青海三江北段斑岩钼铜矿床地质特征与成矿规律研究
|
摘要
近年来在青海南部开展的地质调查和研究工作揭示出三江北段成矿带具有形成大型、特大型金属矿床的赋存条件及地质背景,通过深入研究有望取得继三江中段之后的找矿重大突破。本文在系统收集前人研究成果基础上,通过对典型矿床(纳日贡玛、陆日格)开展野外地质调查和室内测试分析工作,基于成矿地质特征、岩石及矿床地球化学特征、同位素年代学等,对纳日贡玛、陆日格开展成矿地质背景、主要控矿因素、矿化规律、成矿模式等方面进行探讨,并与三江成矿带其它矿床进行对比。取得了如下研究成果和认识:
1、通过野外地质填图、钻孔编录和室内分析测试工作,详细地对陆日格、纳日贡玛斑岩型矿床的矿化类型、矿化特征、矿化元素及矿石学特征开展了大量基础性工作。确定了与青海三江北段Mo-Cu成矿作用有关的斑岩主要为黑云母花岗斑岩和浅色石英花岗斑岩,三江北段斑岩矿化以细脉浸染状、网脉状矿化为主;其矿化类型相对单一,主要为Mo、Cu矿化,伴生丰富的Bi、Te矿化,为进一步的找矿和勘探工作奠定了基础,明确了方向。
2、对陆日格、纳日贡玛矿床开展了斑岩锆石U-Pb同位素定年、辉钼矿Re-Os同位素定年工作。纳日贡玛含矿斑岩锆石LA ICP-MS U-Pb同位素测试结果为42.9 Ma～43.4Ma,陆日格矿床岩浆侵入年龄为61.7 Ma～62.1Ma;辉钼矿Re-Os同位素定年结果为纳日贡玛为40.5±0.87Ma,陆日格为60.7±1.5Ma。从而认为,纳日贡玛和陆日格为各自独立的两个岩浆-热液成矿过程。提出新生代以来青海三江段斑岩型矿床存在两次较大规模的岩浆成矿作用事件。
3、系统地对陆日格、纳日贡玛矿矿床开展了岩石学研究工作,并与三江成矿带其它矿床进行了对比。研究表明纳日贡玛、陆日格斑岩岩性主要为黑云母花岗斑岩、石英花岗斑岩及花岗闪长斑岩。岩石具有高SiO_2、富K_2O及Na_2O,wt(K_2O)>w(Na_2O),与邻近的玉龙矿带相似,斑岩主要为高钾钙碱性-钾玄岩系列。含矿斑岩稀土元素总量较高,稀土分配模式为轻稀土富集的右倾型,弱或无负Eu异常。微量元素表现为大离子亲石元素(LILE)富集、高场强(HFSE)亏损,具显著的Ti、Nb和Sr谷;具有部分埃达克岩的地球化学属性。
4、对陆日格、纳日贡玛含矿斑岩进行Sr-Nd-Pb同位素测试分析工作。三江北段斑岩钼铜矿带含矿斑岩的~(206)Pb/~(204)Pb值为18.4100～19.4290,~(207)Pb/~(204)Pb值为15.6090～15.6850,~(208)Pb/~(204)Pb值为38.5770～39.5228。含矿斑岩的(~(87)Sr/~(86)Sr)_t为0.702873～0.705859,(~(143)Nd/~(144)Nd)_t为0.512573～0.513204,ε_Nd(t)基本处于0.30～0.64,接近玉龙矿带的0.8～1.0Ga。青海三江段岩石Sr-Nd-Pb同位素非常接近EMll地幔端元,表明侵入岩主要来自交代富集地幔。
5、对纳日贡玛、陆日格开展了S、C-H-O同位素、包裹体等矿床地球化学研究,研究表明纳日贡玛硫化物δ~(34)S为4.0‰～7.1‰,陆日格矿石矿物δ~(34)S为-2.60‰～5.8‰。石英金属矿化物脉中H-O测试结果表明,成矿流体与石英达到平衡时,纳日贡玛成矿流体δ~(18)O_(H2O)为0.6‰～3.0‰,陆日格δ~(18)O_(H2O)为-0.76‰～3.54‰。随着深度的加强大,δ~(18)O_(H2O)逐渐变大和δD变小,成矿流体更偏向于岩浆水。成矿后期流体中的δ~13C的分布范围,也与岩浆/地幔源的δ~13C近似。因此,青海南部三江段斑岩矿床为成矿金属物质来源于岩浆,成矿流体为岩浆期后热液。
6、在综合研究基础上,提出了斑岩型矿床的成矿模型及找矿标志。并对区域青海南部三江段斑岩成矿规律进行了总结,认为青海南部三江成矿带的走滑断裂构造活动引起了区域内两期较大规模的成矿(分别以陆日格、纳日贡玛为代表)。对区域的找矿工作提出了建设性的意见和建议。
Recent studies on the Northern Sangjiang ore belt ,Southern Qinghai,reveal that the ore belt have excellent metallogenic conditions and geological background to form the Large, extra large metal deposits and expect to have breakthrough in prospecting after intensive work.By detailed field geological work and systemic modern analysis work ,this dessertation studies the geological Characteristics ,petrology,geochemistry and geochronology of the ore-bearing porphyries,such as Narigong and Lurige deposits.to research the dynamical backgroud,mineralization features and deposit model in Northern Sangjing ore belt and compare orther porphyies deposits in Sangjiang belt.The main conclusions were drawn as follows:
The Northern Sangjiang ore belt’s ore-bearing porphyries include Biotite monzogranite porphyry and Light-colored quartz monzonite porphyry.Ore stone show Veinlets- disseminated structure and mesh-vein texture.Mineralization is mainly Mo-Cu,and associted Bi,Te.
This paper carries out the porphyry zircon LA ICP-MS U-Pb isotope dating method and Molybdenite Re-Os isotope dating method, the first time for Lurige and detailed measurements for Narigongma .The rock-forming ages of Lurige range from 61.7Ma to 62.1Ma, and Narigongma deposit range from 42.9Ma to 43.4Ma.The Molybdeum mineralization age at Lugrge is 60.7±1.5Ma,and Narigongma is 40.5±0.8Ma.So Narigongma and Lurige porphyry deposits are two separate magmatic-hydrothermal ore forming process,and the span age of mineralization age and rock-forming age is about 2-3Ma. Therefore,since Cenozoic the Sanjiang porphyry deposits have two large-scale presence of magmatic mineralization events.
The element geochemical features in Northern SanJiang belt show adakite magmatic affinity ,similar to Yulong ore belt.The ore porphyries rocks are high SiO_2,k_2O and high k_2O/Na_2O ratio and mainly high-K calc-alkaline porphyry-shoshonitic series.The rocks are all enriched in large-ion lithophile elements(eg.K,Rb,Sr,Ba,Th,La)and light rare earthelements,depleted in high field-strength elements and heavy rare earth elements.
The ~(206)Pb/~(204)Pb,~(207)Pb/~(204)Pb,~(208)Pb/~(204)Pb values of Northern Sanjiang ore-bearing porphyries range from 18.4100～19.4290,15.6090～15.6850,38.5770～39.5228.The (~(87)Sr/~(86)Sr)_t,(~(143)Nd/~(144)Nd)_t values range from 0.702873～0.705859, 0.512573～0.513204, and the values ofεNd(t)is 0.30～0.64 Roughly.The Sr-Nd-Pb isotope of Northern Sanjiang ore belt,Southern Qinghai,were very close to Emll,so the intrusive rocks maybe come from the account of enriched mantle.
Theδ~(34)S value of Narigongma’sulfide was 4.0‰~7.1‰and Lurige was -2.60‰~5.8‰.Narigongmaδ~(18)O values of the Forming fluid which Ore-forming fluids and quartz Reach equilibrium was 0.6‰～3.0‰,and Lurige was -0.76‰～3.54‰.As the depth increased,δ~(18)O become larger andδD become smaller.Theδ~(13)C values of the dolomite are smilier with magma/mantle source.So the Ore-forming metals of Northern Sanjiang belt comes from magma and the ore-forming fluid comes from magmatic hydrothermal fluids.
Based on the comprehensive study,the thesis propose porphyries mineralization model and prospecting indications and summarize the metallogenic regularity .The two large-scale regional porphyries mineralization was coused by the conversion of Strike-slip fault tectonic stress in Northern Sanjiang belt ,Southern Qinghai.
1、通过野外地质填图、钻孔编录和室内分析测试工作,详细地对陆日格、纳日贡玛斑岩型矿床的矿化类型、矿化特征、矿化元素及矿石学特征开展了大量基础性工作。确定了与青海三江北段Mo-Cu成矿作用有关的斑岩主要为黑云母花岗斑岩和浅色石英花岗斑岩,三江北段斑岩矿化以细脉浸染状、网脉状矿化为主;其矿化类型相对单一,主要为Mo、Cu矿化,伴生丰富的Bi、Te矿化,为进一步的找矿和勘探工作奠定了基础,明确了方向。
2、对陆日格、纳日贡玛矿床开展了斑岩锆石U-Pb同位素定年、辉钼矿Re-Os同位素定年工作。纳日贡玛含矿斑岩锆石LA ICP-MS U-Pb同位素测试结果为42.9 Ma～43.4Ma,陆日格矿床岩浆侵入年龄为61.7 Ma～62.1Ma;辉钼矿Re-Os同位素定年结果为纳日贡玛为40.5±0.87Ma,陆日格为60.7±1.5Ma。从而认为,纳日贡玛和陆日格为各自独立的两个岩浆-热液成矿过程。提出新生代以来青海三江段斑岩型矿床存在两次较大规模的岩浆成矿作用事件。
3、系统地对陆日格、纳日贡玛矿矿床开展了岩石学研究工作,并与三江成矿带其它矿床进行了对比。研究表明纳日贡玛、陆日格斑岩岩性主要为黑云母花岗斑岩、石英花岗斑岩及花岗闪长斑岩。岩石具有高SiO_2、富K_2O及Na_2O,wt(K_2O)>w(Na_2O),与邻近的玉龙矿带相似,斑岩主要为高钾钙碱性-钾玄岩系列。含矿斑岩稀土元素总量较高,稀土分配模式为轻稀土富集的右倾型,弱或无负Eu异常。微量元素表现为大离子亲石元素(LILE)富集、高场强(HFSE)亏损,具显著的Ti、Nb和Sr谷;具有部分埃达克岩的地球化学属性。
4、对陆日格、纳日贡玛含矿斑岩进行Sr-Nd-Pb同位素测试分析工作。三江北段斑岩钼铜矿带含矿斑岩的~(206)Pb/~(204)Pb值为18.4100～19.4290,~(207)Pb/~(204)Pb值为15.6090～15.6850,~(208)Pb/~(204)Pb值为38.5770～39.5228。含矿斑岩的(~(87)Sr/~(86)Sr)_t为0.702873～0.705859,(~(143)Nd/~(144)Nd)_t为0.512573～0.513204,ε_Nd(t)基本处于0.30～0.64,接近玉龙矿带的0.8～1.0Ga。青海三江段岩石Sr-Nd-Pb同位素非常接近EMll地幔端元,表明侵入岩主要来自交代富集地幔。
5、对纳日贡玛、陆日格开展了S、C-H-O同位素、包裹体等矿床地球化学研究,研究表明纳日贡玛硫化物δ~(34)S为4.0‰～7.1‰,陆日格矿石矿物δ~(34)S为-2.60‰～5.8‰。石英金属矿化物脉中H-O测试结果表明,成矿流体与石英达到平衡时,纳日贡玛成矿流体δ~(18)O_(H2O)为0.6‰～3.0‰,陆日格δ~(18)O_(H2O)为-0.76‰～3.54‰。随着深度的加强大,δ~(18)O_(H2O)逐渐变大和δD变小,成矿流体更偏向于岩浆水。成矿后期流体中的δ~13C的分布范围,也与岩浆/地幔源的δ~13C近似。因此,青海南部三江段斑岩矿床为成矿金属物质来源于岩浆,成矿流体为岩浆期后热液。
6、在综合研究基础上,提出了斑岩型矿床的成矿模型及找矿标志。并对区域青海南部三江段斑岩成矿规律进行了总结,认为青海南部三江成矿带的走滑断裂构造活动引起了区域内两期较大规模的成矿(分别以陆日格、纳日贡玛为代表)。对区域的找矿工作提出了建设性的意见和建议。
Recent studies on the Northern Sangjiang ore belt ,Southern Qinghai,reveal that the ore belt have excellent metallogenic conditions and geological background to form the Large, extra large metal deposits and expect to have breakthrough in prospecting after intensive work.By detailed field geological work and systemic modern analysis work ,this dessertation studies the geological Characteristics ,petrology,geochemistry and geochronology of the ore-bearing porphyries,such as Narigong and Lurige deposits.to research the dynamical backgroud,mineralization features and deposit model in Northern Sangjing ore belt and compare orther porphyies deposits in Sangjiang belt.The main conclusions were drawn as follows:
The Northern Sangjiang ore belt’s ore-bearing porphyries include Biotite monzogranite porphyry and Light-colored quartz monzonite porphyry.Ore stone show Veinlets- disseminated structure and mesh-vein texture.Mineralization is mainly Mo-Cu,and associted Bi,Te.
This paper carries out the porphyry zircon LA ICP-MS U-Pb isotope dating method and Molybdenite Re-Os isotope dating method, the first time for Lurige and detailed measurements for Narigongma .The rock-forming ages of Lurige range from 61.7Ma to 62.1Ma, and Narigongma deposit range from 42.9Ma to 43.4Ma.The Molybdeum mineralization age at Lugrge is 60.7±1.5Ma,and Narigongma is 40.5±0.8Ma.So Narigongma and Lurige porphyry deposits are two separate magmatic-hydrothermal ore forming process,and the span age of mineralization age and rock-forming age is about 2-3Ma. Therefore,since Cenozoic the Sanjiang porphyry deposits have two large-scale presence of magmatic mineralization events.
The element geochemical features in Northern SanJiang belt show adakite magmatic affinity ,similar to Yulong ore belt.The ore porphyries rocks are high SiO_2,k_2O and high k_2O/Na_2O ratio and mainly high-K calc-alkaline porphyry-shoshonitic series.The rocks are all enriched in large-ion lithophile elements(eg.K,Rb,Sr,Ba,Th,La)and light rare earthelements,depleted in high field-strength elements and heavy rare earth elements.
The ~(206)Pb/~(204)Pb,~(207)Pb/~(204)Pb,~(208)Pb/~(204)Pb values of Northern Sanjiang ore-bearing porphyries range from 18.4100～19.4290,15.6090～15.6850,38.5770～39.5228.The (~(87)Sr/~(86)Sr)_t,(~(143)Nd/~(144)Nd)_t values range from 0.702873～0.705859, 0.512573～0.513204, and the values ofεNd(t)is 0.30～0.64 Roughly.The Sr-Nd-Pb isotope of Northern Sanjiang ore belt,Southern Qinghai,were very close to Emll,so the intrusive rocks maybe come from the account of enriched mantle.
Theδ~(34)S value of Narigongma’sulfide was 4.0‰~7.1‰and Lurige was -2.60‰~5.8‰.Narigongmaδ~(18)O values of the Forming fluid which Ore-forming fluids and quartz Reach equilibrium was 0.6‰～3.0‰,and Lurige was -0.76‰～3.54‰.As the depth increased,δ~(18)O become larger andδD become smaller.Theδ~(13)C values of the dolomite are smilier with magma/mantle source.So the Ore-forming metals of Northern Sanjiang belt comes from magma and the ore-forming fluid comes from magmatic hydrothermal fluids.
Based on the comprehensive study,the thesis propose porphyries mineralization model and prospecting indications and summarize the metallogenic regularity .The two large-scale regional porphyries mineralization was coused by the conversion of Strike-slip fault tectonic stress in Northern Sanjiang belt ,Southern Qinghai.
引文
1.莫宣学等,青藏高原新生代碰撞-后碰撞火成岩. 2009.10,北京:地质出版社.
2.侯增谦,王二七,莫宣学,丁林,潘桂棠,张中杰等,青藏高原碰撞造山与成矿作用. 2008,北京:地质出版社.
3.刘增乾,李兴振,叶庆同,罗建宁,沈敢富,杨岳清,三江地区构造岩浆带的划分与矿产分布规律. 1993,北京:地质出版社.
4.莫宣学,路凤香,沈上越等,三江特提斯火山作用与成矿. 1993,北京:地质出版社.
5.戴自希,矿产勘查百年. 2004,北京:地震出版社.
6. Lowell.J.D;Guilbert.J.M, Lateral and vertical alteration-mineralizationg zoning in porphyry ore deposites. Economic Geology, 1970. 65(373～408).
7. Sillitoe.R.H, A plate tectonic model for the origin of porphyty copper deposits Economic Geology, 1972. 67: p. 184～197.
8. 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. 44: p. 373～388.
9. Richard.J.P, Tectono-magmatic precursors for porphyry Cu-Mo-Au deposit formation. Economic Geology, 2003. 98: p. 1515～1533.
10.侯增谦,斑岩Cu-Mo-Au矿床:新认识与新进展.地学前缘, 2004. 11(1): p. 131～144.
11.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.岩石学报, 2004. 20(2): p. 229～238.
12. Cooke.D.R;Hollings.P;Walsh.J.L., Giant porphyry deposits :Characteristics , distribution , and tectonic controls. Economic Geology, 2005. 100(5): p. 801～818.
13.姚春亮,陆建军,郭维民,袁林,李伟,斑岩铜矿若干问题的最新研究进展.矿床地质, 2007. 26(2): p. 221～230.
14.芮宗瑶,张洪涛,陈仁义,王志良,王龙生,王义天,斑岩铜矿研究中若干问题探讨.矿床地质, 2006. 25(4): p. 491～500.
15.张旗,秦克章,王元龙,张福勤,刘红涛,王焰,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): p. 195～204.
16.罗晓玲,国内外铜矿资源分析.世界有色金属, 2000. 4: p. 4～10.
17. HouZQ,KamberBS,WeiRH,MengXJ, G., ibetan continental collision zones : evidence for slab melt metasomatism Adakite一like porPhyries from the southern. Contribution to Mineral Petrology, 2007. 153: p. 105～120.
18.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[矿床地质., 2006. 25(5): p. 521～543.
19.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.矿床地质, 2006. 25(6): p. 629～651.
20.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,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.矿床地质, 2006. 25(4): p. 337～357.
21.芮宗瑶,侯增谦,李光明,张立生,王龙生,唐索寒,俯冲、碰撞、深断裂和埃达克岩与斑岩铜矿.地质与勘探, 2006(1): p. 1～6.
22.夏斌,涂光炽,陈根文,喻享祥,超大型斑岩铜矿床形成的全球地质背景.矿物岩石地球化学通报, 2000. 19(4): p. 406～408.
23. Solomon.M, Subduction,arc reversal,and the origin of porphyry copper-gold deposits in island arcs. Geology, 1990. 18: p. 630～633.
24. James.D.E, S.I.S., Cenozoic formation of the Central Andes:a geophysical perspective. Skinner BJ Geology and ore deposits of the Central Andes. 1999: Spec Pub Soc Econ Geol
25.杨志明,西藏驱龙超大型斑岩铜矿床—岩浆作用与矿床成因. 2008,北京:中国地质科学院:博士论文.
26. Misra.K.C, Understanding mineral deposits. 2000: Kluwer Academic Publishers.
27.杨志明,侯增谦,杨竹林,王淑贤,王贵仁,田世洪,温德银,王召林,刘英超,青海纳日贡玛斑岩钼(铜)矿床:岩石成因衣构造控制.岩石学报, 2008. 24(3): p. 489～502.
28.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.岩石学报, 2004. 20(2): p. 239～248.
29. Kirkham.R.V, S.W.D., Porphyry copper,gold,molybdenum,tungsten,tin,silver. Geology of Canadian mineral deposits. 1995, Ottawa: Geological Survey of canada.
30. Audeta.A, P.T., Dolejs.D, Magmatic anhydrite and calcite in the ore-forming quartz-monzodiorite magma at Santa Rita.New Mexico(USA):Genetic constraints on porphyry Cu Mineralization Lithos, 2004. 72(324): p. 147～161.
31. Davidson.P, K.V., Cooke.D.R, Magmatic precursors of hydrothermal fluids at the Rio Blanco Cu-Mo deposit,Chile:Links to silicate magmas and metal transport. Economic Geology, 2005. 100(5): p. 963～978.
32.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.矿床地质, 2008. 27(3): p. 279～318.
33. Cline.J.S, B.R.J., Can economic porphyry copper mineralization be generated by a typical calc2alkaline melt. Journal of Geophysical Research Solid Earth and Planets, 1991. 96(B5): p. 8113~8126.
34. Burnham.CW, Magmas and hydrothermal fluids, in Geochemistry of Hydrothermal ore deposits Barnes.HL, Editor. 1979, Wiley: New York. p. 71~136.
35. Defant.MJ, D.M., Derivation of some modern arc magmas by melting of young subducted lithosphere Nature 1990. 34: p. 662～665.
36. Sajona.FG, M.R., Bellon.H,Cotten.J,Defant.MJ,Puvellier.M, Initiation of subduction and the generation of slab melts in western and eastern Mindanao,Philippines. Geology, 1993. 21(1007～1010).
37. Peacock.SM, R.T., Thompson.A, Partial melting of subducting oceanic crust. Earth planet sci letter, 1994. 121(224～227).
38. Martin.H, Adakitic magmas:Modern analogues of Archacan granitouds. Lithos, 1999. 46: p. 411～429.
39. Yogadzinski.GM, L.J., Churikova.TG,Dorendorf.F,Woeerner.G,Volynets.ON, Geochemical evidence for the melting of subducting oceanic lithosphere at plate edges. Nature, 2001. 409: p. 500～504.
40. Hildreth.W;Moorbath.S, Crustal contributions to arc magmatism in the Andes of central Chile. Contribution to Mineralogy and Petrology, 1988. 98(455～489).
41. Hedenquist.J.W, R.J.P., The influence of geochemical techniques on the development of genetic models for porphyry copper deposits. Reviews in Economic Geology, 1998. 10: p. 235～256.
42.李振清,杨志明,朱祥坤,侯增谦,李世珍,李志红,王跃,西藏驱龙斑岩铜矿铜同位素研究.地质学报, 2009. 83(12): p. 1985～1996.
43.张绮玲,曲晓明,徐文艺等,西藏南木斑岩铜矿床的流体包裹体研究.岩石学报, 2003. 19(2): p. 251～259.
44.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.地质通报, 2006. 25: p. 792～799.
45.肖波,李.李.秦.张.,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.岩石学报, 2007. 23(5): p. 935～952.
46.王登红等,西南三江地区新生代大陆动力学过程与大规模成矿. 2006.6,北京:地质出版社.
47.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.中国地质, 2001. 28(10): p. 27～30.
48.侯增谦,曲晓明,王淑贤,高永丰,杜安道,黄卫,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): p. 609～618.
49.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?.矿床地质, 2001. 20(4): p. 12.
50.侯增谦,潘小菲,杨志明,曲晓明,初论大陆环境斑岩铜矿.现代地质, 2007. 21(2): p. 332～-351.
51.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. 33(4): p. 412～425.
52.张玉泉,谢应雯,李献华,邱华宁,赵振华,梁华英,钟孙霖,青藏高原东部钾玄岩系岩浆岩同位素特征:岩石成因及其构造意义.中国科学D辑, 2000. 30(5): p. 493～499.
53. Hou Zengqian, Ma Hongwen, Khin Zaw, Zhang Yuquan, Wang Mingjie,Wang Zeng ,Pan Guitang, T.R., The Himalayan Yulong porphyry copper belt:produced by large-scale strike-slip faulting at Eastern Tibet Economic Geology, 2003. 98: p. 125～145.
54. Jiang.Yh;Jiang.Sy;Ling.Hf, Low-degree melting of a metasomatized lithospheric mantle for the origin of Cenozoic Yulong monzogranite-porphyty ,east Tibet :Geochemical and Sr-Nd-Pb-Hf isotopic constraints Earth and Planetary Science Letters, 2006. 241: p. 617～633.
55. Hou.ZQ;Gao.YF;Qu.XM;Rui.ZY;Mo.XX, origin of adakitic Intrusivesg generated during mid-Miocene east-west oxtension in southern Tibet. Earth and Planotary Science Letters, 2004. 220(139～155).
56.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.中国地质, 2006. 33(2): p. 340～351.
57.侯增谦,大陆碰撞成矿论.地质学报, 2010. 84(1): p. 30～58.
58.王登红;杨建民;闫升好;徐珏;陈毓川;薛春纪;骆耀;应汉龙;,西南三江新生代矿集区的分布格局及找矿前景. 23, 2002. 2: p. 6.
59.郭利果,刘玉平,徐伟,张兴春,秦克章,李铁胜,石玉若, SHRIMP锆石年代学对西藏玉龙斑岩铜矿成矿年龄的制约.岩石学报, 2006. 22(4): p. 1009～1016.
60.侯增谦,宋玉财,李政,等,青藏高原碰撞造山带Pb-Zn-Ag-Cu矿床新类型:成矿基本特征与构造控矿模型.矿床地质, 2008. 27(2): p. 123—144.
61.唐仁鲤,罗怀松,西藏玉龙斑岩铜(钼)矿带地质.北京:中国地质大学出版社, 1995. 320.
62.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. 83(12): p. 1887-1900.
63.陈建平,王功文,侯昌波,唐菊兴,基于GIS技术的西南三江北段矿产资源定量预测与评价.矿产地质, 2005. 24(4): p. 15-24.
64.邓军,侯增谦,莫宣学,杨立强,王庆飞,王长明,三江特提斯复合造山与成矿作用.矿床地质, 2010. 29(1): p. 37～42.
65. Spurlin.MS , Yin.A , Horton.BK , Zhou.JY , Wang.JH, Structural evolution of the Yushu-Nanggaian region and its relationship to syncollisional igneous activity,east-central Tibet. GSA bulletin, 2005. 117: p. 1293～1317.
66.郝金华,陈建平,董庆吉,王涛,罗志忠,青海三江北段陆日格含矿斑岩地球化学特征及其地质意义.岩石矿物地球化学通报, 2010. 29(4): p. 328～339.
67.郝金华,陈建平,田永革,李玉龙,尹京武,青海纳日贡玛斑岩钼(铜)矿含矿斑岩矿物学特征及成岩成矿意义.地质与勘探, 2010. 46(3): p. 367～376.
68.曲晓明,侯增谦,李佑国, S、Pb同位素对冈底斯斑岩铜矿带成矿物质来源和造山带物质循环的批示.地质通报, 2002.12. 21(11): p. 9.
69. Wang.JH,Yin.A,Harrison.TM, A tectonic model for Cenozoic igneous activites in the eastern Indo-Asian collison zone. Earth Planet Sci Lett, 2001. 199: p. 123～133.
70.周江羽,王江海,尹安,Spurlin.MS,Horton.BK,青藏东北缘早第三纪盆地充填的沉积型式及构造背景——以囊谦和下拉秀盆地为例.沉积学报, 2002. 20(01): p. 85～91.
71.刘英超,杨竹森,侯增谦,田世洪,王召林,宋玉财,薛万文,鲁海峰,王富春,张玉宝,朱田,俞长捷,苏嫒娜,李真真,于玉帅,青海玉树东莫扎抓铅锌矿床地质特征及碳氢氧同位素地球化学研究.矿床地质, 2009. 28(6): p. 770～784.
72.田世洪,杨竹森,侯增谦,刘英超,高延光,王召林,宋玉财,薛万文,鲁海峰,王富春,苏嫒娜,李真真,王银喜,张玉宝,朱田,俞长捷,于玉帅,玉树地区东莫扎抓和莫海拉亨铅锌矿床Rb-Sr和Sm-Nd等时线年龄及其地质意义.矿床地质, 2009. 28(6): p. 747～758.
73.陈建平,唐菊兴,陈勇,李葆华,尚北川,西南三江北段纳日贡玛铜钼矿床地质特征与成矿模式.现代地质, 2008. 22(1): p. 9～18.
74.宋忠宝,贾群子,陈向阳,陈博,张雨莲,张晓飞,全守村,栗亚芝,三江北段纳日贡玛花岗闪长斑岩成岩时代的确定及地质意义.地球学报, 2011. 32(2): p. 154～162.
75.潘桂棠,李兴振,王立全,丁俊,陈智粱,青藏高原及邻区大地构造单元初步划分. 2002. 21(11): p. 701～707.
76.潘桂棠,肖庆辉,陆松年,邓晋福,冯益民,张克信,张智勇,王方国,邢光福,郝国杰,冯艳芳,中国大地构造单元划分.中国地质, 2009. 36(1): p. 1～28.
77.鲁海峰,薛万文,王贵仁,纳日贡玛铜钼矿床地质特征及成因类型探讨.青海国土经略, 2006(3): p. 37～40.
78.青海地质调查院,中华人民共和国区域地质调查报告(1:25万)治多幅. 2006,西宁.
79. HanYg,ZhangSh,Franco,ZhangYh, Evolution of the Mesozoic Granites in the Xiong’ershan-Waifangshan Region,Western Henan Province,China,and Its Tectonic Implications. Acta Geologica Sinica, 2007. 81(2): p. 253～265.
80.迟清华,鄢明才,应用地球化学元素丰度数据手册. 2007,北京:地质出版社.
81.邱家骧,应用岩浆岩岩石学. 1991,北京:中国地质大学出版社.
82.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.矿床地质, 2003. 22(1): p. 12.
83.孟祥金,西藏碰撞造山带冈底斯中新世斑岩铜矿成矿作用研究. 2004,北京:中国地质科学院:博士论文.
84.何学贤,唐索寒,朱祥坤,多接收器等离子体质谱(MC-ICPMS)高精度测定Nd同位素方法.地球学报, 2007. 26:: p. 19～22.
85.黄萱,山西省花岗岩类的Nd和Sr同位素组成及构造演化意义[岩石学报, 1990. 6: p. 1～11.
86. Andersen.T, Correct ion of common Pb in U-Pb analyses that do not report 204 Pb. Chem Geol 2002. 192: p. 59～79.
87. Ludwig.KR.M;Berkely, Isoplot/Ex version 3.00. A Geochronological Toolkit for Microsoft Excel[2003, Berkeley Geochronology Center Special Publication. p. 1～70.
88.胡培远,李才,苏犁,李春斌,于红,青藏高原羌塘中部蜈蚣山花岗片麻岩锆石U-Pb定年—泛非与印支事件的年代学记录.中国地质, 2010. 37(4): p. 1050～1061.
89. Claesson.S,Vetrin.V,Bayanova.T, U-Pb zircon ages from a Devonian carbonatite dyke, Kola Peninsula, Russia: a record of geological evolution from the Archean to the Paleozoic : . Lithos, 2000. 51: p. 95～108.
90. Hoskin.P,Black.LP, Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon. Journal of Metamorphic Geology, 2000. 18: p. 423～439.
91.姜耀辉,蒋少涌,凌洪飞,戴宝章,陆-陆碰撞靠山环境下含铜斑岩岩石成因-以藏东玉龙斑岩铜矿带为例.岩石学报, 2006. 22(3): p. 697～706.
92.邓万明,孙宏娟,张玉泉,囊谦盆地新生代钾质火山岩成因岩石学研究.地质科学, 2001. 36(3): p. 304～318.
93. Whalen JB, C.B., Opaque mineralogy and mafic mineral chemistry of I-ad S-type granites of Lachlan fold belt,southeast Australia. American Mineralogist, 1988. 73(3): p. 281～296.
94.徐克勤,孙鼐,王德滋,刘昌实,陈克荣,华南两类不同成因花岗岩岩石学特征.岩石矿物及测试, 1982. 1(2): p. 1～12.
95. Clemens JD, W.V., Origin and evolution of a peralum ignous silicic ignimbrite suite:the violet town volcanics. Contrib Mineral Petrol, 1984. 88: p. 354～371.
96. White AJR, C.B., Granitoid types and their dirtribution in the Lachlan Fold Belt,southeastern Australia. Mem.Geol Soc Am, 1983. 159(21～34).
97.丁孝石,西藏中南部各类花岗岩中黑云母标型特征及其地质意义.中国地质科学院矿床地质研究所所刊, 1988. 1: p. 33～50.
98. Miller,SchusterR,KlotzliU,Frank,Purtscheller, Post-collisonal notassic and ultranotassic magmatism in SW Tibet:geochemical and Sr-Nd-Pb-O isotonic constraints for mantle source characteristics and netrogenesis. Petrol, 1999. 1999(40): p. 1339～1424.
99. WangJH,YinA,Harrison, A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collison zone Earth Planet., 2001. 199: p. 123～133.
100. Qu.Xm;Hou.Zq;Khin.Z;Li.Yg, Characteristics and genesis of Gangdese porhyry copper deposits in the south-and geochronological results. ore Geology Review, 2007. 31(205～223).
101.迟效国,李才,金巍,藏北羌塘地区新生代火山作用与岩石圈构造演化.中国科学(D辑), 2005. 35(5): p. 399~410.
102.马鸿文,西藏玉龙斑岩铜矿带花岗岩类与成矿.北京:中国地质大学出版社. 1990. 157.
103.李亚林,王成善,伊海生,刘志飞,李勇,西藏北部新生代大型逆冲推覆构造与唐古拉山的隆起.地质学报, 2006. 80(8): p. 1118～1131.
104. Ohmoto, C.B.H., Late-stage processes of felsic magmatism,In Ishihora S and Takenouchi S. Mining Geology Special Issue, 1980. 8: p. 1～11.
105. Takahashi M, A.S., Ishihara S, Magnetite-series/ilmenite-series vs I-type/S-type granitoids Mining Geology Special Issue, 1980. 8(13～28).
106.吕伯西,王增,张能德,段建中,高子英,沈敢富,潘长云,姚鹏,三江地区花岗岩类及其成矿专属性.中华人民共和国地质矿产部地质专报三岩石矿物地球化学第18号. 1993:地质出版社. 337.
107.秦克章,张连昌,丁奎首,许英霞,唐冬梅,徐兴旺,马天林,李光明,东天山三岔口铜矿床类型、赋矿岩石成因与矿床矿物学特征.岩石学报, 2009. 25(4): p. 845～861.
108.王召林,杨志明,杨竹森,田世洪,刘英超,马彦青,王贵仁,屈文俊,纳日贡玛斑岩钼铜矿床:玉龙铜矿带的北延-来自辉钼矿Re-Os同位素年龄的证据.岩石学报, 2008. 24(3): p. 503～510.
109. Ohmoto.H, Systematic of sulfur and carbon isotopes in hydrothermal ore deposits. Economic Geology, 1972. 67: p. 551～579.
110. Ohmoto.H, R.R.O., Isotopes of sulfur and carbon. Geochemistry of Hydrothermal ore deposits, ed. Barnes.HL. 1979, Now York: Wiley interscience. 509～567.
111.魏菊英,王关玉,同位素地球化学. 1988,北京:地质出版社.
112.黄朋,顾雪祥,唐菊兴,王立全,西藏玉龙斑岩铜(钼)矿床物质来源研究.大地构造与成矿学, 2002. 26(4): p. 429～435.
113.唐菊兴,西藏玉龙斑岩铜(钼)矿成矿作用与矿床定位预测研究. 2003,成都:成都理工大学:博士论文.
114. Harris.AC,Golding.SD,White.NC, Bajo de la Alumbrera copper-gold deposit:Stable isotope evidence for a porphyry-relater hydrothermal system dominated by magmatic aqueous fluids. Economic Geology, 2005. 100: p. 863～886.
115. Sillitoe.R.H, Porphyry Copper Systems. Economic Geology, 2010. 105: p. 3～41.
116.刘慧卿,李保华,唐菊兴,董树义,纳日贡玛铜钼矿床中流熔包裹体的发现及其意义.物探化探计算技术, 2007. 29(6): p. 534-536.
117. Gammons.CH, W.A., Chemical mobility of gold in the pophyry-epithermal environment. Economic Geology, 1997. 92(1): p. 45～59.
118.杨志明,侯增谦,夏代祥,宋玉财,李政,西藏驱龙铜矿西部斑岩与成矿关系的厘定:对矿床未来勘探方向的重要启示.矿床地质, 2008. 27: p. 28 -36.
119. Liang.HY,Campbell.IH, Allen.C, e.a., Ce4+/ce3+ ratios and ages for Yulong ore-bearing porhyries in eastern Tibet Mineralium Deposita, 2006. 41: p. 152～159.
120. Jugo.PJ, L.R., Richards.JP, Experimental determination of sulfur solubility in basaltic melts at sulfide vs.sulfate saturation:Possibale implications for ore formation in Eos,Transactions,AGU (2001 Fall Meeting Supplement ,Abstract V32G-05). 2001.
121. Hamlyn.PR;Keays.RR;Cameron.WE;Crawford.AJ;Waldron.HM, Precious metals in magnesian low-Tilavas:implications for metallogenesis and sulfur saturation in primary magmas Geochimica et Cosmochimica ACTA, 1985. 49(1797～1811).
122. Bornhorst.TJ;Rose.WI, Partitionging of gold in young calc-alkaline volcanic rocks form Guatemala Journal of Geology, 1986. 94(412～418).
123. Richards.JP, Alkalic-type epithermal gold deposits a review Mineralogical Association of Canada short course series 1995. 23: p. 367～400.
124.金章东,李福春,斑岩型铜矿床成矿过程中铜的迁移与沉淀机制研究新进展.矿产与地质, 1998. 12(64): p. 73～78.
125.南征兵,唐菊兴,李葆华,纳日贡玛斑岩铜钼矿成矿元素沉淀机制探讨.矿业研究与开发, 2007. 28(2): p. 1～3.
126. Agterberg FQ, B.C., Logistic regression and weights of evidence modeling in mineral exploration. Proc 28th Intern Symp Computer Applications in the Mineral Industries 1999: p. 483-490.
127.张玉泉,谢应雯,邱华宁,李献华,钟孙霖,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): p. 359～366.
128.朱训,德兴斑岩铜矿. 1983,北京:地质出版社.
129.丁林,张进江,周勇,邓万明,许荣华,钟大赉,青藏高原岩石圈演化的记录:藏北超钾质及钠质火山岩的岩石学与地球化学特征[J].岩石学报, 1999. 015(03): p. 408～421.
130.赖绍聪,青藏高原北部新生代火山岩的成因机制.岩石学报, 1999. 15(4): p. 98～104.
131.姜耀辉,蒋少涌,戴宝章,凌洪飞,玉龙斑岩铜矿含矿与非含矿斑岩元素和同位素地球化学对比研究.岩石学报, 2006. 22(10): p. 2561～2566.
132.莫宣学,赵志丹,邓晋福,董国臣,周肃,郭铁鹰,张双全,王亮亮;,印度—亚洲大陆主碰撞过程的火山作用响应.地学前缘, 2003. 10(3): p. 135～148.
133.王召林,侯增谦,杨竹森,田世洪,刘英超,杨志明,宋玉财,青海杂多地区新生代构造特征与两种类型矿床的关系.矿产地质, 2009. 28(2): p. 157～69.
134.许志琴,杨经绥,李海兵,嵇少丞,张泽明,刘焰,印度-亚洲碰撞大地构造.地质学报, 2011. 85(1): p. 1～32.
135.徐平,矿物成分的电子探针作图及其在矿物学研究中的应用.岩石学报, 1998. 14(3).
136.朱永峰,新一代电子探针是解决一些地球科学问题的好工具.地学前缘, 2003. 10(2): p. 435～436.
137.李雪梅,杜金菊,赵.胡.廖.江.,电子探针中的Map图在矿物出溶体中的应用.中山大学学报(自然科学版), 2004. 43(5): p. 95～97.
138.张文兰,王汝成,陈小明,赖明远,电子探针面分析与相分析技术及其应用.电子显微学报, 1999. 18(6): p. 630～639.
139.陈毓川,毛景文,骆耀南,魏家秀等,四川大水沟碲金矿床地质和地球化学. 1996:原子能出版社. 146.
140.银剑钊,世界首例独立碲矿床的成矿机理及成矿模式. 1996,重庆:重庆出版社. 190.
141.骆耀南,曹志敏,四川省发现世界首例独立碲矿床.中国地质, 1994(2): p. 27～28.
142.毛景文,陈毓川,杨百川,雷蕴芬,周剑雄,四川省石棉县大水沟碲矿床中的辉碲铋矿研究.地质科学, 1995. 30(1): p. 47～51.
143.邱士东,王葆华,徐九化,谢玉玲,因硫碲铋矿在中国的首次发现.矿物学报, 2008. 28(4): p. 357～359.
144.赵玉山,金成洙,关广岳,辽宁舞龙金矿铋矿物与金矿化关系研究.矿物学报, 1994. 14(1): p. 88～91.
145.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. 28(5): p. 515～538.
146. Shirey.SB,Walker.RJ, Carius tube digestion for low-blank Rhenium-Osmium analysis. Anal Chem, 1995. 67: p. 2136～2141.
147.杜安道,赵敦敏,王淑贤, 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): p. 247～252.
148.高一鸣,陈毓川,唐菊兴,西藏沙让斑岩钼矿床锆石SHRIMP定年和角闪石Ar-Ar定年及其地质意义矿床地质, 2010. 29(2): p. 323～331.
149.杨宗喜;毛景文;陈懋弘;童祥;武俊德;程彦博;赵海杰,云南个旧卡房矽卡岩型铜锡矿Re-Os年龄及其地质意义.岩石学报, 2008. 24(8): p. 1937～1944.
150.唐菊兴,王成辉,屈文俊,杜安道,应立娟,高一鸣,西藏玉龙斑岩铜钼矿辉钼矿铼-锇同位素定年及其成矿学意义.岩矿测试, 2009. 28(3): p. 215～218.
151.杜安道,何红蓼,殷宁万,邹晓秋,孙亚利,孙德忠,陈少珍,屈文俊,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): p. 339～347.
152.王登红,屈文俊,李志伟,应汉龙,陈毓川,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), 2004. 34(4): p. 345～349.
153.邢俊兵,郭晓东,屈文俊,王治华,李汉光,马厂箐斑岩型铜、钼矿辉钼矿Re黄金科学技术, 2009. 17(5): p. 24～29.
154. Luo.JL, C.Y., Wang.DH, Chronagenesis of endogenetic mineralization on the east side of the Qinghai-XiZang plateau Acta Geologica Sinica, 2000. 74(3): p. 447～451.
155. Wang.DH, C.Y., Xu.J,Yang.JM.Xue.CJ,Yan.SH, Cenozoic mieralization in China,as a key to past mineralization and a clue to future prospecting. Acta Geologica Sinica, 2000. 74(3): p. 478～484.
156. Camus.F;Dines.JH, A special issue devoted to porphyry copper deposits of northern Chile-perface. Economic Geology, 2001. 96: p. 233～238.
157. Kay.RWJ, Aleutian magnesium andesites:melts from subducted Pacific oceanic crust. jour Volcan Geotherm Res, 1978. 4(117～132).
158. Stern.CR;Kilian.R, Role of the suvducted slab,mantle wedge and continental crust in the generation of adakites from the Andean arutral volcanic zone Contrib Mineral Petrol, 1996. 123(263～281).
159.赵志丹;莫宣学;董国臣;周肃;朱弟成;廖忠礼;孙晨光,青藏高原Pb同位素地球化学及其意义.现代地质, 2007.6. 21(2): p. 265～274.
160.郝金华,陈建平,董庆吉,李玉龙,王涛,马继义,青海三江北段斑岩钼铜矿带含矿斑岩地球化学、Sr-Nd-Pb同位素特征及地质意义.岩石矿物学杂志, 2011. 30(3): p. 515～525.
161.莫宣学,青藏高原岩浆岩成因研究:成果与展望.地质通报, 2009.12. 28(12): p. 1693～1702.
162.莫宣学,青藏高原地质研究的回顾与展望.中国地质, 2010.8. 37(4): p. 841～853.
163.莫宣学,赵志丹,朱弟成,喻学惠,董国臣,周肃.,西藏南部印度—亚洲碰撞带岩石圈:岩石学-地球化学约束.地球科学(中国地质大学学报, 2009. 34(1): p. 17～27.
164. Dewey.JF; Shackleton.RM; Chang.C, e., The tectonic evolution of the Tibetan Plateau. 1988, London: Philosophical Transation of rhe Royal Society
165. Wang.JH;Yin.A;Harrison.TM;Grove.M, A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collision Zone. Earth and Planetary Science Letters, 2001. 88: p. 123～133.
166.董庆吉,西南三江北段区域成矿定量预测与评价. 2009,中国地质大学(北京):北京.
167.王治华,郭晓东,喻万强,邹依林,徐涛,张勇,云南省马厂箐铜钼金多金属矿床地质特征及成矿规律.地质与勘探, 2010. 46(2): p. 214～223.
168.王治华,郭晓东,陈祥,葛良胜,邹依林,云南祥云马厂箐富碱斑岩体的地球化学特征及其形成的构造环境.地质论评, 2010. 56(1): p. 125～135.
169.郭晓东,王治华,陈祥,王欣,王淑贤,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. 83(12): p. 1901～1915.
170.邢俊兵,郭晓东,屈文俊,王治华,李汉光,马厂箐斑岩型铜、钼矿辉钼矿Re-Os年龄及地质意义.黄金科学技术, 2009. 17(5): p. 24～29.
171.梁华英,谢应雯,张玉泉,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(116～120).
172.黄波,梁华英,莫济海,谢应雯,金平铜厂铜钼矿床赋矿岩体锆石LA-ICP-MS U-Pb年龄及意义.大地构造与成矿学, 2009. 33(4): p. 598～602.
173.应汉龙,刘和林,杨许中,李志伟,云南金平铜厂金矿床地质特征和成矿物质来源.地质与资源, 2006. 15(4): p. 265～272.
174.祝向平,云南哈播斑岩型铜(钼金)矿床地质特征与成矿作用研究. 2010,中国地质大学(北京):北京.
175. Leloup.PH;Arnaud.N;Lacassin.R;Kienast.JR;Harrison.TM;Trong.TTP;Replunaz.A;Tapponnier.P, New constraints on the structure,thermochronology,and timing of the Ailao Shan-Red river shear zone,SE Asia. Journal of Geophysical Research, 2001. 106: p. 6683～6732.
176. Yin.A,Harrison.Tm, Geologic evolutin of the Himalayan-Tibetan orogen. Earth Planet sci, 2000. 28: p. 211～280.
2.侯增谦,王二七,莫宣学,丁林,潘桂棠,张中杰等,青藏高原碰撞造山与成矿作用. 2008,北京:地质出版社.
3.刘增乾,李兴振,叶庆同,罗建宁,沈敢富,杨岳清,三江地区构造岩浆带的划分与矿产分布规律. 1993,北京:地质出版社.
4.莫宣学,路凤香,沈上越等,三江特提斯火山作用与成矿. 1993,北京:地质出版社.
5.戴自希,矿产勘查百年. 2004,北京:地震出版社.
6. Lowell.J.D;Guilbert.J.M, Lateral and vertical alteration-mineralizationg zoning in porphyry ore deposites. Economic Geology, 1970. 65(373～408).
7. Sillitoe.R.H, A plate tectonic model for the origin of porphyty copper deposits Economic Geology, 1972. 67: p. 184～197.
8. 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. 44: p. 373～388.
9. Richard.J.P, Tectono-magmatic precursors for porphyry Cu-Mo-Au deposit formation. Economic Geology, 2003. 98: p. 1515～1533.
10.侯增谦,斑岩Cu-Mo-Au矿床:新认识与新进展.地学前缘, 2004. 11(1): p. 131～144.
11.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.岩石学报, 2004. 20(2): p. 229～238.
12. Cooke.D.R;Hollings.P;Walsh.J.L., Giant porphyry deposits :Characteristics , distribution , and tectonic controls. Economic Geology, 2005. 100(5): p. 801～818.
13.姚春亮,陆建军,郭维民,袁林,李伟,斑岩铜矿若干问题的最新研究进展.矿床地质, 2007. 26(2): p. 221～230.
14.芮宗瑶,张洪涛,陈仁义,王志良,王龙生,王义天,斑岩铜矿研究中若干问题探讨.矿床地质, 2006. 25(4): p. 491～500.
15.张旗,秦克章,王元龙,张福勤,刘红涛,王焰,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): p. 195～204.
16.罗晓玲,国内外铜矿资源分析.世界有色金属, 2000. 4: p. 4～10.
17. HouZQ,KamberBS,WeiRH,MengXJ, G., ibetan continental collision zones : evidence for slab melt metasomatism Adakite一like porPhyries from the southern. Contribution to Mineral Petrology, 2007. 153: p. 105～120.
18.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[矿床地质., 2006. 25(5): p. 521～543.
19.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.矿床地质, 2006. 25(6): p. 629～651.
20.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,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.矿床地质, 2006. 25(4): p. 337～357.
21.芮宗瑶,侯增谦,李光明,张立生,王龙生,唐索寒,俯冲、碰撞、深断裂和埃达克岩与斑岩铜矿.地质与勘探, 2006(1): p. 1～6.
22.夏斌,涂光炽,陈根文,喻享祥,超大型斑岩铜矿床形成的全球地质背景.矿物岩石地球化学通报, 2000. 19(4): p. 406～408.
23. Solomon.M, Subduction,arc reversal,and the origin of porphyry copper-gold deposits in island arcs. Geology, 1990. 18: p. 630～633.
24. James.D.E, S.I.S., Cenozoic formation of the Central Andes:a geophysical perspective. Skinner BJ Geology and ore deposits of the Central Andes. 1999: Spec Pub Soc Econ Geol
25.杨志明,西藏驱龙超大型斑岩铜矿床—岩浆作用与矿床成因. 2008,北京:中国地质科学院:博士论文.
26. Misra.K.C, Understanding mineral deposits. 2000: Kluwer Academic Publishers.
27.杨志明,侯增谦,杨竹林,王淑贤,王贵仁,田世洪,温德银,王召林,刘英超,青海纳日贡玛斑岩钼(铜)矿床:岩石成因衣构造控制.岩石学报, 2008. 24(3): p. 489～502.
28.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.岩石学报, 2004. 20(2): p. 239～248.
29. Kirkham.R.V, S.W.D., Porphyry copper,gold,molybdenum,tungsten,tin,silver. Geology of Canadian mineral deposits. 1995, Ottawa: Geological Survey of canada.
30. Audeta.A, P.T., Dolejs.D, Magmatic anhydrite and calcite in the ore-forming quartz-monzodiorite magma at Santa Rita.New Mexico(USA):Genetic constraints on porphyry Cu Mineralization Lithos, 2004. 72(324): p. 147～161.
31. Davidson.P, K.V., Cooke.D.R, Magmatic precursors of hydrothermal fluids at the Rio Blanco Cu-Mo deposit,Chile:Links to silicate magmas and metal transport. Economic Geology, 2005. 100(5): p. 963～978.
32.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.矿床地质, 2008. 27(3): p. 279～318.
33. Cline.J.S, B.R.J., Can economic porphyry copper mineralization be generated by a typical calc2alkaline melt. Journal of Geophysical Research Solid Earth and Planets, 1991. 96(B5): p. 8113~8126.
34. Burnham.CW, Magmas and hydrothermal fluids, in Geochemistry of Hydrothermal ore deposits Barnes.HL, Editor. 1979, Wiley: New York. p. 71~136.
35. Defant.MJ, D.M., Derivation of some modern arc magmas by melting of young subducted lithosphere Nature 1990. 34: p. 662～665.
36. Sajona.FG, M.R., Bellon.H,Cotten.J,Defant.MJ,Puvellier.M, Initiation of subduction and the generation of slab melts in western and eastern Mindanao,Philippines. Geology, 1993. 21(1007～1010).
37. Peacock.SM, R.T., Thompson.A, Partial melting of subducting oceanic crust. Earth planet sci letter, 1994. 121(224～227).
38. Martin.H, Adakitic magmas:Modern analogues of Archacan granitouds. Lithos, 1999. 46: p. 411～429.
39. Yogadzinski.GM, L.J., Churikova.TG,Dorendorf.F,Woeerner.G,Volynets.ON, Geochemical evidence for the melting of subducting oceanic lithosphere at plate edges. Nature, 2001. 409: p. 500～504.
40. Hildreth.W;Moorbath.S, Crustal contributions to arc magmatism in the Andes of central Chile. Contribution to Mineralogy and Petrology, 1988. 98(455～489).
41. Hedenquist.J.W, R.J.P., The influence of geochemical techniques on the development of genetic models for porphyry copper deposits. Reviews in Economic Geology, 1998. 10: p. 235～256.
42.李振清,杨志明,朱祥坤,侯增谦,李世珍,李志红,王跃,西藏驱龙斑岩铜矿铜同位素研究.地质学报, 2009. 83(12): p. 1985～1996.
43.张绮玲,曲晓明,徐文艺等,西藏南木斑岩铜矿床的流体包裹体研究.岩石学报, 2003. 19(2): p. 251～259.
44.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.地质通报, 2006. 25: p. 792～799.
45.肖波,李.李.秦.张.,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.岩石学报, 2007. 23(5): p. 935～952.
46.王登红等,西南三江地区新生代大陆动力学过程与大规模成矿. 2006.6,北京:地质出版社.
47.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.中国地质, 2001. 28(10): p. 27～30.
48.侯增谦,曲晓明,王淑贤,高永丰,杜安道,黄卫,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): p. 609～618.
49.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?.矿床地质, 2001. 20(4): p. 12.
50.侯增谦,潘小菲,杨志明,曲晓明,初论大陆环境斑岩铜矿.现代地质, 2007. 21(2): p. 332～-351.
51.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. 33(4): p. 412～425.
52.张玉泉,谢应雯,李献华,邱华宁,赵振华,梁华英,钟孙霖,青藏高原东部钾玄岩系岩浆岩同位素特征:岩石成因及其构造意义.中国科学D辑, 2000. 30(5): p. 493～499.
53. Hou Zengqian, Ma Hongwen, Khin Zaw, Zhang Yuquan, Wang Mingjie,Wang Zeng ,Pan Guitang, T.R., The Himalayan Yulong porphyry copper belt:produced by large-scale strike-slip faulting at Eastern Tibet Economic Geology, 2003. 98: p. 125～145.
54. Jiang.Yh;Jiang.Sy;Ling.Hf, Low-degree melting of a metasomatized lithospheric mantle for the origin of Cenozoic Yulong monzogranite-porphyty ,east Tibet :Geochemical and Sr-Nd-Pb-Hf isotopic constraints Earth and Planetary Science Letters, 2006. 241: p. 617～633.
55. Hou.ZQ;Gao.YF;Qu.XM;Rui.ZY;Mo.XX, origin of adakitic Intrusivesg generated during mid-Miocene east-west oxtension in southern Tibet. Earth and Planotary Science Letters, 2004. 220(139～155).
56.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.中国地质, 2006. 33(2): p. 340～351.
57.侯增谦,大陆碰撞成矿论.地质学报, 2010. 84(1): p. 30～58.
58.王登红;杨建民;闫升好;徐珏;陈毓川;薛春纪;骆耀;应汉龙;,西南三江新生代矿集区的分布格局及找矿前景. 23, 2002. 2: p. 6.
59.郭利果,刘玉平,徐伟,张兴春,秦克章,李铁胜,石玉若, SHRIMP锆石年代学对西藏玉龙斑岩铜矿成矿年龄的制约.岩石学报, 2006. 22(4): p. 1009～1016.
60.侯增谦,宋玉财,李政,等,青藏高原碰撞造山带Pb-Zn-Ag-Cu矿床新类型:成矿基本特征与构造控矿模型.矿床地质, 2008. 27(2): p. 123—144.
61.唐仁鲤,罗怀松,西藏玉龙斑岩铜(钼)矿带地质.北京:中国地质大学出版社, 1995. 320.
62.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. 83(12): p. 1887-1900.
63.陈建平,王功文,侯昌波,唐菊兴,基于GIS技术的西南三江北段矿产资源定量预测与评价.矿产地质, 2005. 24(4): p. 15-24.
64.邓军,侯增谦,莫宣学,杨立强,王庆飞,王长明,三江特提斯复合造山与成矿作用.矿床地质, 2010. 29(1): p. 37～42.
65. Spurlin.MS , Yin.A , Horton.BK , Zhou.JY , Wang.JH, Structural evolution of the Yushu-Nanggaian region and its relationship to syncollisional igneous activity,east-central Tibet. GSA bulletin, 2005. 117: p. 1293～1317.
66.郝金华,陈建平,董庆吉,王涛,罗志忠,青海三江北段陆日格含矿斑岩地球化学特征及其地质意义.岩石矿物地球化学通报, 2010. 29(4): p. 328～339.
67.郝金华,陈建平,田永革,李玉龙,尹京武,青海纳日贡玛斑岩钼(铜)矿含矿斑岩矿物学特征及成岩成矿意义.地质与勘探, 2010. 46(3): p. 367～376.
68.曲晓明,侯增谦,李佑国, S、Pb同位素对冈底斯斑岩铜矿带成矿物质来源和造山带物质循环的批示.地质通报, 2002.12. 21(11): p. 9.
69. Wang.JH,Yin.A,Harrison.TM, A tectonic model for Cenozoic igneous activites in the eastern Indo-Asian collison zone. Earth Planet Sci Lett, 2001. 199: p. 123～133.
70.周江羽,王江海,尹安,Spurlin.MS,Horton.BK,青藏东北缘早第三纪盆地充填的沉积型式及构造背景——以囊谦和下拉秀盆地为例.沉积学报, 2002. 20(01): p. 85～91.
71.刘英超,杨竹森,侯增谦,田世洪,王召林,宋玉财,薛万文,鲁海峰,王富春,张玉宝,朱田,俞长捷,苏嫒娜,李真真,于玉帅,青海玉树东莫扎抓铅锌矿床地质特征及碳氢氧同位素地球化学研究.矿床地质, 2009. 28(6): p. 770～784.
72.田世洪,杨竹森,侯增谦,刘英超,高延光,王召林,宋玉财,薛万文,鲁海峰,王富春,苏嫒娜,李真真,王银喜,张玉宝,朱田,俞长捷,于玉帅,玉树地区东莫扎抓和莫海拉亨铅锌矿床Rb-Sr和Sm-Nd等时线年龄及其地质意义.矿床地质, 2009. 28(6): p. 747～758.
73.陈建平,唐菊兴,陈勇,李葆华,尚北川,西南三江北段纳日贡玛铜钼矿床地质特征与成矿模式.现代地质, 2008. 22(1): p. 9～18.
74.宋忠宝,贾群子,陈向阳,陈博,张雨莲,张晓飞,全守村,栗亚芝,三江北段纳日贡玛花岗闪长斑岩成岩时代的确定及地质意义.地球学报, 2011. 32(2): p. 154～162.
75.潘桂棠,李兴振,王立全,丁俊,陈智粱,青藏高原及邻区大地构造单元初步划分. 2002. 21(11): p. 701～707.
76.潘桂棠,肖庆辉,陆松年,邓晋福,冯益民,张克信,张智勇,王方国,邢光福,郝国杰,冯艳芳,中国大地构造单元划分.中国地质, 2009. 36(1): p. 1～28.
77.鲁海峰,薛万文,王贵仁,纳日贡玛铜钼矿床地质特征及成因类型探讨.青海国土经略, 2006(3): p. 37～40.
78.青海地质调查院,中华人民共和国区域地质调查报告(1:25万)治多幅. 2006,西宁.
79. HanYg,ZhangSh,Franco,ZhangYh, Evolution of the Mesozoic Granites in the Xiong’ershan-Waifangshan Region,Western Henan Province,China,and Its Tectonic Implications. Acta Geologica Sinica, 2007. 81(2): p. 253～265.
80.迟清华,鄢明才,应用地球化学元素丰度数据手册. 2007,北京:地质出版社.
81.邱家骧,应用岩浆岩岩石学. 1991,北京:中国地质大学出版社.
82.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.矿床地质, 2003. 22(1): p. 12.
83.孟祥金,西藏碰撞造山带冈底斯中新世斑岩铜矿成矿作用研究. 2004,北京:中国地质科学院:博士论文.
84.何学贤,唐索寒,朱祥坤,多接收器等离子体质谱(MC-ICPMS)高精度测定Nd同位素方法.地球学报, 2007. 26:: p. 19～22.
85.黄萱,山西省花岗岩类的Nd和Sr同位素组成及构造演化意义[岩石学报, 1990. 6: p. 1～11.
86. Andersen.T, Correct ion of common Pb in U-Pb analyses that do not report 204 Pb. Chem Geol 2002. 192: p. 59～79.
87. Ludwig.KR.M;Berkely, Isoplot/Ex version 3.00. A Geochronological Toolkit for Microsoft Excel[2003, Berkeley Geochronology Center Special Publication. p. 1～70.
88.胡培远,李才,苏犁,李春斌,于红,青藏高原羌塘中部蜈蚣山花岗片麻岩锆石U-Pb定年—泛非与印支事件的年代学记录.中国地质, 2010. 37(4): p. 1050～1061.
89. Claesson.S,Vetrin.V,Bayanova.T, U-Pb zircon ages from a Devonian carbonatite dyke, Kola Peninsula, Russia: a record of geological evolution from the Archean to the Paleozoic : . Lithos, 2000. 51: p. 95～108.
90. Hoskin.P,Black.LP, Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon. Journal of Metamorphic Geology, 2000. 18: p. 423～439.
91.姜耀辉,蒋少涌,凌洪飞,戴宝章,陆-陆碰撞靠山环境下含铜斑岩岩石成因-以藏东玉龙斑岩铜矿带为例.岩石学报, 2006. 22(3): p. 697～706.
92.邓万明,孙宏娟,张玉泉,囊谦盆地新生代钾质火山岩成因岩石学研究.地质科学, 2001. 36(3): p. 304～318.
93. Whalen JB, C.B., Opaque mineralogy and mafic mineral chemistry of I-ad S-type granites of Lachlan fold belt,southeast Australia. American Mineralogist, 1988. 73(3): p. 281～296.
94.徐克勤,孙鼐,王德滋,刘昌实,陈克荣,华南两类不同成因花岗岩岩石学特征.岩石矿物及测试, 1982. 1(2): p. 1～12.
95. Clemens JD, W.V., Origin and evolution of a peralum ignous silicic ignimbrite suite:the violet town volcanics. Contrib Mineral Petrol, 1984. 88: p. 354～371.
96. White AJR, C.B., Granitoid types and their dirtribution in the Lachlan Fold Belt,southeastern Australia. Mem.Geol Soc Am, 1983. 159(21～34).
97.丁孝石,西藏中南部各类花岗岩中黑云母标型特征及其地质意义.中国地质科学院矿床地质研究所所刊, 1988. 1: p. 33～50.
98. Miller,SchusterR,KlotzliU,Frank,Purtscheller, Post-collisonal notassic and ultranotassic magmatism in SW Tibet:geochemical and Sr-Nd-Pb-O isotonic constraints for mantle source characteristics and netrogenesis. Petrol, 1999. 1999(40): p. 1339～1424.
99. WangJH,YinA,Harrison, A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collison zone Earth Planet., 2001. 199: p. 123～133.
100. Qu.Xm;Hou.Zq;Khin.Z;Li.Yg, Characteristics and genesis of Gangdese porhyry copper deposits in the south-and geochronological results. ore Geology Review, 2007. 31(205～223).
101.迟效国,李才,金巍,藏北羌塘地区新生代火山作用与岩石圈构造演化.中国科学(D辑), 2005. 35(5): p. 399~410.
102.马鸿文,西藏玉龙斑岩铜矿带花岗岩类与成矿.北京:中国地质大学出版社. 1990. 157.
103.李亚林,王成善,伊海生,刘志飞,李勇,西藏北部新生代大型逆冲推覆构造与唐古拉山的隆起.地质学报, 2006. 80(8): p. 1118～1131.
104. Ohmoto, C.B.H., Late-stage processes of felsic magmatism,In Ishihora S and Takenouchi S. Mining Geology Special Issue, 1980. 8: p. 1～11.
105. Takahashi M, A.S., Ishihara S, Magnetite-series/ilmenite-series vs I-type/S-type granitoids Mining Geology Special Issue, 1980. 8(13～28).
106.吕伯西,王增,张能德,段建中,高子英,沈敢富,潘长云,姚鹏,三江地区花岗岩类及其成矿专属性.中华人民共和国地质矿产部地质专报三岩石矿物地球化学第18号. 1993:地质出版社. 337.
107.秦克章,张连昌,丁奎首,许英霞,唐冬梅,徐兴旺,马天林,李光明,东天山三岔口铜矿床类型、赋矿岩石成因与矿床矿物学特征.岩石学报, 2009. 25(4): p. 845～861.
108.王召林,杨志明,杨竹森,田世洪,刘英超,马彦青,王贵仁,屈文俊,纳日贡玛斑岩钼铜矿床:玉龙铜矿带的北延-来自辉钼矿Re-Os同位素年龄的证据.岩石学报, 2008. 24(3): p. 503～510.
109. Ohmoto.H, Systematic of sulfur and carbon isotopes in hydrothermal ore deposits. Economic Geology, 1972. 67: p. 551～579.
110. Ohmoto.H, R.R.O., Isotopes of sulfur and carbon. Geochemistry of Hydrothermal ore deposits, ed. Barnes.HL. 1979, Now York: Wiley interscience. 509～567.
111.魏菊英,王关玉,同位素地球化学. 1988,北京:地质出版社.
112.黄朋,顾雪祥,唐菊兴,王立全,西藏玉龙斑岩铜(钼)矿床物质来源研究.大地构造与成矿学, 2002. 26(4): p. 429～435.
113.唐菊兴,西藏玉龙斑岩铜(钼)矿成矿作用与矿床定位预测研究. 2003,成都:成都理工大学:博士论文.
114. Harris.AC,Golding.SD,White.NC, Bajo de la Alumbrera copper-gold deposit:Stable isotope evidence for a porphyry-relater hydrothermal system dominated by magmatic aqueous fluids. Economic Geology, 2005. 100: p. 863～886.
115. Sillitoe.R.H, Porphyry Copper Systems. Economic Geology, 2010. 105: p. 3～41.
116.刘慧卿,李保华,唐菊兴,董树义,纳日贡玛铜钼矿床中流熔包裹体的发现及其意义.物探化探计算技术, 2007. 29(6): p. 534-536.
117. Gammons.CH, W.A., Chemical mobility of gold in the pophyry-epithermal environment. Economic Geology, 1997. 92(1): p. 45～59.
118.杨志明,侯增谦,夏代祥,宋玉财,李政,西藏驱龙铜矿西部斑岩与成矿关系的厘定:对矿床未来勘探方向的重要启示.矿床地质, 2008. 27: p. 28 -36.
119. Liang.HY,Campbell.IH, Allen.C, e.a., Ce4+/ce3+ ratios and ages for Yulong ore-bearing porhyries in eastern Tibet Mineralium Deposita, 2006. 41: p. 152～159.
120. Jugo.PJ, L.R., Richards.JP, Experimental determination of sulfur solubility in basaltic melts at sulfide vs.sulfate saturation:Possibale implications for ore formation in Eos,Transactions,AGU (2001 Fall Meeting Supplement ,Abstract V32G-05). 2001.
121. Hamlyn.PR;Keays.RR;Cameron.WE;Crawford.AJ;Waldron.HM, Precious metals in magnesian low-Tilavas:implications for metallogenesis and sulfur saturation in primary magmas Geochimica et Cosmochimica ACTA, 1985. 49(1797～1811).
122. Bornhorst.TJ;Rose.WI, Partitionging of gold in young calc-alkaline volcanic rocks form Guatemala Journal of Geology, 1986. 94(412～418).
123. Richards.JP, Alkalic-type epithermal gold deposits a review Mineralogical Association of Canada short course series 1995. 23: p. 367～400.
124.金章东,李福春,斑岩型铜矿床成矿过程中铜的迁移与沉淀机制研究新进展.矿产与地质, 1998. 12(64): p. 73～78.
125.南征兵,唐菊兴,李葆华,纳日贡玛斑岩铜钼矿成矿元素沉淀机制探讨.矿业研究与开发, 2007. 28(2): p. 1～3.
126. Agterberg FQ, B.C., Logistic regression and weights of evidence modeling in mineral exploration. Proc 28th Intern Symp Computer Applications in the Mineral Industries 1999: p. 483-490.
127.张玉泉,谢应雯,邱华宁,李献华,钟孙霖,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): p. 359～366.
128.朱训,德兴斑岩铜矿. 1983,北京:地质出版社.
129.丁林,张进江,周勇,邓万明,许荣华,钟大赉,青藏高原岩石圈演化的记录:藏北超钾质及钠质火山岩的岩石学与地球化学特征[J].岩石学报, 1999. 015(03): p. 408～421.
130.赖绍聪,青藏高原北部新生代火山岩的成因机制.岩石学报, 1999. 15(4): p. 98～104.
131.姜耀辉,蒋少涌,戴宝章,凌洪飞,玉龙斑岩铜矿含矿与非含矿斑岩元素和同位素地球化学对比研究.岩石学报, 2006. 22(10): p. 2561～2566.
132.莫宣学,赵志丹,邓晋福,董国臣,周肃,郭铁鹰,张双全,王亮亮;,印度—亚洲大陆主碰撞过程的火山作用响应.地学前缘, 2003. 10(3): p. 135～148.
133.王召林,侯增谦,杨竹森,田世洪,刘英超,杨志明,宋玉财,青海杂多地区新生代构造特征与两种类型矿床的关系.矿产地质, 2009. 28(2): p. 157～69.
134.许志琴,杨经绥,李海兵,嵇少丞,张泽明,刘焰,印度-亚洲碰撞大地构造.地质学报, 2011. 85(1): p. 1～32.
135.徐平,矿物成分的电子探针作图及其在矿物学研究中的应用.岩石学报, 1998. 14(3).
136.朱永峰,新一代电子探针是解决一些地球科学问题的好工具.地学前缘, 2003. 10(2): p. 435～436.
137.李雪梅,杜金菊,赵.胡.廖.江.,电子探针中的Map图在矿物出溶体中的应用.中山大学学报(自然科学版), 2004. 43(5): p. 95～97.
138.张文兰,王汝成,陈小明,赖明远,电子探针面分析与相分析技术及其应用.电子显微学报, 1999. 18(6): p. 630～639.
139.陈毓川,毛景文,骆耀南,魏家秀等,四川大水沟碲金矿床地质和地球化学. 1996:原子能出版社. 146.
140.银剑钊,世界首例独立碲矿床的成矿机理及成矿模式. 1996,重庆:重庆出版社. 190.
141.骆耀南,曹志敏,四川省发现世界首例独立碲矿床.中国地质, 1994(2): p. 27～28.
142.毛景文,陈毓川,杨百川,雷蕴芬,周剑雄,四川省石棉县大水沟碲矿床中的辉碲铋矿研究.地质科学, 1995. 30(1): p. 47～51.
143.邱士东,王葆华,徐九化,谢玉玲,因硫碲铋矿在中国的首次发现.矿物学报, 2008. 28(4): p. 357～359.
144.赵玉山,金成洙,关广岳,辽宁舞龙金矿铋矿物与金矿化关系研究.矿物学报, 1994. 14(1): p. 88～91.
145.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. 28(5): p. 515～538.
146. Shirey.SB,Walker.RJ, Carius tube digestion for low-blank Rhenium-Osmium analysis. Anal Chem, 1995. 67: p. 2136～2141.
147.杜安道,赵敦敏,王淑贤, 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): p. 247～252.
148.高一鸣,陈毓川,唐菊兴,西藏沙让斑岩钼矿床锆石SHRIMP定年和角闪石Ar-Ar定年及其地质意义矿床地质, 2010. 29(2): p. 323～331.
149.杨宗喜;毛景文;陈懋弘;童祥;武俊德;程彦博;赵海杰,云南个旧卡房矽卡岩型铜锡矿Re-Os年龄及其地质意义.岩石学报, 2008. 24(8): p. 1937～1944.
150.唐菊兴,王成辉,屈文俊,杜安道,应立娟,高一鸣,西藏玉龙斑岩铜钼矿辉钼矿铼-锇同位素定年及其成矿学意义.岩矿测试, 2009. 28(3): p. 215～218.
151.杜安道,何红蓼,殷宁万,邹晓秋,孙亚利,孙德忠,陈少珍,屈文俊,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): p. 339～347.
152.王登红,屈文俊,李志伟,应汉龙,陈毓川,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), 2004. 34(4): p. 345～349.
153.邢俊兵,郭晓东,屈文俊,王治华,李汉光,马厂箐斑岩型铜、钼矿辉钼矿Re黄金科学技术, 2009. 17(5): p. 24～29.
154. Luo.JL, C.Y., Wang.DH, Chronagenesis of endogenetic mineralization on the east side of the Qinghai-XiZang plateau Acta Geologica Sinica, 2000. 74(3): p. 447～451.
155. Wang.DH, C.Y., Xu.J,Yang.JM.Xue.CJ,Yan.SH, Cenozoic mieralization in China,as a key to past mineralization and a clue to future prospecting. Acta Geologica Sinica, 2000. 74(3): p. 478～484.
156. Camus.F;Dines.JH, A special issue devoted to porphyry copper deposits of northern Chile-perface. Economic Geology, 2001. 96: p. 233～238.
157. Kay.RWJ, Aleutian magnesium andesites:melts from subducted Pacific oceanic crust. jour Volcan Geotherm Res, 1978. 4(117～132).
158. Stern.CR;Kilian.R, Role of the suvducted slab,mantle wedge and continental crust in the generation of adakites from the Andean arutral volcanic zone Contrib Mineral Petrol, 1996. 123(263～281).
159.赵志丹;莫宣学;董国臣;周肃;朱弟成;廖忠礼;孙晨光,青藏高原Pb同位素地球化学及其意义.现代地质, 2007.6. 21(2): p. 265～274.
160.郝金华,陈建平,董庆吉,李玉龙,王涛,马继义,青海三江北段斑岩钼铜矿带含矿斑岩地球化学、Sr-Nd-Pb同位素特征及地质意义.岩石矿物学杂志, 2011. 30(3): p. 515～525.
161.莫宣学,青藏高原岩浆岩成因研究:成果与展望.地质通报, 2009.12. 28(12): p. 1693～1702.
162.莫宣学,青藏高原地质研究的回顾与展望.中国地质, 2010.8. 37(4): p. 841～853.
163.莫宣学,赵志丹,朱弟成,喻学惠,董国臣,周肃.,西藏南部印度—亚洲碰撞带岩石圈:岩石学-地球化学约束.地球科学(中国地质大学学报, 2009. 34(1): p. 17～27.
164. Dewey.JF; Shackleton.RM; Chang.C, e., The tectonic evolution of the Tibetan Plateau. 1988, London: Philosophical Transation of rhe Royal Society
165. Wang.JH;Yin.A;Harrison.TM;Grove.M, A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collision Zone. Earth and Planetary Science Letters, 2001. 88: p. 123～133.
166.董庆吉,西南三江北段区域成矿定量预测与评价. 2009,中国地质大学(北京):北京.
167.王治华,郭晓东,喻万强,邹依林,徐涛,张勇,云南省马厂箐铜钼金多金属矿床地质特征及成矿规律.地质与勘探, 2010. 46(2): p. 214～223.
168.王治华,郭晓东,陈祥,葛良胜,邹依林,云南祥云马厂箐富碱斑岩体的地球化学特征及其形成的构造环境.地质论评, 2010. 56(1): p. 125～135.
169.郭晓东,王治华,陈祥,王欣,王淑贤,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. 83(12): p. 1901～1915.
170.邢俊兵,郭晓东,屈文俊,王治华,李汉光,马厂箐斑岩型铜、钼矿辉钼矿Re-Os年龄及地质意义.黄金科学技术, 2009. 17(5): p. 24～29.
171.梁华英,谢应雯,张玉泉,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(116～120).
172.黄波,梁华英,莫济海,谢应雯,金平铜厂铜钼矿床赋矿岩体锆石LA-ICP-MS U-Pb年龄及意义.大地构造与成矿学, 2009. 33(4): p. 598～602.
173.应汉龙,刘和林,杨许中,李志伟,云南金平铜厂金矿床地质特征和成矿物质来源.地质与资源, 2006. 15(4): p. 265～272.
174.祝向平,云南哈播斑岩型铜(钼金)矿床地质特征与成矿作用研究. 2010,中国地质大学(北京):北京.
175. Leloup.PH;Arnaud.N;Lacassin.R;Kienast.JR;Harrison.TM;Trong.TTP;Replunaz.A;Tapponnier.P, New constraints on the structure,thermochronology,and timing of the Ailao Shan-Red river shear zone,SE Asia. Journal of Geophysical Research, 2001. 106: p. 6683～6732.
176. Yin.A,Harrison.Tm, Geologic evolutin of the Himalayan-Tibetan orogen. Earth Planet sci, 2000. 28: p. 211～280.
© 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 |