride,and copper in crystallizing melts,1995.
[88]  Cline J,Bodnar R J,Can economic porphyry copper mineralization be generated by a typical calc-alkaline melt,Journal of Geophysical Research,1991.
[89]  Cooke D R,Hollings P,Walshe J L,Giant Porphyry Deposits:Characteristics,distribution,and tectonic controls,Economic Geology,2005.
[90]  Corbett G J,Leach T M,Southwest Pacific Rim gold-copper systems:structure,alteration and mineralization,Society of Economic Geologists Special Publication,1998.
[91]  Davidson J P,Deciphering mantle and crustal signatures in subduction zone magmatism,Geophysical Monograph,1996.
[92]  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.
[93]  Defant M J,Drummond M S,Derivation of some modern arc magmas by melting of young subducted lithosphere,Nature,1990.
[94]  Dilles J H,Einaudi M T,Wall-rock alteration and hydrothermal flow paths about the Ann-Mason porphyry copper deposit,Nevada-a 6 km vertical reconstruction,Economic Geology,1992.
[95]  Ding Lin,Zhong Dalai,Yin An,Kapp p,Harrison T M,Cenozoic structure and metamorphic evolution of the eastern Himalayan syntaxis (Namche Barwa),Earth and Planetary Science Letters,2001.
[96]  Dobosi G,kempton P D,Downes H,Embey-Isztin A,Thirlwall M,Greenwood P,Lower crust granulite xenolites from the Pannonian basin,Hungary,Part 2:Sr,Nd,Pb,Hf and O isotope evidence for formation of continental lower crust by tectonic emplacement of oceanic crust,Contributions to Mineralogy & Petrology,2003.
[97]  Gao Y F,Hou Z Q,Wei R H,Post-collisional adakitic porphyries in Tibet:geochemical and Sr Nd Pb isotopic constraints on partial melting of oceaniclithosphere and crust mantle interaction,Acta Geologica Sinica,2003.
[98]  Ge L S,Qing M,Yuan S S,Tang M G Xing J B,Prospecting process of Bilihe large-sized gold deposit in Inner Mongolia and its revelatory significance,Mineral Deposits,2009(4).
[99]  Goodell P C,Gilder S A,Fang X H,A preliminary description of the Gan-Hang failed rift,southeastern China,Tectonophysics,1991.
[100]  Gow P,Walshe J L,The role of preexisting geologic architecture in the formation of giant porphyry-related Cu±Au deposits:Examples from New Guinea and Chile,Economic Geology,2005.
[101]  Guilbert J M,Geology,alteration,mineralization,and genesis of the Bajo de la Alumbrera porphyry copper-gold deposit,Catamarca Province,Argentina(in Porphyry copper deposits of the American Cordillera),Arizona Geological Society Digest,1995.
[102]  Gustafson L B,Hunt J P,The porphyry copper deposit at E_l Salvador,Chile,Economic Geology,1975.
[103]  Gutscher M A,Maury R,Eissen J P,Can slab melting be caused by flat subduction?,Geology,2000.
[104]  Hamlyn P R,Keays R R,Cameron W E,Crawford A J Waldron H M,Precious metals in magnesian low-Ti lavas:implications for metallogenesis and sulfur saturation in primary magmas,Geochimica et Cosmochimica Acta,1985.
[105]  Harris A C,Kamenetsky V S,White N C,Steele D A,Volatile phase separation in silicic magmas at Bajo de la Alumbrera porphyry Cu-Au deposit,NW Argentina,Resource Geology,2004.
[106]  He W,Zhengyu B,Tieping L,One-dimensional reactive transport models of alteration in the Tongchang porphyry copper deposit,Dexing District,Jiangxi Province,China,Economic Geology,1999(3).
[107]  Hedenquist J W,Lowenstern J B,The role of magmas in the formation of hydrothermal of deposits,Nature,1994.
[108]  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.
[109]  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.
[110]  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.
[111]  Henley R W,McNabb A,Magmatic vapor plumes and ground-water interaction in porphyry copper emplacement,Economic Geology,1978.
[112]  Hildreth W,Moorbath S,Crustal contributions to arc magmatism in the Andes of central Chile,Contributions to Mineralogy & Petrology,1988.
[113]  Hou Z Q,Cook N,Metallogenesis of the Tibetan Collisional Orogen:A review and introduction to the special issue,Ore Geology Reviews,2009.
[114]  Hou Z Q,Yang Z M,Qu X M,Meng X J Li Z Q Beaudoin G Rui Z Y Gao Y F,The Miocene Gangdese porphyry copper belt generated during post-collisional extension in the Tibetan orogen,Ore Geology Reviews,2009.
[115]  Sillitoe R H,Major regional factors favoring large size,high hypogene grade,elevated gold content and supergene oxidation and enrichment of porphyry copper deposits,in Porter,T.M,ed,Porphyry and hydrothermal copper and gold deposits:A Global Perspective,Perth,1998,South Australia,Australian Mineral Foundation,1998.
[116]  Sillitoe R H,Gold-rich porphyry deposits:descriptive and genetic models and their role in exploration and discovery,Reviews in Economic Geology,2000.
[117]  Sillitoe R H,Gappe I M,Philippine porphyry copper deposits; geologic setting and characteristics,Bangkok,Thailand,United Nations ESCAP,CCOP Technicat Publication,1984.
[118]  Singer D A,Berger V I,Menzie W D,Berger B R,Porphyry copper deposit density,Economic Geology,2005.
[119]  Williams-Jones A E,Migdisov A A,Archibald S M,Xiao Z F,Vapor-transport of ore metals,The Geochemical Society,Special Publication,2002.
[120]  Wu F Y,Zhang Y B,Yang J H,Xie L W,Yang Y H,Zircon U-Pb and Hf isotopic constraints on the Early Archean crustal evolution in Anshan of the North China Craton,Precambrian Research,2008.
[121]  Xu J F,Shinjo J,Defant M J,Wang Q Rapp R P,Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China:Partial melting of delaminated lower continental crust?,Geology,2002.
[122]  Yang Z M,Hou Z Q,White N C,Chang Z S,Li Z Q,Song Y C,Geology of the post-collisional porphyry copper molybdenum deposit at Qulong,Tibet,Ore Geology Reviews,2009.
[123]  Yang Z M,Xie Y L,Li G M,Xu J H,The characteristics and the forming process of ore-forming fluids at Qulong copper deposit in Gangdise porphy copper belt,Tibet,Geology and Prospecting,2005.
[124]  Ye H S,Mao J W,Li Y F,Guo B J Zhang C Q Liu J Yan Q R Liu G Y,SHRIMP zircon U-Pb and molybdenite Re-Os dating for the superlarge Donggou porphyry Mo deposit in East Qinling,China,and its geological implication,Acta Geologica Sinica,2006(7).
[125]  Yin A,Harrison T M,Geologic evolution of the Himalayan-Tibetan orogen,Annual Review of Earth and Planetary Sciences,2000.
[126]  Yogodzinski G M,Lees J M,Churikova T G,Dorendorf F,Woeerner G,Volynets O N,Geochemical evidence for the melting of subducting oceanic lithosphere at plate edges,Nature,2001.
[127]  Zhao Z H,Bao Z W,Zhang B Y,Geochemistry of the Mesozoic basaltic rocks in southern Hunan Province,Science in China(Series D),1998.
[128]  Zheng Y Y,Xue Y X,Cheng L J,Fang Z H Gao S B,Finding,characteristics and significances of Qulong superlarge porphyry copper(molybdenum) deposit,Tibet,Earth Sciences,2004.
[129]  黄典豪.吴澄宇.杜安道.何红蓼 东秦岭地区钼矿床的铼-锇同位素年龄及其意义 [J].-矿床地质1994(3)
[130]  黄典豪.吴澄宇.聂凤军 陕西金堆城斑岩钼矿床地质特征及成因探讨 [J].-矿床地质1987(3)
[131]  黄典豪.杜安道.吴澄宇.刘兰笙.孙亚莉.邹晓秋 华北地台钼(铜)矿床成矿年代学研究--辉钼矿铼-锇年龄及其地质意义 [J].-矿床地质1996(4)
[132]  黄典豪,侯增谦,杨志明,李振清,许道学,东秦岭钼矿带内碳酸岩脉型钼(铅)矿床地质-地球化学特征、成矿机制及成矿构造背景,地质学报,2009(12).
[133]  姜耀辉.蒋少涌.凌洪飞.戴宝章 陆-陆碰撞造山环境下含铜斑岩岩石成因--以藏东玉龙斑岩铜矿带为例 [J].-岩石学报2006(3)
[134]  江迎飞,富金斑岩型铜矿床研究进展,地质学报,2009(12).
[135]  李振清,杨志明,朱祥坤,侯增谦,李世珍,李志红,王?,西藏驱龙斑岩铜矿铜同位素研究,地质学报,2009(12).
[136]  刘孝善.吴澄宇.黄标 河南栾川南泥湖-三道庄钼(钨)矿床热液系统的成因与演化 [J].-地球化学1987(3)
[137]  孟祥金,董光裕,刘建光,江西冷水坑斑岩型铅锌银矿床,北京:地质出版社,2007.
[138]  孟祥金.侯增谦.高永丰.曲晓明.黄卫 碰撞造山型斑岩铜矿蚀变分带模式--以西藏冈底斯斑岩铜矿带为例 [J].-地学前缘2004(1)
[139]  孟祥金,侯增谦,董光裕,刘建光,左力艳,杨竹森,肖茂章,江西冷水坑斑岩型铅锌银矿床地质特征、热液蚀变与成矿时限,地质学报,2009(12).
[140]  聂风军.张洪涛.孙浩.樊建廷 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(2)
[141]  徐文艺.徐兆文.顾连兴.任启江.傅斌.牛翠? 安徽沙溪斑岩铜(金)矿床成岩成矿热历史探讨 [J].-地质论评1999(4)
[142]  徐兆文,杨荣勇,刘红樱,陆现彩,徐文艺,任启江,陕西金堆城斑岩钼矿床成矿流体研究,高校地质学报,1998.
[143]  杨志明,侯增谦,西藏驱龙超大型斑岩铜矿床的成因:流体包裹体及H、O同位素证据,地质学报,2009(12).
[144]  杨志明,侯增谦,初论碰撞造山环境斑岩铜矿成矿模型,矿床地质,2009(5).
[145]  杨志明.谢玉玲.李光明.徐九华 西藏冈底斯斑岩铜矿带驱龙铜矿成矿流体特征及其演化 [J].-地质与勘探2005(2)
[146]  杨志明.谢玉玲.李光明.徐九华.王葆华 西藏冈底斯斑岩铜矿带厅宫铜矿床流体包裹体研究 [J].-矿床地质2005(6)
[147]  杨志明.侯增谦.宋玉财.李振清.夏代详.潘凤雏 西藏驱龙超大型斑岩铜矿床:地质、蚀变与成矿 [J].-矿床地质2008(3)
[148]  叶会寿.毛景文.李永峰.郭保健.张长青.刘?.闫全人.刘国印 东秦岭东沟超大型斑岩钼矿SHRIMP锆石U-Pb和辉钼矿Re-Os年龄及其地质意义 [J].-地质学报2006(7)
[149]  翟明国.朱日祥.刘建明.孟庆任.侯泉林.胡圣标.李忠.张宏福.刘伟 华北东部中生代构造体制转折的关键时限 [J].-中国科学D辑2003(10)
[150]  翟裕生,姚书振,林新多,周?若,万天丰,长江中下游地区铁铜 (金) 成矿规律,北京:地质出版社,1992.
[151]  张国伟,郭安林,刘福田,肖庆辉,孟庆任,秦岭造山带三维结构及其动力学分析,中国科学d辑,1996.
[152]  张洪瑞,侯增谦,宋玉财,斑岩铜矿床在东特提斯成矿域中的时空分布特征,地质学报,2009(12).
[153]  张连昌.秦克章.英基丰.夏斌.舒建生 东天山土屋-延东斑岩铜矿带埃达克岩及其与成矿作用的关系 [J].-岩石学报2004(2)
[154]  张旗.王焰.刘伟.王元龙 埃达克岩的特征及其意义 [J].-地质通报2002(7)
[155]  张旗,王焰,王元龙,燕山期中国东部高原下地壳组成初探:埃达克质岩同位素Sr、Nd制约,岩石学报,2001(4).
[156]  张岳桥.董树文 郯庐断裂带中生代构造演化史:进展与新认识 [J].-地质通报2008(9)
[157]  赵振华.熊小林.王强.白正华.梅厚均 新疆西天山莫斯早特石英钠长斑岩铜矿床--一个与埃达克质岩石有关的铜矿实例 [J].-岩石学报2004(2)
[158]  郑有业.王保生.樊子珲.张华平 西藏冈底斯东段构造演化及铜金多金属成矿潜力分析 [J].-地质科技情报2002(2)
[159]  郑有业.薛迎喜.程力军.樊子珲.高顺宝 西藏驱龙超大型斑岩铜(钼)矿床:发现、特征及意义 [J].-地球科学-中国地质大学学报2004(1)
[160]  钟大赉.丁林.刘福田.刘建华.张进江.季建清.陈辉 造山带岩石层多向层架构造及其对新生代岩浆活动制约--以三江及邻区为例 [J].-中国科学D辑2000(Z1)
[161]  周珂.叶会寿.毛景文.屈文俊.周树峰.孟芳.高亚龙 豫西鱼池岭斑岩型钼矿床地质特征及其辉钼矿铼-锇同位素年龄 [J].-矿床地质2009(2)
[162]  朱金初,金章乐,饶冰,李福春,德兴铜矿斑岩铜矿流体过程,南京大学学报(自然科学版),2002(3).
[163]  朱训,黄崇轲,芮宗瑶,德兴斑岩铜矿,北京:地质出版社,1983.
[164]  Burnham C W,Magmas and hydrothermal fluids,New York:wiley,1979.
[165]  Burnham C W,Magmas and hydrothermal fluids,New York:John Wiley and Sons,Inc,1997.
[166]  Camus F,Silltioe R H,Petersen R,Andean copper deposits:new discoveries,mineralization style and metallogeny,Society of Economic Geologists Special Publication,1996.
[167]  Candela P A,Holland H D,The partitioning of copper and molybdenum between silicate melts and aqueous fluids,Geochimica et Cosmochimica Acta,1984.
[168]  Hou Z Q,Xie Y L,Xu W Y,Li Y Q Zaw K Beaudoin D Huang W Luobu C,Yulong deposit,East Tibet:A high-sulfidation Cu-Au porphyry copper deposit in the eastern Indo-Asian collision zone,International Geology Review,2007.
[169]  Hou Z Q,Zeng P S,Gao Y F,Dong F L,The Himalayan Cu-Mo-Au Mineralization in the eastern Indo-Asian Collision Zone:Constraints from Re-Os Dating of molybdenite,Mineralium Deposita,2006.
[170]  Hou Zengqian,Du A D,Wang S X,Qu X M,Re-Os age of porphyry copper deposits associated NS-striking normal faulting system on the Tibet from molybdenites,Science in China,2004.
[171]  Hou Z Q,Ma H W,Zaw K,Zhang Y Q,Wang M J,Wang Z,Pan G T,Tang R L,The Himalayan Yulong porphyry copper belt:Product of large-scale strike-slip faulting in Eastern Tibet,Economic Geology,2003.
[172]  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.
[173]  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.
[174]  Kesler S E,Copper,molybdenum and gold abundances in porphyry copper deposits,Economic Geology,1973.
[175]  Kilinc I A,Burnham C W,Partioning of chloride between a silicate melt and coexisting aqueous phase from 2 to 8 kilobars,Economic Geology,1972.
[176]  Kind R,Ni J,Zhao W,Wu J,Yuan X,Zhao L,Sandvol E,Reese C,Nabelek J,Hearn T,Evidence from earthquake data for partially molten crustal layerin Southern Tibet,Science,1996.
[177]  Li X H,Chen Z G,Liu D Y,Jurassic gabbro-granite-suites from southern Jiangxi Province,SE China:Age,origin and tectonic significance,International Geology Review,2003.
[178]  Li X H,Zhou H,Liu Y,Lee C Y,Sun M,Chen C H,Shoshonitic intrusive suite in SE Guangxi:Petrology and geochronology,Chinese Science Bulletin,2000.
[179]  Liang H Y,Sun W D,Su W C,Zartman R E,Porphyry copper-gold mineralization at Yulong,China,promoted by decreasing redox potential during magnetite alteration,Economic Geology,2007.
[180]  Lowell J D,Guilbert J M,Lateral and vertical alteration-mineralization zoning in porphyry ore deposits,Economic Geology,1970(4).
[181]  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.
[182]  Martin H,Adakitic magmas:Modern analogues of Archaean granitoids,Lithos,1999.
[183]  Masterman G,Berry R,Cooke D R,Walshe J L,Fluid chemistry,structural setting,and emplacement history of the Rosario Cu-Mo porphyry and Cu-Ag-Au epithermal veins,Collahuasi district,northern Chile,Economic Geology,2005.
[184]  Misra K C,Understanding mineral deposits,Kluwer Academic Publishers,2000.
[185]  Mo X X,Hou Z Q,Niu Y L,Dong G C Qu X M Zhao Z D Yang Z M,Mantle contributions to crustal thickening during continental collision:Evidence from Cenozoic igneous rocks in southern Tibet,Lithos,2007.
[186]  Pan Y,Dong P,The Lower Changjiang(Yangzi/Yangtze River) metallogenic belt,east central China:intrusion-and wall rock-hosted Cu-Fe-Au,Mo,Zn,Pb,Ag deposits,Ore Geology Reviews,1999(4).
[187]  Peacock S M,Rusher T,Thompson A B,Partial melting of subducting oceanic crust,Earth and Planetary Science Letters,1994.
[188]  Pichavant M,An experimental study of the effect of boron on a water saturated haplogranite at 1 kbar vapour pressure,Contributions to Mineralogy & Petrology,1981(4).
[189]  Pitzer K S,Pabalan R T,Thermodynamics of NaCl in steam,Geochimica et Cosmochimica Acta,1986.
[190]  Richards J P,Cumulative factors in the generation of giant calc-alkaline porphyry Cu deposits,PGC Publishng,Adelaide,2005.
[191]  Richards J P,Boyce A J,Pringle M S,Geologic evolution of the Escondida area,northern Chile:a model for spatial and temporal location of porphyry Cu mineralization,Economic Geology,2001.
[192]  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.
[193]  Richards J P,Tectono-magmatic precursors for porphyry Cu-(Mo-Au) deposit formation,Economic Geology,2003.
[194]  Rolland Y,Picard C,Pecher A,Lapierre H Bosch D Keller F,The Cretaceous Ladakh of NW Himalaya-slab melting and melt-mantle interacting during fast northwestern drift of Indian Plate,Chemical Geology,2002.
[195]  Sajona F G,Maury R C,Bellon H,Cotten J Defant M J Pubellier M,Initiation of subduction and the generation of slab melts in western and eastern Mindanao,Philippines,Geology,1993.
[196]  Sasso A M,Clark A H,Northwet Argentina:magmatic,hydrothermal and tectonic implications for Cu Au metallogeny in the Andean backarc,Society of Economic Geologists Newsletter,1998.
[197]  Seedorff E,Dilles J H,Proffett J M,Einaudi M T Zurcher L Stavast W J A Johnson D A Barton M D,Porphyry deposits:Characteristics and origin of hypogene features,2005.
[198]  Seltman R,Faragher A E,Collisional orogens and their related metallogeny; a preface,Czech Geological Survey,Prague,Czech Republic,1994.
[199]  Shinohara H,Hedenquist J W,Constraints on magma degassing beneath the Far Southeast porphyry Cu Au deposit,Philippines,1997.
[200]  Shinohara H,Kazahaya K,Lowenstern J B,Volatile transport in a convecting magma column:Implication for porphyry Mo mineralization,Geology,1995.
[201]  Sillitoe R H,A plate tectonic model for the origin of porphyry copper deposits,Economic Geology,1972.
[202]  Sillitoe R H,Geology of the Los Pelambres porphyry copper deposit,Chile Econ Geol,1973.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133