云南宝兴厂富碱斑岩型铜钼金多金属矿床构造—岩浆—成矿时空结构
|
摘要
宝兴厂钼铜金多金属矿床位于扬子地台西南缘的丽江台缘褶皱带南西端的边缘,北西向金沙江-哀牢山深大断裂与北北东向的程海-宾川深大断裂所挟持的三角地带。金沙江-哀牢山造山带是在被动大陆边缘裂谷环境基础上发展起来的一条陆内造山带。始新世早期(E_2~1)-渐新世晚(E_3~2),由于印度大陆-欧亚大陆汇聚碰撞和向北推挤,形成一系列的右行走滑断裂。其后由于印度大陆向北东方向的强烈楔入并与扬子大陆对接碰撞,造成强大的东西向挤压应力分量,以至渐新世晚期,金沙江-哀牢山断裂北段(德钦以北)呈SN向右行走滑,南段(德钦以南)呈左行走滑,构成东侧扬子陆块与西侧羌塘地体的边界断裂带。沿走滑断裂带发育新生代富碱侵入岩和钾质火山岩,宝兴厂矿区的马厂箐岩体位于其带中。
论文在前人区域研究成果的基础上,以成矿系统理论为指导,运用岩石学、构造地质学、矿床学、放射性同位素测年和示踪,主量、微量、稀土元素,稳定同位素,流体包裹体等多学科的方法进行了研究。
研究认为宝兴厂矿区马厂箐岩体成岩环境为碰撞后的大陆边缘的大陆弧环境,成岩物质来源于富集地幔与下地壳,是在拉张环境下下地壳岩石圈拆沉作用或地幔岩浆底侵过程中加厚的下地壳发生2～10%的部分熔融,分离结晶度为0.6,混染率为0.2的条件下形成的;岩浆活动时间跨度为23.18～55.49Ma;岩体属于富碱的斑岩,具有埃达克岩的特点;建立了矿区构造-岩浆-矿化的时空结构模型,探讨了钼铜金铅锌的成矿系列;确定了本区的矿床类型,钼铜矿为中高温岩浆热液型矿床,铜金为中温岩浆热液型矿床,金铅锌矿为中低温热液型矿床;根据矿化类型和产出位置划分了3种矿化类型:斑岩型钼-铜矿、接触带钼-铜-金矿、断裂带(破碎蚀变岩)铜-金-铅-锌矿,3种矿化类型属于同一成矿流体和同一成矿作用下不同成矿阶段演化的产物,构成了从高温高压→低温低压演化的系列;运用成岩成矿动力学机制模型进行了成矿预测,确定了6个预测靶区。
Baoxingchang Mo-Cu-Au polymetallic deposit located in the triangle land which surrounded by SW of fold in Lijiang platform edge,NW of deep-big fault of Jinshajiang-Ailaoshan and NNE of deep-big fault.Jinshajiang-Ailaoshan orogenic belt was an intracontinental orogenic belt which grew under marginal rift of passive continent.From early Eocene to later Oligocene epoch,a series of right-lateral strike slip fault formed by convergence and collision of Indian-Eurasian continent,and jostle in North,Thereafter EW strong compressional stress component formed by Indian continent wedging fiercely,and colliding with Yangtze continent in NE,Up to later Oligocene epoch,North part of Jinshajiang-Ailaoshan fault(North of Deqin) was SN left-slip,and formed bounding fault zone of East Yangtze landmass and West Qiangtang massif.Along the slip fault zone grew alkali-rich intrusive rock and kali lava in Cenozoic era,where Machangqing rock body of Baoxingchang deposit located in.
Based on the former theories;directed by metallogenic system;used lithology,tectonics, study of mineral deposit,trace and time by radioactive isotope,major and micro lanthanon, stable isotope and fluid inclusion as the methods to do the research.
The paper reveals that diagenetic environment of Machangqing rock body in Boxingchang deposit was continental arc environment of continental margin after collision. Diagenetic mineral rooted in rich mantle and lower crust,2～10%of lower crust that thickened caused by delamination of lithosphere in lower crust or subface erosion of magma in mantle was partial fusion,fractional crystal degree is 0.6,contamination ratio is 0.2,in extension environment;magmatic intrusive age is from 23.18 to 55.49Ma;rock body is alkali-rich porphyry with the character of adakite;it builds the space-time structure model of tectonics-magma-mineralization of the deposit,and discussed the metallogenic series of Mo-Cu-Au-Pb-Zn.Mo-Cu ore was high-medium temperature magmatic hydrothermal deposit;Cu-Au was medium temperature magmatic hydrothermal deposit;Au-Pb-Zn was medium-low temperature hydrothermal deposit,There were 3 types of mineralization: porphyry-type Mo-Cu deposit,contact belt Mo-Cu-Au deposit,fault zone(fracture altered rock) Cu-Au-Pb-Zn-Ag deposit;they all belonged to the same mineralizing fluid and mineralization,but in different mineralizing phases,all of which formed whole evolution series,temperature and pressure from high to low;it also predicted 6 prospecting areas by using model of diagenetic and mineralized dynamic mechanism.
论文在前人区域研究成果的基础上,以成矿系统理论为指导,运用岩石学、构造地质学、矿床学、放射性同位素测年和示踪,主量、微量、稀土元素,稳定同位素,流体包裹体等多学科的方法进行了研究。
研究认为宝兴厂矿区马厂箐岩体成岩环境为碰撞后的大陆边缘的大陆弧环境,成岩物质来源于富集地幔与下地壳,是在拉张环境下下地壳岩石圈拆沉作用或地幔岩浆底侵过程中加厚的下地壳发生2～10%的部分熔融,分离结晶度为0.6,混染率为0.2的条件下形成的;岩浆活动时间跨度为23.18～55.49Ma;岩体属于富碱的斑岩,具有埃达克岩的特点;建立了矿区构造-岩浆-矿化的时空结构模型,探讨了钼铜金铅锌的成矿系列;确定了本区的矿床类型,钼铜矿为中高温岩浆热液型矿床,铜金为中温岩浆热液型矿床,金铅锌矿为中低温热液型矿床;根据矿化类型和产出位置划分了3种矿化类型:斑岩型钼-铜矿、接触带钼-铜-金矿、断裂带(破碎蚀变岩)铜-金-铅-锌矿,3种矿化类型属于同一成矿流体和同一成矿作用下不同成矿阶段演化的产物,构成了从高温高压→低温低压演化的系列;运用成岩成矿动力学机制模型进行了成矿预测,确定了6个预测靶区。
Baoxingchang Mo-Cu-Au polymetallic deposit located in the triangle land which surrounded by SW of fold in Lijiang platform edge,NW of deep-big fault of Jinshajiang-Ailaoshan and NNE of deep-big fault.Jinshajiang-Ailaoshan orogenic belt was an intracontinental orogenic belt which grew under marginal rift of passive continent.From early Eocene to later Oligocene epoch,a series of right-lateral strike slip fault formed by convergence and collision of Indian-Eurasian continent,and jostle in North,Thereafter EW strong compressional stress component formed by Indian continent wedging fiercely,and colliding with Yangtze continent in NE,Up to later Oligocene epoch,North part of Jinshajiang-Ailaoshan fault(North of Deqin) was SN left-slip,and formed bounding fault zone of East Yangtze landmass and West Qiangtang massif.Along the slip fault zone grew alkali-rich intrusive rock and kali lava in Cenozoic era,where Machangqing rock body of Baoxingchang deposit located in.
Based on the former theories;directed by metallogenic system;used lithology,tectonics, study of mineral deposit,trace and time by radioactive isotope,major and micro lanthanon, stable isotope and fluid inclusion as the methods to do the research.
The paper reveals that diagenetic environment of Machangqing rock body in Boxingchang deposit was continental arc environment of continental margin after collision. Diagenetic mineral rooted in rich mantle and lower crust,2～10%of lower crust that thickened caused by delamination of lithosphere in lower crust or subface erosion of magma in mantle was partial fusion,fractional crystal degree is 0.6,contamination ratio is 0.2,in extension environment;magmatic intrusive age is from 23.18 to 55.49Ma;rock body is alkali-rich porphyry with the character of adakite;it builds the space-time structure model of tectonics-magma-mineralization of the deposit,and discussed the metallogenic series of Mo-Cu-Au-Pb-Zn.Mo-Cu ore was high-medium temperature magmatic hydrothermal deposit;Cu-Au was medium temperature magmatic hydrothermal deposit;Au-Pb-Zn was medium-low temperature hydrothermal deposit,There were 3 types of mineralization: porphyry-type Mo-Cu deposit,contact belt Mo-Cu-Au deposit,fault zone(fracture altered rock) Cu-Au-Pb-Zn-Ag deposit;they all belonged to the same mineralizing fluid and mineralization,but in different mineralizing phases,all of which formed whole evolution series,temperature and pressure from high to low;it also predicted 6 prospecting areas by using model of diagenetic and mineralized dynamic mechanism.
引文
[1]毕献武,胡瑞忠,叶造军,等.A型花岗岩类与铜成矿关系研究-以马厂箐铜矿为例.中国科学(D 辑),1999,2(6):489-495
[2]毕献武,胡瑞忠,彭建堂,等.姚安和马厂箐富碱侵入岩体的地球化学特征.岩石学报,2005,21(1):113-124
[3]毕献武,胡瑞忠,J.E.Mungall,等.与铜、金矿化有关的富碱侵入岩矿物化学研究.矿物学报,2006,26(4):377-385
[4]毕献武,胡瑞忠,何明友,等.哀牢山金矿带ESR年龄测定及其地质意义.科学通报,1996,14(14):1301-1303
[5]毕献武,胡瑞忠.哀牢山金矿带成矿流体稀土元素地球化学.地质论评,1998,44(3):264-269
[6]陈德潜,陈刚.实用稀土元素地球化学.北京:冶金工业出版社,1990
[7]陈岳龙,杨忠芳,赵志丹,等.同位素年代学与地球化学.北京:地质出版,2005
[8]陈骏,王鹤年.地球化学.北京:科学出版社,2004
[9]邓晋福,赵海玲,莫宣学,等.中国大陆根-柱构造-大陆动力学的钥匙.北京:地质出版社,1996
[10]邓晋福.火成岩构造组合与壳幔成矿系统.地学前缘,1999,6(2):259-270
[11]邓晋福,罗照华,苏尚国,等.岩石成因、构造环境与成矿作用.北京:地质出版社,2004
[12]邓万明,黄萱,钟大赉,等.滇西新生代富碱斑岩的岩石特征与成因.地质科学,1998,33(4):412-425
[13]邓万明,黄萱,钟大赉,等.滇西金沙江带北段的富碱斑岩及其与板内变形的关系.中国科学(D 辑),1998,28(2):111-117
[14]邓万明,孙宏娟.青藏高原新生代火山活动与高原隆升关系.地质论评,1999,45(增刊):952-958
[15]邓万明,郑锡澜,松本征夫,等.青海可可西里地区新生代火山岩的岩石特征与时代.岩石矿物学杂志,1996,15(4):289-298
[16]杜安道,何红蓼,殷宁万,等.辉钼矿的铼-锇同位素地质年龄测定方法研究.地质学报,1994,68(4):339-347
[17]杜安道,赵敦敏,王淑贤,等.Carius管溶样和负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄.岩矿测试,2001,20(4):247-252
[18]葛良胜,邹依林,李振华,等.云南马厂箐(铜、钼)金矿床地质特征及成因研究.地质与勘探,2002,38(5):11-17
[19]葛良胜,王文成,李汉光,等.滇西北富碱岩体与金矿成矿.北京:地震出版社,2005
[20]葛良胜.滇西北富碱岩浆活动与金多金属成矿系统[博士论文].北京:中国地质大学,2007
[21]何明友,胡瑞忠.哀牢山金矿带深源流体及其成矿作用.成都理工学院学报,1997,24(1):73-77
[22]何明勤,杨世瑜,刘家军,等.云南祥云金厂箐金(铜)矿床的成矿流体特征及流体来源.矿物岩石,2004,24(2):35-40
[23]何明勤,杨世瑜,陈昌勇,等.滇西小龙潭-马厂箐地区铜金多金属矿床地质地球化学及成因研究.北京:地质出版社,2004
[24]何明勤,杨世瑜,刘家军,等.云南祥云金厂箐金-铜矿床中的有机质及与金成矿的关系.昆明理工大学学报,2003,28(1):4-7
[25]侯增谦,莫宣学,高永丰,等.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.矿床地质,2003,22(1):1-12
[26]侯增谦,孟祥金,曲晓明,等.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.矿床地质,2005,24(2):108-121
[27]侯增谦,潘小菲,杨志明,等.初论大陆环境斑岩铜矿.现代地质,2007,21(2):332-351
[28]侯增谦,钟大赉,邓万明,等.青藏高原东缘斑岩铜钼金成矿带的构造模式.中国地质,2004,31(1):1-14
[29]侯增谦,杨岳清,曲晓明,等.三江地区义敦岛弧造山带演化与成矿系统.地质学报,2004,78(1):109-120
[30]侯增谦,曲晓明,王淑贤,等.西藏高原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(D辑),2003,33(7):609-618
[31]胡受权、郭文平.云南宁蒗地区喜山斯斑岩地质特征与成矿,地质与勘探,1996,32(3):7-13
[32]胡受权.滇西北宁蒗县白牛厂铅锌矿成矿地质条件,火山地质与矿产,1998,19(1):47-52
[33]胡受权.罗卜地喜山期斑岩地质特征与成矿远景,地质找矿论丛,1998,13(1):48-59
[34]胡受权,郭立平.云南宁蒗地区喜山期斑岩体岩石化学特征与成矿性及其岩浆来源探讨.岩石矿物学杂志,1998,17(2):136-144
[35]胡受权,曹运江,郭文平,等.宁蒗地区喜山期斑岩带成矿系列地质特征.矿产与地质,1998,12(4):217-224
[36]胡瑞忠,毕献武,何明友,等.哀牢山金矿带矿化剂对金矿的制约.中国科学(D辑),1998,28(增刊):24-30
[37]胡祥昭,黄震.扬子地台西缘富碱花岗斑岩特征及成因探讨.大地构造与成矿学,1997,21(2):173-180
[38]胡祥昭.扬子地台西缘富碱斑岩成矿专属性,中南工业大学学报,1996,27(2):127-131
[39]胡云中,唐尚鹑,王海平,等.哀牢山金矿地质.北京:地质出版社,1995
[40]黄智龙,金志升,朱成明,等.云南老王寨金矿区煌斑岩的Sm-Nd同位素研究.地球学报-中国地质科学院院报,1997,18(增刊):160-163
[41]黄智龙,刘丛强,朱成民,等.云南老王寨金矿区煌斑岩成因及其与金矿化的关系.北京:地质出版社,1999
[42]黄智龙、王联魁、朱成明,等.云南马厂箐金矿区煌斑岩地球化学及成因探讨,矿物岩石,1996,16(2):82-89
[43]梁华英,谢应雯,张玉泉,等.富钾碱性岩体形成演化对铜矿成矿制约-以马厂箐铜矿为例.自然科学进展,2004,14(1):116-120
[44]刘秉光,陆德复,蔡新平,等.滇川西部金矿床研究.北京:海洋出版社,1999
[45]李昌年.火成岩微量元素岩石学.武汉:中国地质大学出版社,1992
[46]李定谋,曹志敏,覃功炯,等.哀牢山蛇绿混杂岩带金矿床,北京:地质出版社,1998
[47]李定谋,李保华.云南哀牢山金矿床的成矿条件.沉积与特提斯地质,2000,20(1):60-77
[48]李元.墨江金矿床的成矿物质来源.云南地质,1992,11(2):130-143
[49]刘福田,刘建华,何建坤,等.滇西特提斯造山带下扬子地块的俯冲板片.科学通报,2000,45(1):79-83
[50]李峰,段嘉瑞.滇西地区板块-地体构造.昆明理工大学学报,1999,24(1):29-35
[51]刘红涛,孙世华,刘建国,等.华北北缘地区中生代高锶花岗岩类-地球化学与源区性质.岩石学报,2002,18(3):257-274
[52]刘红涛,张旗,刘建明,等.埃达克岩与Cu-Au成矿作用有待深入研究的岩浆成矿关系.岩石学报,2004,20(2):205-218
[53]吕伯西,王增,张能德,等.“三江”地区花岗岩类及其成矿专属性.北京:地质出版社,1993
[54]刘晓煌,孙柏年,屈文俊,等.北祁连山西段西柳沟钨钼矿的Re-Os定年及地质意义.岩石学报,2007,32(10):2434-2442
[55]刘显凡,刘家铎,张成江,等.滇西富碱斑岩型矿床岩体和矿脉同位素地球化学研究.矿物岩石地球化学通报,2004,23(1):32-39
[56]刘显凡.富碱斑岩特征及其成岩成矿地球化学机制研究[博士后论文].中国科学院地球化学研究所,1999
[57]刘显凡,战新志,高振敏,等.云南六合深源包体与富碱斑岩成矿的关系.中国科学(D 辑),1999,29(5):413-420
[58]李兴振,刘文均,王义昭,等.西南三江地区特提斯构造演化与成矿(总论).北京:地质出版社,1999
[59]李兴振,刘文均,王义昭,等.西南“三江”地区特提斯构造演化与成矿(总论).北京:地质出版社,1999
[60]刘增乾,李兴振,叶庆同,等.“三江”地区构造岩浆带的划分与矿产分布规律.北京:地质出版社,1993
[61]罗建宁,张正贵,陈明,等.“三江”特提斯沉积地质与成矿.北京:地质出版社,1992
[62]罗建宁,杜德勋.西南三江地区沉积地质与成矿.北京:地质出版社,1999
[63]莫宣学,路风香,沈上越,等.“三江”特提斯火山作用与成矿.北京:地质出版社,1993
[64]莫宣学,沈上越,朱勤文,等.“三江”中南段火山岩-蛇绿岩与成矿.北京:地质出版社,1998
[65]马鸿文.论西藏玉龙斑岩铜矿带岩浆侵入时代.地球化学,1989,3:210-216
[66]潘桂棠,陈智梁,李兴振,等.东特提斯地质构造形成演化.北京:地质出版社,1997
[67]潘桂棠,李定谋,李兴振,等.西南“三江”地区贵金属、有色金属成矿规律和成矿模式.当代矿产资源勘查,1999,2:12-16
[68]潘桂棠,徐强,侯增谦,等.西南“三江”多岛弧造山过程成矿系统与资源评价.北京:地质出版社,2003
[69]彭建堂,毕献武,胡瑞忠,等.滇西马厂箐斑岩铜(钼)矿床成岩成矿时限的厘定.矿物学报,2005,25(1):69-74
[70]曾普胜,侯增谦,高永峰,等.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.地质论评,2006,52(1):72-84
[71]甫为民,胡锦平.鹤庆北衙富碱斑岩侵入体的岩石学特征及其构造环境.云南地质,1994,13(1):25-28
[72]屈文俊,杜安道.高温密闭溶样电感耦合,等离子体质谱准确测定辉钼矿铼-锇地质年龄.岩矿测试,2003,22(4):254-257
[73]屈文俊.杜安道.电感耦合等离子体质谱测定辉钼矿中Re、Os含量时的质量分馏效应的校正.质谱学报,2004,25(增刊):181-182
[74]曲晓明,侯增谦,黄卫,等.冈底斯斑岩铜成矿带:西藏第二条“玉龙”斑岩铜矿带.矿床地质,2001,20(4):355-366
[75]邱家骧.应用岩浆岩石学.武汉:中国地质大学出版社,1991
[76]邱家骧.岩浆岩石学.北京:地质出版社,1983
[77]任胜利.云南镇沅老王寨-冬瓜林金矿床的地球化学研究.矿物岩石地球化学通讯,1993,4:199-201
[78]芮宗瑶,黄崇轲,齐国明,等.中国斑岩型铜(钼)矿.北京:地质出版社,1984
[79]沈上越,魏启荣,程惠兰,等.云南哀牢山金矿带成因类型探讨.特提斯地质,1997,21(21):73-84
[80]沈渭洲.稳定同位素地质.北京:原子能出版社,1997
[81]涂光炽,张玉泉,赵震华,等.华南两个富碱侵入岩带的初步研究-花岗岩地质和成矿关系.南京:江苏科学技术出版社,1984
[82]涂光炽,徐克勤.花岗岩地质和成矿关系.南京:江苏科学出版社,1986
[83]涂光炽.关于富碱侵入岩.矿产与地质,1989,13(3):1-4
[84]唐仁鲤,罗怀松.西藏玉龙斑岩铜(钼)矿带地质.北京:地质出版社,1993
[85]王强,赵振华,熊小林,等.底侵玄武质下地壳的熔融:来自安微沙溪埃达克(adakite)质富钠石英闪长玢岩的证据.地球化学,2001,30(4):353-362
[86]王强,赵振华,许继峰,等.鄂东南铜山口、殷祖埃达克质岩(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.岩石学报,2004,20(02)351-360
[87]王强,许继峰,王建新,等.大别山adakite型灰色片麻岩的确立及其与超高压变质作用的关系. 科学通报,2000,46(10):1017-1024
[88]王登红,陈毓川,徐珏,等.中国新生代的金属成矿作用的主要特点与成矿系列.中国地质学会:第31届国际地质大会中国代表团学术论文集.北京:地质出版社,2001
[89]王登红,屈文俊,李志伟,等.金沙江-红河成矿带斑岩铜钼矿的成矿集中期:Re-Os同位素定年.中国科学(D辑地球科学),2004,34(4):345-349
[90]杨建民,薛春纪,徐珏,等.滇西北喜马拉雅期富碱斑岩地质特征及其成矿作用.陈毓川.喜马拉雅期内生成矿作用研究.北京:地质出版社,2002
[91]李汉光,郭晓东,王绍明,等.云南宝兴厂金矿床地质特征及成因.矿床地质,2008,27(5):587-595
[92]王建、李建平、王江海,等.滇西剑川-大理地区新生代钾玄岩系中深源包体的地质意义,岩石学报,2002,22(2):113-124
[93]王义昭,李兴林,段丽兰,等.三江地区南段大地构造与成矿.北京:地质出版社,2000
[94]熊德信,孙晓明,石贵勇,等.云南哀牢山喜马拉雅期造山型金矿带矿床地球化学及成矿模式.北京:地质出版社,2007
[95]杨建琨,唐志国.云南省新生代浅成侵入斑岩型金矿成矿特征及找矿预测.北京地质,1996,3:27-31
[96]冶金工业部地质研究所.中国斑岩铜矿,北京:科学出版社,1984
[97]应汉龙.云南墨江镍金矿床富金石英脉的~(40)Ar/~(39)Ar快中子活化年龄.地质科学,2002,31(1):107-109
[98]应汉龙,蔡新平,刘秉光,等.云南墨江金矿成矿作用探讨.地质地球化学,2000,28(1):1-9
[99]应汉龙,蔡新平.云南北衙矿区富碱斑岩正长石和白云母的~(40)Ar-~(39)Ar年龄.地质科学,2004,39(1):107-110
[100]俞广钧.马厂箐金矿床成矿地质条件及其成因探讨.昆明工学院学报,1988,1:1-10
[101]云南省地质调查局.大理幅1:20万区域地质调查报告(地质部分),1973,1～150
[102]云南省地质调查局.大理县幅、下关市幅、凤仪镇幅1:5万区域地质调查报告.北京:地质出版社,1990
[103]云南省地质矿产局.大理幅1:20万水系沉积物测量地球化学图说明书.北京:地质出版社,1990
[104]云南省地质矿产局.云南省区域地质志.北京:地质出版社,1990
[105]张旗,王焰,钱青,等.中国东部中生代埃达克岩特征及其构造-成矿意义.岩石学报,2001,17(2):236-244
[106]张旗,李承东,王焰,等.中国东部中生代高Sr低Yb和低Sr高Yb型花岗岩对比及其地质意义,岩石学报,2005,21(6):1527-1529
[107]张旗,钱青,王二七,等.燕山中晚期的中画东部高原:埃达克岩的启示.地质科学,2001,36(2):248-255
[108]张旗,王焰,刘红涛,等.中国埃达克岩的时空分布及其形成背景.地学前缘,2003,10(4):385-400
[109]张旗,王焰,玉元龙,等.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约.岩石学报,2001,17(4):505-513
[110]张旗,桑克章,王元龙,等.加强埃达克岩研究,开创中国Cu、Au等找矿工作的新局面.岩石学报,2004,20(2):195-204
[111]张旗,许继峰,王焰,等.埃达克岩的多样性.地质通报,2004,23(9-10):959-965
[112]张旗,王焰,刘伟,等.埃达克岩的特征及其意义.地质通报,2002,21(7):431-435
[113]张旗,周德进,赵大升,等.滇西古特提斯造山带的威尔逊旋回:岩浆活动记录和深部过程讨论,岩石学报,1996,12(1):17-28
[114]张理刚.稳定同位素在地质科学中的应用.西安:陕西科学技术出版社,1985
[115]赵振华.稀土元素地球化学研究方法.地质地球化学,1982,1:65-66
[116]赵振化.微量元素地球化学原理.北京:科学出版社,1997
[117]赵振化,周玲棣.我国某些富碱侵入岩的稀土元素地球化学,中国科学(B),1994,24(10):1110-1113
[118]张海涛,杨家瑞.超基性岩蚀变热液型金矿床-云南金厂矿床成因探讨.云南地质,1984,3(4):311-325
[119]张玉泉.哀牢山-金沙江富碱侵入岩及其与裂谷构造关系初步研究,岩石学报.1987,1:17-25
[120]张玉泉,谢应雯,梁华英,等.藏东玉龙铜矿带含矿斑岩及成岩系列.地球化学,1998,27(3):236-243
[121]张玉泉,谢应雯.哀牢山-金沙江富碱侵入岩年代学和Nd,Sr同位素特征.中国科学(D 辑),1997,27(4):289-293
[122]张玉泉,谢应雯,邱华宁,等.钾玄岩系列:藏东玉龙铜矿带含矿斑岩sr,Nd,Pb同位素组成.地质科学,1998,33(3):359-366
[123]周玲棣,赵振华.我国富碱侵入岩的岩石学和岩石化学特征,中国科学(B辑).1994,24(10):1093-1095
[124]中国人民武装警察部队黄金第十三支队.云南省祥云县金厂箐岩金矿勘探报告.1993
[125]中国人民武装警察部队黄金第十支队.云南省大理州宝兴厂矿区人头箐矿段金矿普查报告.2007
[126]朱炳泉.地球科学中同位素体系理论与应用-兼论中国大陆壳幔演化.北京:科学出版社,1998
[127]朱创业,夏文杰,尹海生,等.兰坪-思茅中生代盆地性质及构造演化.成都理工学院学报,1997,24(4):23-30
[128]钟大赉.滇川西部古特提斯造山带.北京:科学出版社,1998
[129]钟立志,何毅特,李宗光,等.扬子地台西缘富碱斑岩铜金多金属成矿区划及成矿地质条件分析.西南矿产地质,1996,1-2
[130] Atheron, M. P. and Petford, N. Generation of sedium-rich magmas, 1993, 25
[131] Burnham C W and ohmoto H. Late-stage processes of feisic magmatism. In Ishihora S and Takenouchi S, (ed), Mining Geology Special Issue , 1980,8:1—11
[132] Burnham C W. Magma and hydrothermal fluidsA . In:Barnes HL ed. Geochemistry of hydrothermal ore deposits C. 2nd ed. New York :Wiley, 1979, 71—136
[133] Clayton R N,O' neil J R and Mayeda T K,Oxygen isotope exchange between quartz and water. Geophys. Res. 77.1972, 3057-3067
[134] Candela P A. Controls on ore metal ratios in grante-related oresystems:An experimental and computational approaeh. Transaetions of the Royal Soeiety of Edinburgh, Earth Seienees, 1992,83:317
[135] Cline J and Bodnar R J. Can economic porphyry copper mineralization be generated by a typical cale-alkaline melt?. Journal of Geophysical Research, 1991,96:8113-8126
[136] Cooke D R,Hollings P, and Walshe J L. .Giant Porphyry Deposits: Characteristics.dis tribution,and tectonic controls. Econ. Geol, 2005,100:801—818
[137] Defant M J, Drummond MS. Derivation of some modem arc magmas by reeking of young subducted lilhosphere. Nature, 1990, 347:662-665
[138] Dilles J H. Petrology of the yerington Batholith, Nevada:Evidence for evolution of porphyry copper ore fluids. Economic Geology,1987, 82:1750—1780
[139] Harris, N.B.W.Pearce.J. A. and Tindle .A. G. Geochemical Characteristics of collisionz one magmatism. In Collision Tectonic. ed. by Coaward.M.P.etal. Geol. Soc. Sp. publ, 1986,19:67-81
[140] Heinrich C A. The physical and chemical evolution of low-Salinity magmatic fluids at the porphyry to epithermal transition:a thermodynamic study.Mineralium Deposita, 2005,39:864-889
[141] Heinrich C A, Gunther D, Audetat A, Ulrich T and Frischknecht R. Metal fractionation between magmatic brine and vapor, determined by microanalysis of fluid inclusions. Geology, 1999,27:755-758
[142] Hedenquist J W, and Lowenst J B. The role of magmas in formation of hydrothermal ore deposits. Nature, 1994, 370:519-527
[143] Hollister V F, Potter R R, and Barker A L. Porphyry-tyoe deposits of the Appalachian orogen. Econ. Geol, 1974, 69:618—630
[144] Hollister V F, Potter R R, and Barker A L Porphyry-tyoe deposits of the Appalachian orogen. Econ. Geol, 1974,69:618-630
[145] Hou ZQ, Qu XM, Wang SX,et al. Re-Os age for molybdenites from the Gangdese porphyry copper belt in the Xizang (Tibetan) plateau: implication to mineralization duration and geodynamic settings. Science in China,2003,33:509—518
[146] Gustafson L B, and Hunt J P. The porphyry copper deposits at El Salvador, Chile[J]. Econ.Geol, 1975, 70:857-912
[147] Kay RW, Kay SM. Creation and destruction of lower continental crust. Geologische Rundsehau, 1991, 80:259～278
[148] Kay RW, Kay SM. Delamination and detanaination Tecconophyssics. 1993,219:177—189
[149] Kay R W. Aleutian magnesium andesites:melts from subducted Pacific oceanic crust. J. Volcanol. Geotherm. Res, 1978,4:117～132
[150] Le Maitre RW. A Classification of Igneous Rocks and Glossary of Terms. Blac-kwell. Oxford, 1989:193
[151] Lowell J D, Guibert J M. Lateral and vertical alteration-mineralization zoning in porphyry ore deposits. Econ Geal, 1974,65:373～408
[152] Middlemost E A K .Magmas and magmatic rocks.Longmas.London & New York. 1985:1—275
[153] Martin H. Smithies RH, RappR, MoyenJ-F, Champion D. An overview of adakite. lonalite-trondhjemite-granodiorite (TTG) , and sanukitoid: relationships and some implications for crustal evolution. Lilhos, 2005,79:1—24
[154] Muller D, Groves D I. Direct and indirect associations between potassic igneous rocks, shoshonites and gold-copper deposits. Ore Geology Reviews, 1993, 8:383～406
[155] Sillitoe R H. A plate tectonic model for the origin of porphyry capper deposits. Econ. Geol, 1972,67:184-197
[156] Muller D,StumpS E F, Taylor W R. Shoshonitic and alkaline lamprophyres with elevated Au and PGE concentrations from the Kreuzeck Mountains, Eastern Alps. Austria-Mineral PetrOl, 1992,46:23～42
[157] Martin H. Adakitic magmas:Modern analoguesof Archean granitoidsJ. Lithos, 1999, 46: 411 -429
[158] Mitchell A H G. Metallogenic belts and angle of dip of Benioff zones. Nature, 1973,245:49-52
[159] Ohmoto H. Systematics of sulfur and carbon isotopes in hydrothermal ore deposits. Econ Geol, 1972,67:551—579
[160] Ohmoto H, Rye R O. Isotope of Sulfur and Carbon. In:Geochemistry of Hydrothermal Ore Deposits, 2nd Edeition, John Wiley and Sons. New York, 1979:509—567
[161]Peccerillo R and Taylor S R. Geochemistry of eocene calc-alkaline volcanic rocKs from the Kastamonu area. Northern Turkey. Contrib. Mineral Petrol, 1976, 58(1): 63—81
[162]Petford N, Atherton MP, Halliday AN. Rapid magma production rates, Pitcher. W.S. Granite type and teconic environment.Mountain building processes, 1983:19—37
[163] Pitcher. W.S. Granite and yet more granites forty years on. Rundschau, 1987, 76(1) :51—79
[164]Rapp R P. Shimizu N Norman M D, Growth of early continental. crust by partial melting of eclogite. Nature, 2003, 425:605—609
[165] Redmond P B,Einaudi M T, Inan E E, Landtwing M R, and Heinrich C A. Copper deposition by fluid cooling in intrusion-centered systems:New insights from the Bingham porphyry ore deposit, Utah. Geology, 2004:217～230
[166]Rusk B G, Reed M H,Dilles J H,Klemm L M and Heinrich C A. Compositions of magmatic hydrothermal fluids determined by La-ICP-MS of fluid inclusion from the porphyry copper-molybdenum deposit at Butte, MT. Chemical Geology, 2004, 210:173—199
[167]Richards J P,Boyce A J and Pringle M S. Geologic evolution of the Escondida area, northern Chile: a model for spatial and temporal location of porphyry Cu mineralization. Econ. Geol, 2001, 96:271-306
[168]Richards,J P. Cumulative factors in the generation of giant cale-alkaline porphyry Cu deposits: In Porter T. M. (ed). Super-Porphyry Copper and Gold Deposits:A Global Perspective, PGC Publishng, Adelaide, pp, 2005:7—25
[169]Richard G, Monnereau M, Ingrin J. Is t he t ransition zone an empty water reservoir ? Inferences from numerical model of mantle dynamics. Earth and Planetary Science Letters, 2002, 205:37-51
[170] Richards J P. Tectono-magmatic precursors forporphyryCu-(Mo-Au) deposit formation. Economic Geology, 2003, 98:1515-1533
[171] Richards J P, McCulloch, M T, Chappell,B W, et al. Sourcesof metals in the Porgera gold deposit, PapuaNew Guinea: evidence from alteration, isotope, and noble metal geochemistry. Geochim et Cosmochim Acta, 1991, 55:565—580
[172]Richards J P. Alkalic-type epithermal gold deposits-a review. Mineralogical Association of Canada Short Course Series,1995,23:367—400
[173]Richards J P ang Kerrich R. Adakike-like rocks:Their diverse origins and questionable role in metallogenesis.Economic Geology, 2007, 102:537—576
[174]Sajona F G and Maury R C. Association of adakites with gold and copper mineralization in the Philippines. CR. Acad. Sci. Paris, 1998, 326(1):27—34
[175]Sillitoe R H. A plate tectonic model for the origin of porphyry copper deposits[J]. Econ. Geol., 1972,67:184-197
[176]Sillitoe R H. Geology of the Los Pelambres porphyry copper deposits,Chile. Econ. Geol, 1973,67:1-10
[177]Sillitoe R H. Andean mineralization:a model for the metallogeny of convergent plate margins. In Strong D F, (ed.), Metallogeny and Plate tectonis,Geol. Assoc. Can ada, special Paper, 1976,14:59—100
[178]Uyeda S, Kanamori H. Back-arc opening and the model of subduction. Jour Geophys Res, 1979,84:1040-1061
[2]毕献武,胡瑞忠,彭建堂,等.姚安和马厂箐富碱侵入岩体的地球化学特征.岩石学报,2005,21(1):113-124
[3]毕献武,胡瑞忠,J.E.Mungall,等.与铜、金矿化有关的富碱侵入岩矿物化学研究.矿物学报,2006,26(4):377-385
[4]毕献武,胡瑞忠,何明友,等.哀牢山金矿带ESR年龄测定及其地质意义.科学通报,1996,14(14):1301-1303
[5]毕献武,胡瑞忠.哀牢山金矿带成矿流体稀土元素地球化学.地质论评,1998,44(3):264-269
[6]陈德潜,陈刚.实用稀土元素地球化学.北京:冶金工业出版社,1990
[7]陈岳龙,杨忠芳,赵志丹,等.同位素年代学与地球化学.北京:地质出版,2005
[8]陈骏,王鹤年.地球化学.北京:科学出版社,2004
[9]邓晋福,赵海玲,莫宣学,等.中国大陆根-柱构造-大陆动力学的钥匙.北京:地质出版社,1996
[10]邓晋福.火成岩构造组合与壳幔成矿系统.地学前缘,1999,6(2):259-270
[11]邓晋福,罗照华,苏尚国,等.岩石成因、构造环境与成矿作用.北京:地质出版社,2004
[12]邓万明,黄萱,钟大赉,等.滇西新生代富碱斑岩的岩石特征与成因.地质科学,1998,33(4):412-425
[13]邓万明,黄萱,钟大赉,等.滇西金沙江带北段的富碱斑岩及其与板内变形的关系.中国科学(D 辑),1998,28(2):111-117
[14]邓万明,孙宏娟.青藏高原新生代火山活动与高原隆升关系.地质论评,1999,45(增刊):952-958
[15]邓万明,郑锡澜,松本征夫,等.青海可可西里地区新生代火山岩的岩石特征与时代.岩石矿物学杂志,1996,15(4):289-298
[16]杜安道,何红蓼,殷宁万,等.辉钼矿的铼-锇同位素地质年龄测定方法研究.地质学报,1994,68(4):339-347
[17]杜安道,赵敦敏,王淑贤,等.Carius管溶样和负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄.岩矿测试,2001,20(4):247-252
[18]葛良胜,邹依林,李振华,等.云南马厂箐(铜、钼)金矿床地质特征及成因研究.地质与勘探,2002,38(5):11-17
[19]葛良胜,王文成,李汉光,等.滇西北富碱岩体与金矿成矿.北京:地震出版社,2005
[20]葛良胜.滇西北富碱岩浆活动与金多金属成矿系统[博士论文].北京:中国地质大学,2007
[21]何明友,胡瑞忠.哀牢山金矿带深源流体及其成矿作用.成都理工学院学报,1997,24(1):73-77
[22]何明勤,杨世瑜,刘家军,等.云南祥云金厂箐金(铜)矿床的成矿流体特征及流体来源.矿物岩石,2004,24(2):35-40
[23]何明勤,杨世瑜,陈昌勇,等.滇西小龙潭-马厂箐地区铜金多金属矿床地质地球化学及成因研究.北京:地质出版社,2004
[24]何明勤,杨世瑜,刘家军,等.云南祥云金厂箐金-铜矿床中的有机质及与金成矿的关系.昆明理工大学学报,2003,28(1):4-7
[25]侯增谦,莫宣学,高永丰,等.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.矿床地质,2003,22(1):1-12
[26]侯增谦,孟祥金,曲晓明,等.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.矿床地质,2005,24(2):108-121
[27]侯增谦,潘小菲,杨志明,等.初论大陆环境斑岩铜矿.现代地质,2007,21(2):332-351
[28]侯增谦,钟大赉,邓万明,等.青藏高原东缘斑岩铜钼金成矿带的构造模式.中国地质,2004,31(1):1-14
[29]侯增谦,杨岳清,曲晓明,等.三江地区义敦岛弧造山带演化与成矿系统.地质学报,2004,78(1):109-120
[30]侯增谦,曲晓明,王淑贤,等.西藏高原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(D辑),2003,33(7):609-618
[31]胡受权、郭文平.云南宁蒗地区喜山斯斑岩地质特征与成矿,地质与勘探,1996,32(3):7-13
[32]胡受权.滇西北宁蒗县白牛厂铅锌矿成矿地质条件,火山地质与矿产,1998,19(1):47-52
[33]胡受权.罗卜地喜山期斑岩地质特征与成矿远景,地质找矿论丛,1998,13(1):48-59
[34]胡受权,郭立平.云南宁蒗地区喜山期斑岩体岩石化学特征与成矿性及其岩浆来源探讨.岩石矿物学杂志,1998,17(2):136-144
[35]胡受权,曹运江,郭文平,等.宁蒗地区喜山期斑岩带成矿系列地质特征.矿产与地质,1998,12(4):217-224
[36]胡瑞忠,毕献武,何明友,等.哀牢山金矿带矿化剂对金矿的制约.中国科学(D辑),1998,28(增刊):24-30
[37]胡祥昭,黄震.扬子地台西缘富碱花岗斑岩特征及成因探讨.大地构造与成矿学,1997,21(2):173-180
[38]胡祥昭.扬子地台西缘富碱斑岩成矿专属性,中南工业大学学报,1996,27(2):127-131
[39]胡云中,唐尚鹑,王海平,等.哀牢山金矿地质.北京:地质出版社,1995
[40]黄智龙,金志升,朱成明,等.云南老王寨金矿区煌斑岩的Sm-Nd同位素研究.地球学报-中国地质科学院院报,1997,18(增刊):160-163
[41]黄智龙,刘丛强,朱成民,等.云南老王寨金矿区煌斑岩成因及其与金矿化的关系.北京:地质出版社,1999
[42]黄智龙、王联魁、朱成明,等.云南马厂箐金矿区煌斑岩地球化学及成因探讨,矿物岩石,1996,16(2):82-89
[43]梁华英,谢应雯,张玉泉,等.富钾碱性岩体形成演化对铜矿成矿制约-以马厂箐铜矿为例.自然科学进展,2004,14(1):116-120
[44]刘秉光,陆德复,蔡新平,等.滇川西部金矿床研究.北京:海洋出版社,1999
[45]李昌年.火成岩微量元素岩石学.武汉:中国地质大学出版社,1992
[46]李定谋,曹志敏,覃功炯,等.哀牢山蛇绿混杂岩带金矿床,北京:地质出版社,1998
[47]李定谋,李保华.云南哀牢山金矿床的成矿条件.沉积与特提斯地质,2000,20(1):60-77
[48]李元.墨江金矿床的成矿物质来源.云南地质,1992,11(2):130-143
[49]刘福田,刘建华,何建坤,等.滇西特提斯造山带下扬子地块的俯冲板片.科学通报,2000,45(1):79-83
[50]李峰,段嘉瑞.滇西地区板块-地体构造.昆明理工大学学报,1999,24(1):29-35
[51]刘红涛,孙世华,刘建国,等.华北北缘地区中生代高锶花岗岩类-地球化学与源区性质.岩石学报,2002,18(3):257-274
[52]刘红涛,张旗,刘建明,等.埃达克岩与Cu-Au成矿作用有待深入研究的岩浆成矿关系.岩石学报,2004,20(2):205-218
[53]吕伯西,王增,张能德,等.“三江”地区花岗岩类及其成矿专属性.北京:地质出版社,1993
[54]刘晓煌,孙柏年,屈文俊,等.北祁连山西段西柳沟钨钼矿的Re-Os定年及地质意义.岩石学报,2007,32(10):2434-2442
[55]刘显凡,刘家铎,张成江,等.滇西富碱斑岩型矿床岩体和矿脉同位素地球化学研究.矿物岩石地球化学通报,2004,23(1):32-39
[56]刘显凡.富碱斑岩特征及其成岩成矿地球化学机制研究[博士后论文].中国科学院地球化学研究所,1999
[57]刘显凡,战新志,高振敏,等.云南六合深源包体与富碱斑岩成矿的关系.中国科学(D 辑),1999,29(5):413-420
[58]李兴振,刘文均,王义昭,等.西南三江地区特提斯构造演化与成矿(总论).北京:地质出版社,1999
[59]李兴振,刘文均,王义昭,等.西南“三江”地区特提斯构造演化与成矿(总论).北京:地质出版社,1999
[60]刘增乾,李兴振,叶庆同,等.“三江”地区构造岩浆带的划分与矿产分布规律.北京:地质出版社,1993
[61]罗建宁,张正贵,陈明,等.“三江”特提斯沉积地质与成矿.北京:地质出版社,1992
[62]罗建宁,杜德勋.西南三江地区沉积地质与成矿.北京:地质出版社,1999
[63]莫宣学,路风香,沈上越,等.“三江”特提斯火山作用与成矿.北京:地质出版社,1993
[64]莫宣学,沈上越,朱勤文,等.“三江”中南段火山岩-蛇绿岩与成矿.北京:地质出版社,1998
[65]马鸿文.论西藏玉龙斑岩铜矿带岩浆侵入时代.地球化学,1989,3:210-216
[66]潘桂棠,陈智梁,李兴振,等.东特提斯地质构造形成演化.北京:地质出版社,1997
[67]潘桂棠,李定谋,李兴振,等.西南“三江”地区贵金属、有色金属成矿规律和成矿模式.当代矿产资源勘查,1999,2:12-16
[68]潘桂棠,徐强,侯增谦,等.西南“三江”多岛弧造山过程成矿系统与资源评价.北京:地质出版社,2003
[69]彭建堂,毕献武,胡瑞忠,等.滇西马厂箐斑岩铜(钼)矿床成岩成矿时限的厘定.矿物学报,2005,25(1):69-74
[70]曾普胜,侯增谦,高永峰,等.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.地质论评,2006,52(1):72-84
[71]甫为民,胡锦平.鹤庆北衙富碱斑岩侵入体的岩石学特征及其构造环境.云南地质,1994,13(1):25-28
[72]屈文俊,杜安道.高温密闭溶样电感耦合,等离子体质谱准确测定辉钼矿铼-锇地质年龄.岩矿测试,2003,22(4):254-257
[73]屈文俊.杜安道.电感耦合等离子体质谱测定辉钼矿中Re、Os含量时的质量分馏效应的校正.质谱学报,2004,25(增刊):181-182
[74]曲晓明,侯增谦,黄卫,等.冈底斯斑岩铜成矿带:西藏第二条“玉龙”斑岩铜矿带.矿床地质,2001,20(4):355-366
[75]邱家骧.应用岩浆岩石学.武汉:中国地质大学出版社,1991
[76]邱家骧.岩浆岩石学.北京:地质出版社,1983
[77]任胜利.云南镇沅老王寨-冬瓜林金矿床的地球化学研究.矿物岩石地球化学通讯,1993,4:199-201
[78]芮宗瑶,黄崇轲,齐国明,等.中国斑岩型铜(钼)矿.北京:地质出版社,1984
[79]沈上越,魏启荣,程惠兰,等.云南哀牢山金矿带成因类型探讨.特提斯地质,1997,21(21):73-84
[80]沈渭洲.稳定同位素地质.北京:原子能出版社,1997
[81]涂光炽,张玉泉,赵震华,等.华南两个富碱侵入岩带的初步研究-花岗岩地质和成矿关系.南京:江苏科学技术出版社,1984
[82]涂光炽,徐克勤.花岗岩地质和成矿关系.南京:江苏科学出版社,1986
[83]涂光炽.关于富碱侵入岩.矿产与地质,1989,13(3):1-4
[84]唐仁鲤,罗怀松.西藏玉龙斑岩铜(钼)矿带地质.北京:地质出版社,1993
[85]王强,赵振华,熊小林,等.底侵玄武质下地壳的熔融:来自安微沙溪埃达克(adakite)质富钠石英闪长玢岩的证据.地球化学,2001,30(4):353-362
[86]王强,赵振华,许继峰,等.鄂东南铜山口、殷祖埃达克质岩(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.岩石学报,2004,20(02)351-360
[87]王强,许继峰,王建新,等.大别山adakite型灰色片麻岩的确立及其与超高压变质作用的关系. 科学通报,2000,46(10):1017-1024
[88]王登红,陈毓川,徐珏,等.中国新生代的金属成矿作用的主要特点与成矿系列.中国地质学会:第31届国际地质大会中国代表团学术论文集.北京:地质出版社,2001
[89]王登红,屈文俊,李志伟,等.金沙江-红河成矿带斑岩铜钼矿的成矿集中期:Re-Os同位素定年.中国科学(D辑地球科学),2004,34(4):345-349
[90]杨建民,薛春纪,徐珏,等.滇西北喜马拉雅期富碱斑岩地质特征及其成矿作用.陈毓川.喜马拉雅期内生成矿作用研究.北京:地质出版社,2002
[91]李汉光,郭晓东,王绍明,等.云南宝兴厂金矿床地质特征及成因.矿床地质,2008,27(5):587-595
[92]王建、李建平、王江海,等.滇西剑川-大理地区新生代钾玄岩系中深源包体的地质意义,岩石学报,2002,22(2):113-124
[93]王义昭,李兴林,段丽兰,等.三江地区南段大地构造与成矿.北京:地质出版社,2000
[94]熊德信,孙晓明,石贵勇,等.云南哀牢山喜马拉雅期造山型金矿带矿床地球化学及成矿模式.北京:地质出版社,2007
[95]杨建琨,唐志国.云南省新生代浅成侵入斑岩型金矿成矿特征及找矿预测.北京地质,1996,3:27-31
[96]冶金工业部地质研究所.中国斑岩铜矿,北京:科学出版社,1984
[97]应汉龙.云南墨江镍金矿床富金石英脉的~(40)Ar/~(39)Ar快中子活化年龄.地质科学,2002,31(1):107-109
[98]应汉龙,蔡新平,刘秉光,等.云南墨江金矿成矿作用探讨.地质地球化学,2000,28(1):1-9
[99]应汉龙,蔡新平.云南北衙矿区富碱斑岩正长石和白云母的~(40)Ar-~(39)Ar年龄.地质科学,2004,39(1):107-110
[100]俞广钧.马厂箐金矿床成矿地质条件及其成因探讨.昆明工学院学报,1988,1:1-10
[101]云南省地质调查局.大理幅1:20万区域地质调查报告(地质部分),1973,1～150
[102]云南省地质调查局.大理县幅、下关市幅、凤仪镇幅1:5万区域地质调查报告.北京:地质出版社,1990
[103]云南省地质矿产局.大理幅1:20万水系沉积物测量地球化学图说明书.北京:地质出版社,1990
[104]云南省地质矿产局.云南省区域地质志.北京:地质出版社,1990
[105]张旗,王焰,钱青,等.中国东部中生代埃达克岩特征及其构造-成矿意义.岩石学报,2001,17(2):236-244
[106]张旗,李承东,王焰,等.中国东部中生代高Sr低Yb和低Sr高Yb型花岗岩对比及其地质意义,岩石学报,2005,21(6):1527-1529
[107]张旗,钱青,王二七,等.燕山中晚期的中画东部高原:埃达克岩的启示.地质科学,2001,36(2):248-255
[108]张旗,王焰,刘红涛,等.中国埃达克岩的时空分布及其形成背景.地学前缘,2003,10(4):385-400
[109]张旗,王焰,玉元龙,等.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约.岩石学报,2001,17(4):505-513
[110]张旗,桑克章,王元龙,等.加强埃达克岩研究,开创中国Cu、Au等找矿工作的新局面.岩石学报,2004,20(2):195-204
[111]张旗,许继峰,王焰,等.埃达克岩的多样性.地质通报,2004,23(9-10):959-965
[112]张旗,王焰,刘伟,等.埃达克岩的特征及其意义.地质通报,2002,21(7):431-435
[113]张旗,周德进,赵大升,等.滇西古特提斯造山带的威尔逊旋回:岩浆活动记录和深部过程讨论,岩石学报,1996,12(1):17-28
[114]张理刚.稳定同位素在地质科学中的应用.西安:陕西科学技术出版社,1985
[115]赵振华.稀土元素地球化学研究方法.地质地球化学,1982,1:65-66
[116]赵振化.微量元素地球化学原理.北京:科学出版社,1997
[117]赵振化,周玲棣.我国某些富碱侵入岩的稀土元素地球化学,中国科学(B),1994,24(10):1110-1113
[118]张海涛,杨家瑞.超基性岩蚀变热液型金矿床-云南金厂矿床成因探讨.云南地质,1984,3(4):311-325
[119]张玉泉.哀牢山-金沙江富碱侵入岩及其与裂谷构造关系初步研究,岩石学报.1987,1:17-25
[120]张玉泉,谢应雯,梁华英,等.藏东玉龙铜矿带含矿斑岩及成岩系列.地球化学,1998,27(3):236-243
[121]张玉泉,谢应雯.哀牢山-金沙江富碱侵入岩年代学和Nd,Sr同位素特征.中国科学(D 辑),1997,27(4):289-293
[122]张玉泉,谢应雯,邱华宁,等.钾玄岩系列:藏东玉龙铜矿带含矿斑岩sr,Nd,Pb同位素组成.地质科学,1998,33(3):359-366
[123]周玲棣,赵振华.我国富碱侵入岩的岩石学和岩石化学特征,中国科学(B辑).1994,24(10):1093-1095
[124]中国人民武装警察部队黄金第十三支队.云南省祥云县金厂箐岩金矿勘探报告.1993
[125]中国人民武装警察部队黄金第十支队.云南省大理州宝兴厂矿区人头箐矿段金矿普查报告.2007
[126]朱炳泉.地球科学中同位素体系理论与应用-兼论中国大陆壳幔演化.北京:科学出版社,1998
[127]朱创业,夏文杰,尹海生,等.兰坪-思茅中生代盆地性质及构造演化.成都理工学院学报,1997,24(4):23-30
[128]钟大赉.滇川西部古特提斯造山带.北京:科学出版社,1998
[129]钟立志,何毅特,李宗光,等.扬子地台西缘富碱斑岩铜金多金属成矿区划及成矿地质条件分析.西南矿产地质,1996,1-2
[130] Atheron, M. P. and Petford, N. Generation of sedium-rich magmas, 1993, 25
[131] Burnham C W and ohmoto H. Late-stage processes of feisic magmatism. In Ishihora S and Takenouchi S, (ed), Mining Geology Special Issue , 1980,8:1—11
[132] Burnham C W. Magma and hydrothermal fluidsA . In:Barnes HL ed. Geochemistry of hydrothermal ore deposits C. 2nd ed. New York :Wiley, 1979, 71—136
[133] Clayton R N,O' neil J R and Mayeda T K,Oxygen isotope exchange between quartz and water. Geophys. Res. 77.1972, 3057-3067
[134] Candela P A. Controls on ore metal ratios in grante-related oresystems:An experimental and computational approaeh. Transaetions of the Royal Soeiety of Edinburgh, Earth Seienees, 1992,83:317
[135] Cline J and Bodnar R J. Can economic porphyry copper mineralization be generated by a typical cale-alkaline melt?. Journal of Geophysical Research, 1991,96:8113-8126
[136] Cooke D R,Hollings P, and Walshe J L. .Giant Porphyry Deposits: Characteristics.dis tribution,and tectonic controls. Econ. Geol, 2005,100:801—818
[137] Defant M J, Drummond MS. Derivation of some modem arc magmas by reeking of young subducted lilhosphere. Nature, 1990, 347:662-665
[138] Dilles J H. Petrology of the yerington Batholith, Nevada:Evidence for evolution of porphyry copper ore fluids. Economic Geology,1987, 82:1750—1780
[139] Harris, N.B.W.Pearce.J. A. and Tindle .A. G. Geochemical Characteristics of collisionz one magmatism. In Collision Tectonic. ed. by Coaward.M.P.etal. Geol. Soc. Sp. publ, 1986,19:67-81
[140] Heinrich C A. The physical and chemical evolution of low-Salinity magmatic fluids at the porphyry to epithermal transition:a thermodynamic study.Mineralium Deposita, 2005,39:864-889
[141] Heinrich C A, Gunther D, Audetat A, Ulrich T and Frischknecht R. Metal fractionation between magmatic brine and vapor, determined by microanalysis of fluid inclusions. Geology, 1999,27:755-758
[142] Hedenquist J W, and Lowenst J B. The role of magmas in formation of hydrothermal ore deposits. Nature, 1994, 370:519-527
[143] Hollister V F, Potter R R, and Barker A L. Porphyry-tyoe deposits of the Appalachian orogen. Econ. Geol, 1974, 69:618—630
[144] Hollister V F, Potter R R, and Barker A L Porphyry-tyoe deposits of the Appalachian orogen. Econ. Geol, 1974,69:618-630
[145] Hou ZQ, Qu XM, Wang SX,et al. Re-Os age for molybdenites from the Gangdese porphyry copper belt in the Xizang (Tibetan) plateau: implication to mineralization duration and geodynamic settings. Science in China,2003,33:509—518
[146] Gustafson L B, and Hunt J P. The porphyry copper deposits at El Salvador, Chile[J]. Econ.Geol, 1975, 70:857-912
[147] Kay RW, Kay SM. Creation and destruction of lower continental crust. Geologische Rundsehau, 1991, 80:259～278
[148] Kay RW, Kay SM. Delamination and detanaination Tecconophyssics. 1993,219:177—189
[149] Kay R W. Aleutian magnesium andesites:melts from subducted Pacific oceanic crust. J. Volcanol. Geotherm. Res, 1978,4:117～132
[150] Le Maitre RW. A Classification of Igneous Rocks and Glossary of Terms. Blac-kwell. Oxford, 1989:193
[151] Lowell J D, Guibert J M. Lateral and vertical alteration-mineralization zoning in porphyry ore deposits. Econ Geal, 1974,65:373～408
[152] Middlemost E A K .Magmas and magmatic rocks.Longmas.London & New York. 1985:1—275
[153] Martin H. Smithies RH, RappR, MoyenJ-F, Champion D. An overview of adakite. lonalite-trondhjemite-granodiorite (TTG) , and sanukitoid: relationships and some implications for crustal evolution. Lilhos, 2005,79:1—24
[154] Muller D, Groves D I. Direct and indirect associations between potassic igneous rocks, shoshonites and gold-copper deposits. Ore Geology Reviews, 1993, 8:383～406
[155] Sillitoe R H. A plate tectonic model for the origin of porphyry capper deposits. Econ. Geol, 1972,67:184-197
[156] Muller D,StumpS E F, Taylor W R. Shoshonitic and alkaline lamprophyres with elevated Au and PGE concentrations from the Kreuzeck Mountains, Eastern Alps. Austria-Mineral PetrOl, 1992,46:23～42
[157] Martin H. Adakitic magmas:Modern analoguesof Archean granitoidsJ. Lithos, 1999, 46: 411 -429
[158] Mitchell A H G. Metallogenic belts and angle of dip of Benioff zones. Nature, 1973,245:49-52
[159] Ohmoto H. Systematics of sulfur and carbon isotopes in hydrothermal ore deposits. Econ Geol, 1972,67:551—579
[160] Ohmoto H, Rye R O. Isotope of Sulfur and Carbon. In:Geochemistry of Hydrothermal Ore Deposits, 2nd Edeition, John Wiley and Sons. New York, 1979:509—567
[161]Peccerillo R and Taylor S R. Geochemistry of eocene calc-alkaline volcanic rocKs from the Kastamonu area. Northern Turkey. Contrib. Mineral Petrol, 1976, 58(1): 63—81
[162]Petford N, Atherton MP, Halliday AN. Rapid magma production rates, Pitcher. W.S. Granite type and teconic environment.Mountain building processes, 1983:19—37
[163] Pitcher. W.S. Granite and yet more granites forty years on. Rundschau, 1987, 76(1) :51—79
[164]Rapp R P. Shimizu N Norman M D, Growth of early continental. crust by partial melting of eclogite. Nature, 2003, 425:605—609
[165] Redmond P B,Einaudi M T, Inan E E, Landtwing M R, and Heinrich C A. Copper deposition by fluid cooling in intrusion-centered systems:New insights from the Bingham porphyry ore deposit, Utah. Geology, 2004:217～230
[166]Rusk B G, Reed M H,Dilles J H,Klemm L M and Heinrich C A. Compositions of magmatic hydrothermal fluids determined by La-ICP-MS of fluid inclusion from the porphyry copper-molybdenum deposit at Butte, MT. Chemical Geology, 2004, 210:173—199
[167]Richards J P,Boyce A J and Pringle M S. Geologic evolution of the Escondida area, northern Chile: a model for spatial and temporal location of porphyry Cu mineralization. Econ. Geol, 2001, 96:271-306
[168]Richards,J P. Cumulative factors in the generation of giant cale-alkaline porphyry Cu deposits: In Porter T. M. (ed). Super-Porphyry Copper and Gold Deposits:A Global Perspective, PGC Publishng, Adelaide, pp, 2005:7—25
[169]Richard G, Monnereau M, Ingrin J. Is t he t ransition zone an empty water reservoir ? Inferences from numerical model of mantle dynamics. Earth and Planetary Science Letters, 2002, 205:37-51
[170] Richards J P. Tectono-magmatic precursors forporphyryCu-(Mo-Au) deposit formation. Economic Geology, 2003, 98:1515-1533
[171] Richards J P, McCulloch, M T, Chappell,B W, et al. Sourcesof metals in the Porgera gold deposit, PapuaNew Guinea: evidence from alteration, isotope, and noble metal geochemistry. Geochim et Cosmochim Acta, 1991, 55:565—580
[172]Richards J P. Alkalic-type epithermal gold deposits-a review. Mineralogical Association of Canada Short Course Series,1995,23:367—400
[173]Richards J P ang Kerrich R. Adakike-like rocks:Their diverse origins and questionable role in metallogenesis.Economic Geology, 2007, 102:537—576
[174]Sajona F G and Maury R C. Association of adakites with gold and copper mineralization in the Philippines. CR. Acad. Sci. Paris, 1998, 326(1):27—34
[175]Sillitoe R H. A plate tectonic model for the origin of porphyry copper deposits[J]. Econ. Geol., 1972,67:184-197
[176]Sillitoe R H. Geology of the Los Pelambres porphyry copper deposits,Chile. Econ. Geol, 1973,67:1-10
[177]Sillitoe R H. Andean mineralization:a model for the metallogeny of convergent plate margins. In Strong D F, (ed.), Metallogeny and Plate tectonis,Geol. Assoc. Can ada, special Paper, 1976,14:59—100
[178]Uyeda S, Kanamori H. Back-arc opening and the model of subduction. Jour Geophys Res, 1979,84:1040-1061
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |