Ballard J R,et al.2001.Two age of porphyry intrusion resoved for the super-giant Chuquicamata copper deposit of northern Chile by ELAICP-MS and SHRIMP[J].Geology,29(5):383-393.
[2]
Bi X W,Hu R Z,Ye Z J and Sbso S X.1999.Research on the rehtionship between A-type granitoid and Cu metallogenic:Taking Machengqing Cu deposit as an example[J].Science in China (Series D),29(6):489-495(in Chinese).
[3]
Bi X W,Hu R Z,Peng J T,Wu K X,Su W C and Zhan Z X.2005.Geochemical characteristics of the Yao\'an and Machangqing alkalinerich intrusions[J].Acta Petrolngica Sinica,21(1):113-124 (in Chinese with English abstract).
[4]
Blevin P L,et al.1992.The role of magma sourees,oxidation states and fraetzonation in determining the granite metallogeny of eastern Australia[J].Transactions of the Royal Sceiety of Edinburgh,Earth Scinces,83:305-315.
[5]
Candela P A.1992.Controls on ore metal ratios in grante-related oresysterns:An experimental and computational approaeh[J].Transactions of the Royal Soeiety of Edinburgh,Earth Sciences,83:317-27.
[6]
Cherniak D J,et al.1997.Rare-earth diffusion in zircon[J].Chemical Geology,134:289-299.
[7]
Ge L S,Zou Y L,Li Z H,Guo X D,Xing J B and Zhang X H.2002.Geological features and genesis of Machangqing Cu-Mo-Au deposit related to the alkali-rich magmatie rock,Yuannan Province[J].Geology and Prospecting,38(5):11-17 (in Chinese with English abstract).
[8]
Guo X D,Wang Z H and Qu W J.2008.Re-Os dating of molybdenites from Machangqing porphyry-type Cu-Mo deposit in Yunnan Province,and its geological significance[A].In:Chen Y C,et al.ed.Symposium of the 9th National Conference on Mineral Resources of China[C].The 9th National Coherence on Mineral Resources of China.2008.Beijing:Geol.Pub.House.453-454 (in Chinese).
[9]
Guo X D,Hou Z Q,Chert X and Wang Z H.2009a.Identification of adakitic characteristics of Machangqing alkali-rich porphyry in Yunnan Province and its significance to mineralization research[J].Acts Petrolngica et Mineralogica,28(4):375-386 (in Chinese with English abstract).
[10]
Guo X D,Wang Z H,Chen X,Wang X and Wang S X.2009b.Machangqing porphyry-type Cu-Mo-Au deposit,Yunnan Province:Geological charaeteristica and its genesis[J].Acta Geological Sinica,83(12):1901-1914 (in Chinese with English abstract).
[11]
He M Q,Yang S Y and Liu J J.2003.The relationship between the organic matter and the gold content of Jingchangqing Au-Cu ore deposits in Xiangyun of Yunnan[J].Journal of Kunming University of Science and Technoloy (Science and Technology Edition),28(1):4-7 (in Chinese with English abstract).
[12]
He M Q and Yang S Y.2004a.Geological geochemistry and genesis of Xiaolongtan-Maehengqing Cu-Au polymetallic ore deposit in Western Yunnan[M].Beijing:Geol.Pub.House (in Chinese).
[13]
He M Q,Yang SY,Liu J J and Li C Y.2004b.Characteristics of oreforming fluids and their origin in Jinchenqing gold (copper) ore deposits in Xiangyun,Yunnan[J].Mineral and Rock,24(2):35-40(in Chinese with English abstract).
[14]
Hedenquist J W and Lowenst J B.1994.The role of magmas in formation of hydrothermal ore deposits[J].Nature,370:519-527.
[15]
Hou Z Q.2004.Porphyry Cu-Mo-Au deposits:Some new insights and advances[J].Earth Science Frontiers,11(1):131-144 (in Chinese with English abstract).
[16]
Hu R Z,Bi X W,Turner G and Burnard P G.1997.He-At isotopic system in pyrite fluid inclusions of Machangqing Cu deposit[J].Science in China (Series D),27(6):503-508 (in Chinese).
[17]
Hu X Z and Huang Z.1997.The characteristics and genesis of alkali-rich granite-porphyry in west margin of Yangtze Craton,China[J].Geotectonica et Metallogenica,21(2):173-180 (in Chinese).
[18]
Liu X F,Liu J D,Zhang C J,Yang Z X,Wu D C and Li Y G.2004.Isotopic geochemistry of intrusives and ore-veins from alkali-rich por phyry type deposits in western Yunnan,China[J].Bulletin of Mineralogy,Petrology and Geochemistry,23(1):32-39 (in Chinese with English abstract).
[19]
Liang H Y,Xie Y W,Zhang Y Q and Campbell I.2004.Forming of Krich alkalescence rock restrict the metaUogenic of Cu:Machangqing Cu deposit as an example[J].Natural Science Evolution,14(1):116-120(inChinese).
[20]
Luo Z H,Lu X X,Guo S F,Sun J,Chen B H,Huang F and Yang Z F.2008.Metallogenic systems on the transmagmatic fluid theory[J].Acta Petrologica Sinica,24(12):2669-2678 (in Chinese with English abstract).
[21]
更多...
[22]
Luo Z H,Lu X X,Chen B H,Li M L,Liang T,Huang F and Yang Z F.2009.Introduction to the metaUogenic theory on the transmagmatic fluids[M].Beijing:Geol.Pub.House (in Chinese).
[23]
Ohmoto H.1972.Systematics of sulfur and carbon isotopes in Hydrothermal ore deposits[J].Econ.Geol.,67:551-578.
[24]
Peng J T,Bi X W,Hu R Z,Wu K X and Sang H Q.2005.Determination of porpahyry ore and rock forming time of the Machangqing Cu (Mo) deposit,western Yunnan Province[J].Acts Mineralogica Sinica,25(1):69-74 (in Chinese with English abstract).
[25]
Shen W Z,et al.1987.Stable isotopic geology[M].Beijing:Atomic Energy Press (in Chinese).
[26]
Sillitoe R H.1997.Characteristics and controls of the largest porphyry copper-gold and epithermal gold deposits in the circum-Pacific region[J].Austr.Jour.Earth Sci.,44:373-388.
[27]
Wang D H,Qu W J,Li Z W,Ying HL and Chen Y H.2004.The mineralization concentration stage of Jinshajiang-Honghe metallogenetic belt porphyry copper,molybdenum deposit[J].Science in China (Series D),34(4):345-349(in Chinese).
[28]
Wybon D.1994.Sulphur-underssturated magmatism:A key factor for generating magma-related copper-gold deposits[J].AGSO Research Newsletter,21:7-8.
[29]
Yang J K and Tang Z G.1996.Mineralization characteristics and prospective prediction of the Cenozoic hypabyssal porphyry gold deposit in Yunnan Province[J].Beijing Geology,(3):27-31 (in Chinese with English abstract).
[30]
Yu G J.1988.A preliminary study on geological conditions of metallogenesis and genesis of Machangqin gold deposit[J].Journal of Kunming Institute of Technology,13(1):1-10 (in Chinese with English abstract).
[31]
Zeng P S,Mo X X and Yu X H.2002.Nd,Sr and Pb isotopic characteristics of the alkali-rich porphy zone in western Yonnan and its compression strike-slip setting[J].Acts Petrologica et Mineralogica,21 (3):231-241 (in Chinese with English abstract).
[32]
Zeng P S,Hou Z Q,Gao Y F and Du A D.2006.The Himalayen CuAu mineralization in the Eastern Indo-Asian collision zone:Constraints from Re-Os dating of molybdenite[J].Geological Review,52(1):72-84 (in Chinese with English abstract).
[33]
Zhang Y Q,Xie Y W and Tu G Z.1987.Preliminary studies of the alkali-rich intrusive rocks in the Ailacahan-Jinshajiang belt and their relationship with rift tectonics[J].Acta Petrologica Sinica,(1):17-25(in Chinese).
[34]
Zhang Y Q and Xie Y W.1997.Chronology and Nd-Sr isotopes of tbe Ailaoshan-Jinshajiang alkali-rich intrusions[J].Science in China (Series D),27(4):289-293 (in Chinese).
[35]
Zhao H.1995.Metallogenic model of Pb-Cu-Mo-Au deposit rehted to porphyry of Himalaya period in Zhongdien-Dali-Jinping area[J].Yunnan Geology,14(4):333-341(in Chinese).
[36]
Zhu B Q.1997.The theory and application of the isotopic systematic in the earth science[M].Beijing:Science Press (in Chinese with English abstract).
[37]
Zhu X,Huang C K,Rui Z Y,Zhou Y H,Zhu X J,Hu Z S end Mei Z K.1983.Dexing porphyry-type copper deposit,China[M].Beijing:Geol.Pub.House (in Chinese).