德兴斑岩铜矿含矿斑岩成因及成矿机制
|
摘要
德兴斑岩铜矿是中国最大的斑岩型铜矿,属环太平洋斑岩型铜矿带西带的一部分。前人已对该矿床做了大量的研究,但在含矿斑岩成因及其成岩成矿构造背景等方面仍存在很大的分歧。针对德兴斑岩铜矿目前研究现状及存在问题,本论文在前人工作基础上,重点对德兴斑岩铜矿三个矿区的含矿斑岩开展了锆石U-Pb年代学、元素和Sr-Nd-Pb同位素地球化学以及锆石原位Hf同位素地球化学研究,同时还开展了辉钼矿Re-Os年代学、矿石Pb同位素地球化学和大脉型矿石中热液锆石U-Pb年代学、微量元素地球化学以及流体包裹体测温等研究工作。通过研究取得了新进展。
LA-ICP-MS锆石U-Pb定年结果表明,德兴三个矿区的含矿斑岩均形成于中侏罗世早期(170-171 Ma)。含矿斑岩主要属于高钾钙碱性系列,同时具有埃达克岩特征,例如,高Sr、低Y和Yb含量,高Sr/Y和La/Y比值以及高Mg#。这些含矿斑岩的初始87Sr/86Sr比值介于0.7044-0.7047之间,εNd(T)值介于-1.4～+0.5之间,锆石原位εHf(T)值介于+2.6～+4.6之间。斑岩具有非常高的放射成因Pb同位素组成,初始206Pb/204Pb比值可达18.377,207Pb/204Pb比值可达15.614,208Pb/204Pb比值可达38.491。这些Sr-Nd-Pb-Hf同位素特征明显不同于扬子下地壳和太平洋洋中脊玄武岩,但与西太平洋海沟沉积物相一致。详细的元素和同位素地球化学数据表明,德兴含矿斑岩形成于与古太平洋板块俯冲有关的活动大陆边缘环境。俯冲大洋板片(主要为上覆沉积物)部分熔融形成的熔体,在其上升过程中与岩石圈地幔相互作用,最终形成了高钾钙碱性的埃达克质斑岩岩浆。
辉钼矿Re-Os定年结果表明,德兴斑岩铜矿主成矿作用与岩浆侵入作用几乎同时发生(～171Ma)。德兴斑岩铜矿中辉钼矿含有非常高的Re和187Os含量,完全不同于陆壳改造(南岭成矿带)或拆沉加厚下地壳部分熔融(东秦岭-大别成矿带)所形成的辉钼矿的Re-Os同位素组成特征,而与俯冲板片起源的含矿斑岩相关的辉铝矿(太平洋东岸Cordillera和Andes成矿带)极为相似。可见,德兴斑岩铜矿更可能形成于活动大陆边缘环境,与前文通过含矿斑岩成因研究得出的结论相一致。矿石中黄铁矿的Pb同位素组成与含矿斑岩相一致,而明显不同于与围岩双桥山群地层有成因联系的矿石Pb同位素组成。Os-Pb同位素组成特征表明成矿物质主要来自含矿斑岩岩浆,是板片起源的埃达克质岩浆通过与岩石圈地幔相互作用从岩石圈地幔中萃取出来的。
大脉型含矿石英脉中锆石SHRIMP U-Pb年代学、微量元素地球化学以及流体包裹体研究结果表明,德兴斑岩铜矿存在早白垩世晚期(～104.3 Ma)成矿作用事件,该期成矿热液显示中低温低盐度特征,形成矿区大脉型矿石。有关该期成矿事件机制及经济价值还有待今后进一步研究。
The Dexing porphyry copper deposits (Tongchang, Fujiawu and Zhushahong), comprising the circum-Pacific porphyry copper ore belt, is the largest porphyry copper deposit in China. Although considerable studies have been done for the deposits, there are some controversies on the petrogenesis of the ore-bearing porphyries and geological setting. This paper presents new LA-ICP-MS zircon U-Pb and molybdenite Re-Os dating, whole-rock elemental, Sr-Nd-Pb isotopic and in-situ zircon Hf isotopic geochemistry for the three ore-bearing porphyries, Pb isotopic geochemistry for pyrites, SHRIMP U-Pb dating and trace elemental geochemistry, as well as fluid-inclusion measurements for the ore-bearing quartz veins or their hydrothermal zircons, in order to better constrain their petrogenesis and metallogeny.
LA-ICP-MS zircon U-Pb dating shows that the Dexing ore-bearing porphyries were emplaced in the early Middle Jurassic (～171 Ma). The porphyries are mainly high-K calc-alkaline and show some adakitic affinities, i.e. characterized by high Sr and low Y and Yb contents, with high Sr/Y and La/Yb ratios, and by high Mg#, higher than pure crustal melts. These porphyries have initial 87Sr/86Sr ratios of 0.7044-0.7047,εNd(T) values of-1.4 to+0.5 andεHf(T) (in-situ zircon) values of +2.6 to+4.6. They show unusually radiogenic Pb isotopic compositions with initial 206Pb/204Pb up to 18.377,207Pb/204Pb up to 15.614 and 208Pb/204Pb up to 38.491.These Sr-Nd-Pb-Hf isotopic signals are distinctly different either from the Pacific MORB or from the Yangtze lower crust, but similar to the subducting sediments in the West Pacific trenches. Detailed elemental and isotopic data suggest that the Dexing porphyries were emplaced in a continental arc setting coupled with the westward subduction of the Paleo-Pacific plate. Partial melting of the subducted slab (mainly overlying sediments), with subsequent melts interacting with the lithospheric mantle wedge, formed the high-K calc-alkaline porphyry magmas.
The molybdenite Re-Os dating indicates that the associated Cu-Mo mineralization was nearly contemporaneous (～171 Ma) with the porphyry emplacement. The molybdenites from the Dexing porphyry copper deposits show high rhenium and 187Os contents, which is obviously different from those related to crust re-melting (Nanling Metallogenic Belt) or partial melting by the delamination thickened crust (east Qinling-Dabie Metallogenic Belt), but compatible with those related to partial melting by the subducted slab (Andes and Cordillera Metallogenic Belts). Thus, the Dexing porphyry copper deposits should be emplaced in an active continental arc setting, which is consistent with the studies above on the ore-bearing porphyries. Pb isotopic compositions in Pyrites from Tongchang and Fujiawu are uniform and distinctly different from those derived from Shuangqiaoshan Strata meta-sedimentary rocks, but similar to those of the ore-bearing granodiorite porphyries. Detail Pb-Os isotopic evidences suggest the sources of Cu-Au-Mo metals were related to the intrusion magmas, other than the wall-rocks. They should be mainly extracted from the lithospheric mantle, after the oceanic crust-derived adakitic magmas interacting with the lithospheric mantle wedge.
SHRIMP zircon U-Pb dating, trace elemental geochemistry and fluid-inclusion measurements for the ore-bearing quartz veins indicate that a subordinate Cu mineralization related to the hydrothermal event occurred at the late stage of Lower Jurassic (～104.3 Ma). The ore-forming fluids show epithermal and low salinity affinities, which is distinctly different from the magmatic fluids. We uncertain whether this metallogenic event has contributed some economic ore-bodies to the Dexing porphyry copper deposit. Thus, a further study should be done in the future.
LA-ICP-MS锆石U-Pb定年结果表明,德兴三个矿区的含矿斑岩均形成于中侏罗世早期(170-171 Ma)。含矿斑岩主要属于高钾钙碱性系列,同时具有埃达克岩特征,例如,高Sr、低Y和Yb含量,高Sr/Y和La/Y比值以及高Mg#。这些含矿斑岩的初始87Sr/86Sr比值介于0.7044-0.7047之间,εNd(T)值介于-1.4～+0.5之间,锆石原位εHf(T)值介于+2.6～+4.6之间。斑岩具有非常高的放射成因Pb同位素组成,初始206Pb/204Pb比值可达18.377,207Pb/204Pb比值可达15.614,208Pb/204Pb比值可达38.491。这些Sr-Nd-Pb-Hf同位素特征明显不同于扬子下地壳和太平洋洋中脊玄武岩,但与西太平洋海沟沉积物相一致。详细的元素和同位素地球化学数据表明,德兴含矿斑岩形成于与古太平洋板块俯冲有关的活动大陆边缘环境。俯冲大洋板片(主要为上覆沉积物)部分熔融形成的熔体,在其上升过程中与岩石圈地幔相互作用,最终形成了高钾钙碱性的埃达克质斑岩岩浆。
辉钼矿Re-Os定年结果表明,德兴斑岩铜矿主成矿作用与岩浆侵入作用几乎同时发生(～171Ma)。德兴斑岩铜矿中辉钼矿含有非常高的Re和187Os含量,完全不同于陆壳改造(南岭成矿带)或拆沉加厚下地壳部分熔融(东秦岭-大别成矿带)所形成的辉钼矿的Re-Os同位素组成特征,而与俯冲板片起源的含矿斑岩相关的辉铝矿(太平洋东岸Cordillera和Andes成矿带)极为相似。可见,德兴斑岩铜矿更可能形成于活动大陆边缘环境,与前文通过含矿斑岩成因研究得出的结论相一致。矿石中黄铁矿的Pb同位素组成与含矿斑岩相一致,而明显不同于与围岩双桥山群地层有成因联系的矿石Pb同位素组成。Os-Pb同位素组成特征表明成矿物质主要来自含矿斑岩岩浆,是板片起源的埃达克质岩浆通过与岩石圈地幔相互作用从岩石圈地幔中萃取出来的。
大脉型含矿石英脉中锆石SHRIMP U-Pb年代学、微量元素地球化学以及流体包裹体研究结果表明,德兴斑岩铜矿存在早白垩世晚期(～104.3 Ma)成矿作用事件,该期成矿热液显示中低温低盐度特征,形成矿区大脉型矿石。有关该期成矿事件机制及经济价值还有待今后进一步研究。
The Dexing porphyry copper deposits (Tongchang, Fujiawu and Zhushahong), comprising the circum-Pacific porphyry copper ore belt, is the largest porphyry copper deposit in China. Although considerable studies have been done for the deposits, there are some controversies on the petrogenesis of the ore-bearing porphyries and geological setting. This paper presents new LA-ICP-MS zircon U-Pb and molybdenite Re-Os dating, whole-rock elemental, Sr-Nd-Pb isotopic and in-situ zircon Hf isotopic geochemistry for the three ore-bearing porphyries, Pb isotopic geochemistry for pyrites, SHRIMP U-Pb dating and trace elemental geochemistry, as well as fluid-inclusion measurements for the ore-bearing quartz veins or their hydrothermal zircons, in order to better constrain their petrogenesis and metallogeny.
LA-ICP-MS zircon U-Pb dating shows that the Dexing ore-bearing porphyries were emplaced in the early Middle Jurassic (～171 Ma). The porphyries are mainly high-K calc-alkaline and show some adakitic affinities, i.e. characterized by high Sr and low Y and Yb contents, with high Sr/Y and La/Yb ratios, and by high Mg#, higher than pure crustal melts. These porphyries have initial 87Sr/86Sr ratios of 0.7044-0.7047,εNd(T) values of-1.4 to+0.5 andεHf(T) (in-situ zircon) values of +2.6 to+4.6. They show unusually radiogenic Pb isotopic compositions with initial 206Pb/204Pb up to 18.377,207Pb/204Pb up to 15.614 and 208Pb/204Pb up to 38.491.These Sr-Nd-Pb-Hf isotopic signals are distinctly different either from the Pacific MORB or from the Yangtze lower crust, but similar to the subducting sediments in the West Pacific trenches. Detailed elemental and isotopic data suggest that the Dexing porphyries were emplaced in a continental arc setting coupled with the westward subduction of the Paleo-Pacific plate. Partial melting of the subducted slab (mainly overlying sediments), with subsequent melts interacting with the lithospheric mantle wedge, formed the high-K calc-alkaline porphyry magmas.
The molybdenite Re-Os dating indicates that the associated Cu-Mo mineralization was nearly contemporaneous (～171 Ma) with the porphyry emplacement. The molybdenites from the Dexing porphyry copper deposits show high rhenium and 187Os contents, which is obviously different from those related to crust re-melting (Nanling Metallogenic Belt) or partial melting by the delamination thickened crust (east Qinling-Dabie Metallogenic Belt), but compatible with those related to partial melting by the subducted slab (Andes and Cordillera Metallogenic Belts). Thus, the Dexing porphyry copper deposits should be emplaced in an active continental arc setting, which is consistent with the studies above on the ore-bearing porphyries. Pb isotopic compositions in Pyrites from Tongchang and Fujiawu are uniform and distinctly different from those derived from Shuangqiaoshan Strata meta-sedimentary rocks, but similar to those of the ore-bearing granodiorite porphyries. Detail Pb-Os isotopic evidences suggest the sources of Cu-Au-Mo metals were related to the intrusion magmas, other than the wall-rocks. They should be mainly extracted from the lithospheric mantle, after the oceanic crust-derived adakitic magmas interacting with the lithospheric mantle wedge.
SHRIMP zircon U-Pb dating, trace elemental geochemistry and fluid-inclusion measurements for the ore-bearing quartz veins indicate that a subordinate Cu mineralization related to the hydrothermal event occurred at the late stage of Lower Jurassic (～104.3 Ma). The ore-forming fluids show epithermal and low salinity affinities, which is distinctly different from the magmatic fluids. We uncertain whether this metallogenic event has contributed some economic ore-bodies to the Dexing porphyry copper deposit. Thus, a further study should be done in the future.
引文
Aguillon-Robles, A., Caimus, T., Bellon, H., Maury, R. C., Cotton, J., Bourgois, J. and Michaud, F.,2001, Late Miocene adakites and Nb-enriched basalts from Vizcaino Peninsula, Mexico: indicators of East Pacific Rise subduction below southern Baja California. Geology, v.29, p. 531-534.
Alt, J.C.B., and Urdett, J.W.,1992, Sulphur in Pacific deep-sea sediments (Leg 129) and implications for cycling of sediment in subduction zones. Proceedings ODP Science Research, v.129, p.283-294.
Andersen, T.,2002, Correction of common Pb in U-Pb analyses that do not report 204Pb. Chemical Geology, v.192, p.59-79.
Barra, F., Ruiz, J., Valencia V.A., Ochoa-Landin, L., Chesley, J.T., and Zurcher, L.,2005, Laramide Porphyry Cu-Mo Mineralization in Northern Mexico:Age Constraints from Re-Os Geochronology in Molybdenite. Economic Geology, v.100, p.1605-1616.
Barry, T. L., Saunders, A. D., Kempton, P. D., Windley, B. F., Pringle, M. S., Dorjnamjaa, D., and Saandar, S.,2003, Petrogenesis of Cenozoic basalts from Mongolia:Evidence for the role of asthenospheric versus metasomatized lithospheric mantle sources. Journal of Petrology, v.44, p. 55-91.
Black, L.P. and Gulson, B.L.,1978, The age of the Mud Tank carbonatite, Strangways Range, Northern Territory. BMR Journal of Australian Geology and Geophysics, v.3, p.227-232.
Blichert-Toft, J., and Albarede, F.,1997, The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system. Earth and Planetary Science Letters, v.148, p.243-258.
Bodnar, R.J.,1993, Revised equation and table for determining the freezing point depression of H2O-NaCl solutions. Geochimica et Cosmochimica Aeta, v.57, p.683-684.
Bourdon, E., Eissen, J.P., Monzier, M., Robin, C., Martin, H., Cotton, J., and Hall, M.L.,2002, Adakite-like lavas from Antisana volcano (Ecuador):evidence for slab melt metasomatism beneath the Andean Northern Volcanic Zone. Journal of Petrology, V.43, p.199-217.
Boynton, W.V.,1984, Cosmochemistry of the earth elements. meteorite studies. In:Henderson, R. (ed.) Rare Earth Element Geochemistry. Developments in Geochemistry 2, Amsterdam, Elsevier, p.89-92.
Burnham, C.W., and Ohmoto, H.,1980, Late-stage processes of felsic magmatism. Mining Geology Special Issue, v.8, p.1-11.
Carroll, M., and Rutherford, M.J.,1985, Sulfide and sulfate saturation hydrous silicate melts. Journal of Geophysics, v.90, p. C601-C612.
Carroll, M., and Rutherford, J.M.,1987, The stability of igneous anhydrite experimental results and implications for sulfur behavior in the 1982 El Chichon trachyandesite and other evolved magmas., Journal of Petrology, v.28, p.781-801.
Carter, A., Roques, D., Bristow, C., and Kinny, P.,2001, Understanding Mesozoic accretion in Southeast Asia:Significance of Triassic thermotectonism (Indosinian orogeny) in Vietnam. Geology, v.29, p.211-214.
Charvet, J., Lapierre, H., and Yu, Y.,1994, Geodynamic significance of the Mesozoic volcanism of southeastern China. Journal of Southeast Asian Earth Sciences, v.68, p.387-396.
Chaussidon, M., Albarede, F., and Sheppard, S.M.F.,1987, Sulphur isotope heterogeneity in the mantle from ion microprobe measurements of sulphide inclusions in diamond, Nature, v.330, p. 242-244.
Chaussidon, M., Albarede, F., and Sheppard, S.M.F.,1989, Sulphur isotope variation in the mantle from ion microprobe analyses of mic-sulphide inclusion. Earth Planet. Sci. Lett., v.92, p. 144-156.
Chaussidon, M., and Lorand, J.P.,1990, Sulphur isotope composition of orogenic spinel lherzolite massifs from Ariege (North-Eastern Pyrenees, France):an ion microprobe study. Geochim. Cosmochim. Acta, v.54, p.2835-2846.
Chen, J.F.& Jahn, B.M.,1998, Crustal evolution of Southeast China:Nd and Sr isotopic evidence. Tectonophysics, v.284, p.101-133.
Chiaradia, M., Vallance, J., Fontbote, L., Stein, H., Schaltegger, U., Coder, J., Richards, J., Villeneuve, M., and Gendall,I.,2009, U-Pb, Re-Os, and 40Ar/39Ar geochronology of the Nambija Au-skarn and Pangui porphyry Cu deposits, Ecuador:implications for the Jurassic metallogenic belt of the Northern Andes. Miner Deposita, v.44, p.371-387.
Claoue-Long, J.C., King, R.W., Kerrich, R.,1990, Archaean hydrothermal zircon in the Abitibi greenstone belt:Constraintson the timing of gold mineralization. Earth and Planetary Science Letters, v.98, p.109-128.
Condie, K.C.,1976, Plate Tectonics and Crustal Evolutionsecond ed:Pergamon Press, New York.
Cooke, D.R., Hollings, P., and Walsh, J.L.,2005, Giant porphyry deposits:Characteristics, distribution, and tectonic controls. Economic Geology, v.100, p.801-818.
Defant, M.J., and Drummond, M.S.,1990, Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, v.347, p.662-665.
de Hoog, J.C.M., Mason, P.R.O., and van Bergen, M,J,,2001, Sulfur and chalcophile elements in Subduction zones:Constraint from a laser ablation ICP-MS study of melt inclusions from Galunggung volcano, Indonesia. Geochimica et Cosmochimica Aeta, v.65, p.3147-3167.
Dubinska, E., Bylina, P., Kozlowski, A., Dorr, W., Nejbert, K., Schastok, J., and Kulicki, C.,2004, U-Pb dating of serpentinization:hydrothermal zircon from a metasomatic rodingite shell (Sudetic ophiolite, SW Poland). Chemical Geology, v.203, p.183-203.
Eldridge, C.S., Compston, W., Williams, I.S., Harris, J.W., and Bristow, J.W.,1991, Isotopic evidence for the involvement of recycled sediments in diamond formation. Nature, v.353, p. 649-653.
Force, E.R.,1998, Laramide alteration of Proterozoic diabase:A likely contributor of copper to porphyry systems in the Dripping Spring mountains area, southeastern Arizona. Economic Geology, v.93, p.171-183.
Fu, B., Mernagh, T.P., Kita, N.T., Kemp, A.I.S., and Valley, J.W.,2009, Distinguishing magmatic zircon from hydrothermal zircon:A case study from the Gidginbung high-sulphidation Au-Ag-(Cu) deposit, SE Australia. Chemical Geology 259 (2009) 131-142.
Gammons, C.H., Bloom, M.S., and Yu, Y.,1992, Experimental investigation of the hydrothermal geochemistry platinum and palladium,1, Solubility of platinum and palhdlum sulphide minerals in NaCl/H2SO4 solutions at 300℃. Geochimica et Cosmochimica Aeta, v.56, p.3881-3894.
Gao, Y.F., Hou, Z.Q., and Wei, R.H.,2003, Post-collisional adakitic porphyries in Tibet: Geochemical and Sr-Nd-Pb isotopic constraints on partial melting of oceanic lithosphere and crust-mantle inter action. Acta Geologica Sinica, v.77, p.123-135.
Gao, S, Liu, X.M., Yuan, H.L., Hattendorf, B., Gunther, D., Chen, L., and Hu, S.H.,2002, Determination of forty two major and trace elements in USGS and NIST SRM glasses by laser ablation-inductively coupled plasma-mass spectrometry. Geostandards Newsletter, v.26, p. 181-195.
Gao, Y.F., Wei, R.H., Hou, Z.Q., Tian, S.H., Zhao, R.S.,2008, Eocene high-MgO volcanism in southern Tibet:New constraints for mantle source characteristics and deep processes. Lithos, v. 105, p.63-72.
Cathles, L.M., Guber, A.L., and Lenagh, T.C., et al.,1983, Kuroko-type massive sulfide deposits of Japan:Products of an aborted island arc rift. Economic Geology, v.78, p.96-114.
Gerstenberger, H., and Haase, G.,1997, A highly effective emitter substance for mass spectrometric Pb isotope ratio determinations. Chemical Geology, v.136, p.309-312.
Gilder, S.A., Keller, G.R., Luo, M., and Goodell, P.C.,1991, Timing and spatial distribution of rifting in China. Tectonophysics, v.197, p.225-243.
Gilder, S. A., Gill, J., Coe, R. S., Zhao, X., Liu, Z., and Wang, G.,1996, Isotopic and paleomagnetic constraints on the Mesozoic tectonic evolution of south China. Journal of Geophysical Research, v.101, p.16137-16154.
Gomez-Tuena A., Langmuir C.H., Goldstein S.L., et al.,2007, Geochemical Evidence for Slab Melting in theTrans-Mexican Volcanic Belt. Journal of Petrology, v.48, p.537-562.
Gutscher, M.A., Maury, R.., Eissen, J.P., and Bourdon, E.,2000, Can slab melting be caused by flat subduction? Geology, v.28, p.535-538.
Haeussler, P.J., Bradley, D., Goldfarb, R., Snee, L., and Taylor, C.,1995, Link between ridge subduction and gold mineralization in Southern Alaska. Geology, v.23, p.995-998.
Hall, D.L., Sterner, S.M., and Bodnar, R.J.,1988, Freezing point depression of NaCl-KCl-H2O solutions. Economic Geology, v.83, p.197-202.
Han, C.M., Xiao, W.J., Zhao, G.H., Mao, J.W., Yang, J.M., Wang, Z.L., Yan, Z., and Mao, Q.G.,
2006, Geological characteristics and genesis of the Tuwu porphyry copper deposit, Hami, Xinjiang, Central Asia. Ore Geology Reviews, v.29, p.77-94.
He, W., Zhengyu, B., Tieping, L.,1999, One-dimensional reactive transport models of alteration in the Tongchang porphyry copper deposit, Dexing district, Jiangxi Province, China. Economic Geology, v.94, p.307-323.
Hermann, J., and Spandler, C.,2008, Sediment melts at sub-arc depths:an experimental study. Journal of Petrology, v.49,717-740.
Hintenberger, W., Herr, W., and Voshage, H.,1954, Radiogenic osmium from rhenium-containing molybdenite. Phys Rev, v.95, p.1690-1694.
Hoskin, P.W.O.,2005, Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills, Australia. Geochimica et Cosmochimica Acta,69 (3): 637-648.
Hou, M.L., Jiang, Y.H., Jiang, S.Y., Ling, H.F., and Zhao, K.D.,2007, Contrasting origins of late Mesozoic adakitic granitoids from the northwestern Jiaodong Peninsula, east China: implications for crustal thickening to delamination. GeologicalMagazine, v.144, p.619-631.
Hou, Z.Q., Ma, H.W., Zaw,K., Zhang, Y.Q., Wang, M.J., Wang, Z., Pan, G.T., and Tang, R.L. 2003, The Himalayan Yulong porphyry copper belt:Produced by large-scale strike-slip faulting at eastern Tibet. Economic Geology, v.98, p.125-145.
Hou, Z.Q., Gao, Y.F., Qu, X.M., Rui, Z.Y., and Mo, X.X.,2004, Origin of adakitic intrusives generated during mid-Miocene east-west extension in southern Tibet. Earth and Planetary Science Letters, v.220, p.139-155.
Hou, Z.Q, Yang, Z.M., Qu, X.M., Meng, X.J., Li, Z.Q., Beaudoin, G., Rui, Z.Y., and Gao, Y.F., 2009. The Miocene gangdese porphyry Cu belt:Generated during post-collisional extension in the Tibetan orogen. Ore Geology Review, v.36, p.25-51.
Hou, Z.Q, Zhang, H.R., Pan, X.F., and Yang, Z.M.,2011, Porphyry Cu (-Mo-Au) deposits related to melting of thickened mafic lower crust:Examples from the eastern Tethyan metallogenic domain. Ore Geology Reviews, v.39, p.21-45.
Hu, F.F., Fan, H.R., Yang, J.H., et al,2004, Mineralizing age of the Rushan lode gold deposit in t he Jiaodong Peninsula:SHRIMP U-Pb dating on hydrothermal zircon. Chinese Science Bulletin, v.49, p.1629-1636.
Huang, F., Li, S.G., Dong, F., Li, Q.L., Chen, F.K., Wang, Y., and Yang, W.,2007, Recycling of deeply subducted continental crust in the Dabie Mountains, central China. Lithos, v.96:p. 151-169.
Imai, A., Listanco, E.L., and Fujii, T.,1993, Petrologic and sulfur isotopic significance of highly oxidized and sulfur-rich magma of Mount Pinatubo, Philippines. Geology, v.21, p.699-702.
Imai, A.,2002, Metallogenesis of porphyry Cu deposits of the western Luzon arc, Philippines: K-Ar ages, SO3 contents of microphenocrystic apatite and significance of intrusive rocks. Resource Geology, v.52, p.147-161.
Imai, A.,2004, Variation of Cl and SO3 contents of microphenocrystic apatite in intermediate to silicic igneous rocks of Cenozoic Japanese island arcs:Implications for porphyry Cu metallogenesis in the Western Pacific Island arcs. Resource Geology, v.54, p.357-372.
Ishihara, S.,1977, The magnetite-series and ilmentite-series granitic rocks. Mining Geology, v.27, p.293-305.
Isozaki Y.,1997, Jurassic accretion tectonics of Japan. The Island Arc, v.6, p.25-51.
Jackson, S.E., Pearson, N.J., Griffin, W.L. and Belousova, E.A.,2004, The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology. Chemical Geology, v.211:p.47-69.
Jahn, B.M., Zhou, X.H., and Li, J.L.,1990, Formation and tectonic evolution of southeastern China and Taiwan:Isotopic and geochemical constraints. Tectonophysics, v.183, p.145-160.
Jahn, B.M., Wu, F.Y., and Lo, C.H.,1999, Crust-mantle interaction induced by deep subduction of the continental crust:geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie Complex, Central China. Chemical Geology, v.157, p.119-146.
Jiang, Y.H., Ling, H.F., Jiang, S.Y., Fan, H.H., Shen, W.Z., and Ni, P.,2005, Petrogenesis of a Late Jurassic peraluminous volcanic complex and its high-Mg, potassic, quenched enclaves at Xiangshan, Southeast China. Journal of Petrology, v.46, p.1121-1154.
Jiang, Y.H., Jiang, S.Y., Zhao, K.D., Ling, H.F., and Dai, B.Z.,2006. Low-degree melting of a metasomatized lithospheric mantle for the origin of Cenozoic Yulong monzogranite-porphyry, east Tibet:Geochemical and Sr-Nd-Pb-Hf isotopic constraints. Earth and Planetary Science Letters, v.241:p.617-633.
Jiang, Y.H., Jiang, S.Y., Dai, B.Z., and Ling, H.F.,2008, Discrimination of ore-bearing and barren porphyries in the Yulong porphyry copper ore belt, east Tibet. International Geology Review, v. 50:p.583-595.
Jiang, Y.H., Jiang, S.Y., Dai, B.Z., Liao, S. Y., Zhao, K.D., and Ling, H.F.,2009, Middle to Late Jurassic felsic and mafic magmatism in southern Hunan Province, Southeast China: implications for a continental arc to rifting. Lithos, v.107, p.185-204.
Jiang, Y.H., Jin, G.D., Liao, S.Y., Zhou, Q., and Zhao, P.,2010a, Geochemical and Sr-Nd-Hf isotopic constraints on the origin of Late Triassic granitoids from the Qinling orogen, central China:implications for a continental arc to continent-continent collision. Lithos, v.117, p. 183-197.
Jiang, Y.H., Zhao, P., Zhou, Q., Liao, S.Y., and Jin, G.D.,2011, Petrogenesis and tectonic implications of Early Cretaceous S-and A-type granites in the northwest of the Gan-Hang rift, SE China. Lithos, v.121, p.55-73.
Jin, Z.D., Zhu, J.C., Ji, J.F., Lu, X.W., and Li, F.C.,2001, Ore-forming fluid constraints on illite crystallinity (IC) at Dexing porphyry copper deposit, Jiangxi Province. Science in China (Series D), v.44, p.177-184.
Jin, Z.D., Zhu, J.C., Ji, J.F., Li, F.C., and Lu, X.W.,2002, Two origins of illite at the Dexing porphyry Cu deposit, East China:implications for ore-forming fluid constraint on illite crystallinity. Clays and Clay Minerals, v.50, p.381-387.
Kay, R.W.J.,1978, Aleutian magnesium andesites:melts from subducted Pacific oceanic crust. Jour Volcan Geotherm Res, v,4, p.117-132.
Kay, S.M., Ramos, V.A., and Marquez, M.,1993, Evidence in Cerro Pampa volcanic rocks of slab melting prior to ridge trench collision in southern South America. Journal of Geology, v.101, p. 703-714.
Keleman, B.P.,1995, Genesis of high Mg# andesites and the continental crust. Contribute to Mineralogy and Petrology, v.120, p.1-19.
Kerrich R.,1993, Hydrothermal zircon and baddeleyite in Val-d'Or Archean mesothermal gold deposits:Characteristics, compositions, and fluid inclusion properties, wit h implications for timing of primary gold mineralization. Canadia Journal of Earth Sciences, v.30, p.2334-2351.
Kerich, R., Goldfarb, R., and Groves, D., et al.,2000, The characteristics, origins, and geodynamic settings of supergiant gold metallogenic provinces. Science in China, v.43, p.12-68.
Kirkham, R.V., and Sinclair, W.D.,1995, Porphyry copper, gold, molybdenum, tungsten, tin, silver. In:Eckstrand OR, Sinclair WD, Thorpe RI (eds) Geology of Canadian mineral deposit types. Geological Survey of Canada, Ottawa, p.421-446.
Lang, J.R., and Titley, S.R.,1998, Isotopic and geochemical characteristics of Laramide magmatic systems in Arizona and implications for the genesis of porphyry copper deposits. Economic Geology, v.93, p.138-170.
Lapierre, H., Jahn, B.M., Charvet, J.,1997. Mesozoic magmatism in Zhejiang Province and its relation with the tectonic activities in SE China. Tectonophysics, v.274, p.321-338.
Lee C.A.,2005. Trace Element Evidence for Hydrous Metasomatism at the Base of the North American Lithosphere and Possible Association with Laramide Low-Angle Subduction. The Journal of Geology, v.113, p.673-685.
Lepvrier, C., Maluski, H., Tich V.V., Leyerloup, A., Phan T.P., and Nguyen V.V.,2004, The Early Triassic Indosinian orogeny in Vietnam (Truong Son Belt and Kontum Massif: implications for the geodynamic evolution of Indochina. Tectonophysics, v.393, p.87-118.
Li, S.G., Chen, Y., Cong, B.L., Zhang, Z., Zhang, Y., Liou, D.L., Hart, S.A., and Ge, N.,1993, Collision of the North China and Yangtze Blocks and formation of coesite-bearing eclogites: timing and processes. Chemical Geology, v.109, p.80-89.
Li, X.F., and Sasaki, M.,2007, Hydrothermal Alteration and Mineralization of Middle Jurassic Dexing Porphyry Cu-Mo Deposit, Southeast China. Resource Geology, v.57, p.409-426.
Li, X.H., and McCulloch, M.T.,1996, Secular variation in the Nd isotopic composition of Neoproterozoic sediments from the southern margin of the Yangtze block:evidence for a Proterozoic continental collision in southeast China. Precambrian Research,v.76, p.67-76.
Li, X.H., Li, Z.X., Li, W.X., Liu, Y., Yuan, C., Wei, G., and Qi, C.,2007, U-Pb zircon, geochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I-and A-type granites from central Guangdong, SE China:A major igneous event in response to foundering of a subducted flat-slab? Lithos, v.96, p.186-204.
Li, X.H., Li, W.X., Wang, X.C., Li, Q.L., Liu, Y., Tang, G.Q., Gao, Y.Y., and Wu, F.Y.,2010, SIMS U-Pb zircon geochronology of porphyry Cu-Au-(Mo) deposits in the Yangtze River Metallogenic Belt, eastern China: Magmatic response to early Cretaceous lithospheric extension. Lithos,v.119, p.427-438.
Li, Z.X., and Li, X.H.,2007, Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China:a flat-slab subduction model. Geology, v.35:p.179-182.
Liang, H.Y., Sun, W.D., Su, W.C., and Zartman, R.E.,2009, Porphyry Copper-Gold Mineralization at Yulong, China, Promoted by Decreasing Redox Potential during Magnetite Alteration. Economic Geology, v.104, p.587-596.
Ling, M.X., Wang, F.Y., Ding, X., Hu, Y.H., Zhou, J.B., Zartman, R.E., Yang, X.Y., Sun, W.D., 2009. Cretaceous ridge subduction along the lower Yangtze River belt, eastern China. Economic Geology 104,303-321.
Livingston, D.E,1978, A plate tectonic hypothesis for the genesis of porphyry copper deposits of the southern Basin and Range Province. Earth Planetary Science Letters, v.20, p.171-179.
Lowell, J.D., and Gnilbert, J.M.,1970, Lateral and vertical alteration-mineralization zoning in porphyry ore deposits. Economic Geology, v.65, p.373-408.
Lu, J.J., Hua, R.M., Jiang, S.Y., Chen, X.M., and Gao, J.F.,2004. A study on copper isotope compositions of Dexing porphyry Cu-Au deposit of Jiangxi, China. Geochimica et Cosmochimica Acta, v.68, p. A302.
Ludwig, K.R.,1999, Isoplot/Ex, Version 2.0:A geochrological toolkit for Microsoft excel. Berkeley. Geochronology Center.
Ludwig, K.R.,2001, Using Isoplot/EX, version 2.49. In:A geolocronolgical toolkit for Microsoft excel, Berkeley Geochronological Center Special Publication, Berkeley, p.1-55.
Luhr, J.F.,1990, Experimental phase relations of water-and-sulfur-saturated arc magmas and the 1982 eruptions of El Chichon volcano. Journal of Petrology, v.31, p.1071-1114.
Mao J.W., Zhang Z.C., Zhang Z.H., and Du A.D.,1999, Re-Os isotopic dating of molybdenites in the Xiaoliugou W (Mo) deposit in the northern Qilian mountains and its geological significance. Geochimica et Cosmochimica Acta, v.63:p.1815-1818.
Mao, J.W., Xie, G.Q., Bierlein, F., Qu, W.J., Du, A.D., Ye, H.S., Pirajno, F., Li, H.M., Guo, B.J., Li, Y.F. and Yang, Z.Q.,2008,Tectonic implications from Re-Os dating of Mesozoic molybdenum deposits in the East Qinling-Dabie orogenic belt. Geochimica et Cosmochimica Acta, v.72:p.4607-4626.
Martin, H., Bonin, B., and Capdevila, R.,1994, The Kuiqi peralkaline granitic complex (SE China):petrology and geochemistry:Journal of Petrology, v.35, p.983-1015.
Martin, H., Smithies, R.H., Rapp, R., Moyen, J.F., and Champion, D.,2005, An overview of adakite, tonalite-trondhjemite-granodiorite (TTG), and sanukitoid:relationships and some implications for crustal evolution. Lithos, v.79, p.1-24.
Masterman, G.J., Cooke, D. R., Berry, R.F., Clark, A.H., Archibald, D.A., Mathur, R., Walshe, J.L., and Uuran, M.,2004, 40Ar/39Ar and Re-Os Geochronology of Porphyry Copper-Molybdenum Deposits and Related Copper-Silver Veins in the Collahuasi District, Northern Chile. Economic Geology, v.99:p.673-690.
Mathes, E.A.,1976, Sulfur solubility and magmatic sulfides in submarine basalt glass. Journal of Ceophyslell Research, v.81, p.4269-4276.
Mavrogenes, J.A., and O'Neill, H.S.C.,1999, The relative effects of pressure, temperature and oxygen fugacity on the solubility of sulfide in mafic magmas. Geochimica et Cosmochimica Aeta, v.63, p.1173-1180.
McDonough, W.F., and Sun, S.S.,1985, Isotopic and geochemical systematics in Tertiary-Recent basalts from southeastern Australia and implication for the sub-continental lithosphere. Geochimica et Cosmochimica Acta, v.49, p.2051-2067.
McInnes, B.I.A., and Cameron, E.M.,1994, Carbonated, alkaline hybridizing melts from a sub-arc environment:mantle wedge samples from the Tabar Lihir-tanga-Feni arc, Papua New Guinea. Earth and Planetary Science Letters, v.122, p.125-141.
Meyer, C., and Hemley, J.J.,1967, Wall rock alteration:in Geochemistry of Hydrothermal Ore Deposits. Barnes, H.L., ed., Holt, Rinehart and Winston, New York, p.166-235.
Mitchell, A.H.G., and Garson, M.S.,1972, Relationship of porphyry copper and circum-Pacific tin deposits to palaeo-Benioff zones. Institute of Mining and Metallurgy Transactions, v.81, p. B10-B25.
Mitchell, A. H. G.,1973, Metallogenic belt and angle of dip of Benioff zones. Nature, v.245, p. 49-52.
Mungall, J.E.,2002, Roasting the mantle:Slab melting and the genesis of major Au and Au-rich Cu deposits. Geology, v.30, p.915-918.
Mysen, B.O., and Popp, R.K.,1981, Solubility of sulfur in CaMgSi2O6 and NaAlSi3O8 melts at high pressure and temperature with controlled. American Journal of Science, v.280, p.78-92.
Oyarzun, R., Marquez, A., Lillo, J., Lopez, I., and Rivera, S.,2001, Giant versus small porphyry copper deposits of Cenozoic age in northern Chile. Adakitic versus normal calc-alkaline magmatism:Mineralium Deposita, v.36, p.794-798.
Oyarzun, R., Marquez, A., Lillo, J., Lopez, I., and Rivera, S.,2002, Reply to discussion on "Giant versus small porphyry copper deposits of Cenozoic age in northern Chile:Adakitic versus normal calc-alkaline magmatism" by Oyarzun, R., Marquez, A., Lillo, J., Lopez, I., and Rivera, S.,2001, Mineralium Deposita, v.36, p.794-798. Mineral Depos, v.37, p.795-799.
Pasteris, J.D.,1996, Mount Pinatubo volcano and "negative" porphyry copper deposits. Geology, v.24, p.1075-1078.
Patino Douce, A.E., Johnston, A.D.,1991, Phase equilibria and melt productivity in the pelitic system:implications for the origin of peraluminous granitoids and aluminous granulites. Contributions to Mineralogy and Petrology, v.107, p.202-218.
Pearce, J.A., and Norry, M.J.,1979, Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks. Contribution to Mineralogy and Petrology, v.69, p.33-47.
Pearce, J.A., Harris, N.B.W. and Tindle, A.G.,1984, Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology, v.25, p.956-983.
Pelleter, E., Cheilletz, A., Gasquet, D., Mouttaqi, A., Annich, M., Hakour, A.E., Deloule, E., and Feraud, G.,2007, Hydrothermal zircons:A tool for ion microprobe U-Pb dating of gold mineralization (Tamlalt-Menhouhou gold deposit-Morocco). Chemical Geology, v.245, p. 135-161.
Peng, G., Luhr, J.F., and MeGee, J.J.,1997, Factors control ling sulfur concentrations in volcanic apatite. American Mineralogist, v.82, p.1210-1224.
Peng, J.T., Zhou, M.F., Hu, R.Z., Shen, N.P., Yuan, S.D., Bi, X.W., Du, A.D., and Qu, W.J.,2006, Precise molybdenite Re-Os and mica Ar-Ar dating of the Mesozoic Yaogangxian tungsten deposit, central Nanling district, South China. Miner Deposita, v.41:p.661-669.
Perello, J.,1994, Geology, porphyry Cu-Au,and epithermal Cu-Au-Ag mineralization of the Tombuliato district, North Sulawesi, Indonesia. Jour Geochem Explor, v.50, p.221-256.
Petford, N. and Atherton, M.,1996, Na-rich partial melts from newly underplated basaltic crust: the Cordillera Blanca Batholith, Peru. Journal of Petrology, v.37, p.1491-1521.
Pettke T., Lee D.C., Halliday, A.N., Rea D.K.,2002, Radiogenic Hf isotopic compositions of continental eolian dust from Asia, its variability and its implications for seawater. Earth and Planetary Science Letters, v.202:p.453-464.
Pettke, T., Audetat, A., Schaltegger, U., and Heinrich, C.A.,2005, Magmatic-to-hydrothermal crystallization in the W-Sn mineralized Mole Granite (NSW, Australia) Part Ⅱ:Evolving zircon and thorite trace element chemistry. Chemical Geology, v.220, p.191-213.
Plank T., and Langmuir C.H.,1998, The chemical composition of subducting sediment and its consequences for the crust and mantle. Chemical Geology, v.145, p.325-394.
Polt, A., and Kerrich, R.,2002, Nd-isotope systematics of-2.7 Ga adakites, magnesian andesites, and arc basalts, Superior Province:evidence for shallow crustal recycling at Archean subduction zones. Earth and Planetary Science Letters, v.202, p.345-360.
Qiu, Y.M., Gao, S., McNaughton, N.J., Groves, D.I., and Ling, W.L.,2000, First evidence of N3.2 Ga continental crust in the Yangtze craton of South China and its implications for Archean crustal evolution and phanerozoic tectonics. Geology, v.28, p.11-14.
Qu X.M., Hou Z.Q., and Li, Y.G.,2004, Melt components derived from a subducted slab in late orogenic ore-bearing porphyries in the Gangdese copper belt, southern Tibetan plateau. Lithos, v.74, p.131-148.
Qu X.M., Hou Z.Q., Zaw, K., and Li, Y.G.,2007, Characteristics and genesis of Gangdese porphyry copper deposits in the southern Tibetan Plateau:Preliminary geochemical and geochronological results. Ore Geology Reviews, v.31, p.205-223.
Rapp, R.P., and Watson, E.B.,1995, Dehydration melting of metabasalt at 8-32 kbar:implications for continental growth and crust-mantle recycling. Journal of Petrology, v.36, p.891-931.
Ratschbacher, L., Hacker, B.R., Calvert, A, Webb, L.E., Grimmer, J.C., McWilliams, M.O., Ireland, T., Dong, S.W., and Hu, J.M.,2003, Tectonics of the Qinling (central China): Tectonostratigraphy, geochronology, and deformation history. Tectonophysics, v.366, p.1-53.
Reich, M., Parada, M.A,, Palacios C., et al. Adakite-like signature of Late Miocene intrusions at the Los Pelambres giant porphyry copper deposit in the Andes of central Chile:Metallogenic implications. Mineral Deposit,2003,38:876-885.
Richards, J.P.,2003, Tectono-magmatic precursors for porphyry Cu-(Mo-Au) deposit formation. Economic Geology, v.98, p.1515-1533.
Robb, L.,2005, Introduction to ore-forming process. Oxford:Blackwell, p.153-166.
Roedder, E.,1992, Fluid inclusion evidence for immiscibility in magmatic differentiation. Geochimica et Cosmochimica Aeta, v.56, p.5-20.
Sajona, F.G., Naury, R.C., Pubellier, M., Leterrier, J., Bellon, H. and Cotton, J.,2000, Magmatic source enrichment by slab-derived melts in a young post-collision setting, central Mindanao (Philippines). Lithos, v.54, p.173-206.
Schmidt, M.W., Vielzeuf, D., and Auzanneau, E.,2004, Melting and dissolution of subducting crust at high pressures:the key role of white mica. Earth and Planetary Science Letters, v.228, p.65-84.
Selby, D., and Creaser, R.A.,2001, Late and mid-Cretaceous mineralization in the northern Canadian Cordillera:constraints from Re-Os molybdenite dates. Economic Geology, v.96:p. 1461-1467.
Shimoda G., Tatsumi Y., Nohda S., Ishizakaa K., and Jahn B.M.,1998, Setouchi high-Mg andesites revisited:geochemical evidence for melting of subducting sediments. Earth and Planetary Science Letters. V.160, p.479-492.
Shimoda G., and Tatsumi Y.,1999, Generation of rhyolite magmas by melting of subducting sediments in Shodo-Shima island, Southwest Japan, and its bearing on the origin of high-Mg andesites. The Island Arc, v.8, p.383-392.
Shirey, S.B., and Walker R.J.,1995, Carius tube digestion for low-blank rhenium-osmium analyses. Analytical Chemistry, v.67:p.2136-2141
Sillitoe, R.H.,1972, A Plate Tectonic Model for the Origin of Porphyry Copper Deposits. Economic Geology, v.67, p.184-197.
Sillitoe, R.H.,1988, Epochs of intrusion-related copper mineralization in the Andes. Jour South Am Ear Sci, v.1, p.89-108.
Sillitoe, R.H.,1993, Gold-rich porphyry copper deposits: geological model and exploration implication. Mineral Deposit Modeling, Geological Association of Canada Special Paper, v.40, p.465-478.
Sillitoe, R.H.,1997, Characteristics and controls of the largest porphyry copper-gold and epithermal gold deposits in the circum-Pacific region. Australian Journal of Earth Sciences, v. 44, p.373-388.
Simon, A.C., Pettke, T., Candela, P.A., Piccoli, P.M., and Heinrich, C.A.,2004, Magnetite solubility and iron transport in magmatic-hydrothermal environments Geochimica et Cosmochimica Acta,2004, v.68, p.4905-4914.
Sisson, T.W., Ratajeski, K., Hankins, W.B., Glazner, A.F.,2005, Voluminous granitic magmas from common basaltic sources. Contributions to Mineralogy and Petrology, v.148, p.635-661.
Smith, R.E. and Smith, S.E.,1976, Comments on the use of Ti, Zr, Y, Sr, K, P and Na in classification of basaltic magmas. Earth and Planetary Science Letters, v.32, p.114-120.
Smoliar, M.I., Walker, R.J., and Morgan, J.W.,1996, Re-Os ages of group IIA, IIIA, IVA and VIB iron meteorites. Science, v.271, p.1099-1102.
Solomon,1990, Subduction, arc reversal, and the origin of porphyry copper-gold deposits in island arcs. Geology, v.18, p.630-633.
Stein, H.J., Markey, R.J., Morgan, J.W., Du, A., and Sun, Y.,1997, Highly Precise and Accurate Re-Os Ages for Molybdenite from the East Qinling Molybdenum Belt, Shanxi Province, China. Economic Geology, v.92, p.827-835.
Streck, M.J., and Dilles, J.H.,1998, Sulfur evolution of oxidized arc magmas as recorded in apatite from a porphyry copper batholith. Geology, v.26, p.523-526.
Sun, W.D., Arculus, R.J., Kamenetsky, V.S., and Binns, R.A.,2004, Release of gold-bearing fluids in convergent margin magmas prompted by magnetite crystallization:Nature, v.431, p. 975-978.
Sun W.D., Ding X., and Hu Y.H.,2007, The golden transformation of the Cretaceous plate subduction in the west Pacific. Earth and Planetary Science Letters, v.262, p.533-542.
Sun, W.D., Ling, M.X., Yang, X.Y., Fan, W.M., Ding, X., Liang, H.,2010. Ridge subduction and porphyry copper-gold mineralization:an overview. Science China Series Dearth Science 53, 475-484.
Tarkian, M., and Stribrny, B.,1999, Platinum-gToup dements in porphyry copper deposit, a reconnaissance study. Mineralogy and Petrology, v.65, p.161-183.
Tatsumi, Y.,1986, Formation of the volcanic from:in sumuction zones. Geophysical Research Letters, v.17, p.717-720.
Tatsumi Y,2001, Geochemical modeling of partial melting of subducting sediments and subsequent melt-mantle interaction:Generation of high-Mg andesites in the Setouchi volcanic belt, southwest Japan. Geological Society of America, v.29, p.323-326.
Todt W., Cliff R.A., and Hanser A.,1996, Evaluation of a 202Pb-205Pb double spike for high-precision lead isotope analyses. Geophys. Monogr., v.95, p.429-437.
Tosdal, R.M., Richards, J.P.,2001, Magmatic and structural controls on the development of porphyry Cu±Mo±Au deposits. In:Richards JP, Tosdal RM (eds) Structural controls on ore genesis. Reviews in Economic Geology, v.14, p.157-181.
Uyeda, S., and Kanamori, H.,1979, Back-arc opening and the model of subduction. Journal of Geophysical Research, v.84, p.1040-1061.
Valencia, V.A., Ruiz, J., and Barra, F.,2005, U-Pb zircon and Re-Os molybdenite geochronology from La Caridad porphyry copper deposit: Insights for the duration of magmatism and mineralization in the Nacozari district, Sonora, Mexico. Mineralium Deposita, v.40, p. 175-191.
Vervoort, J.D., Blichert-Toft, J., Patchett, P.J., and Albarede, F.,1999, Relationships between Lu-Hf and Sm-Nd isotopic systems in the global sedimentary system. Earth and Planetary Science Letters, v.168, p.79-99.
Wang, Q., Xu, J.F., Jian, P., Bao, Z.W., Zhao, Z.H., Li, C.F., Xiong, X.L., and Ma, J.L.,2006, Petrogenesis of Adakitic Porphyries in an Extensional Tectonic Setting, Dexing, South China: Implications for the Genesis of Porphyry Copper Mineralization. Journal of Petrology, v.47, p. 119-144.
Watson, E.B., Cherniak, D.J., Hanchar, J.M., Harrison, T.M. and Wark, D.A.,1997, The incorporation of Pb into zircon. Chemical Geology, v.141, p.19-31.
Wendlandt, R.F.,1982, Sulfur saturation of basalt and andesite melts at high pressures and temperatures. American Mineralogist, v.67, p.877-885.
Whitney, J.A., and Stomer, J.C.,1983, Igneous sulfides in the Fish canyon tuff and the role of S in calc-alkaline. Geology, v.11, p.99-102.
Whitney, J.A.,1984, Fugacities of sulfurous gases in pyrrhotite-bearing magmas. American Mineralogist, v.60, p.69-78.
Williams, I.S., Buick, A., and Cartwright, I.,1996, An extended episode of early Mesoproterozoic metamorphic fluid flow in the Reynold Region, central Australia. Journal of Metamorphic Geology, v.14, p.29-47.
Winchester, J.A. and Floyd, P.A.,1977, Geochemical discrimination of different magma series and their differentiation products using immobile elements:Chemical Geology,20, p.325-343.
Wu, F.Y., Yang, Y.H., Xie, L.W. Yang, J.H., and Xu, P.,2006, Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology. Chemical Geology, v.234:p. 105-126.
Wyman, D.A., Ayer, J.A., and Devaney, J.R.,2000, Niobium-enriched basalts from the Wabigoon subprovince, Canada:evidence for adakitic metasomatism above an Archean subduction zone. Earth and Planetary Science Letters, v.179, p.21-30.
Xiong, Y.L., and Wood, S.A.,2001, Hydrothermal transport and deposition of rhenium under subcritical conditions (up to 200℃) in light of experimental studies. Economic Geology, v.96, p.1429-1444.
Xiong, Y.L., and Wood, S.A.,2002, Hydrothermal solubility of ReS2 and the Re-ReO2 buffer assemblage and transport of rhenium under supercritical conditions. Geochemical Transactions, v.3, p.1-10.
Xiong, Y.L., Wood, S.A., and Kruszewski J,2006, Hydrothermal transport and deposition of Rhenium under subcritical conditions revisited. Economic Geology, v.101, p.471-478
Xu, J.F., Shinjo, R., Defant, M.J., Wang, Q., and Rapp, R.P.,2002, Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China:partial melting of delaminated lower continental crust. Geology, v.30, p.1111-1114.
Yao J.M., Hua R.M., Qu W.J., Qi H.R., Lin J.F., and Du A.D.,2007, Re-Os isotope dating of molybdenites in the Huangshaping Pb-Zn-W-Mo polymetallic deposit, Hunan province, South China and its geological significance. Science in China (Series D), v.50, p.519-526.
Yan, M.Z., and Hu, K.,1980, Geological characteristics of the Dexing porphyry copper deposits, Jiangxi, China. Mining Geology, Special Issue v.8, p.197-203.
Yogodzinski G. M., Kay R. W., Volynets O. N., and Koloskov A. V.,1995, Magnesian andesite in the western Aleutian Komandorsky region:Implications for slab melting and processes in the mantle wedge. GSA Bulletin, v.107, p.505-519.
Zartman, R.E., and Doe, B.R.,1981, Plumb tectonics-The model tectonophys. Tectonophys, v.75, p.125-177.
Zaw K., Peters S.G., Cromie P., et al.,2007, Nature, diversity of deposit types and metallogenic relations of South China. Ore Geology Reviews, v.31, p.3-47.
Zhai, Y., Deng, J., and Peng, R.,1997, Some major mineral deposits in China:their tectonic setting and deposit model characteristics. Proceeding,30th International Geology Congress, v.9, p.367-379.
Zhang, Z.M., Hou, Z.Q., White, N.C., Chang, Z.S., Li, Z.Q., and Song, Y.C.,2009, Geology of the post-collisional porphyry copper-molybdenum deposit at Qulong, Tibet. Ore Geology Reviews, v.36, p.133-159.
Zhang, S.B., Zheng, Y.F., Wu, Y.B., Zhao, Z.F, Gao, S., and Wu, Y.,2006, Zircon U-Pb age and Hf-O isotope evidence for Paleoproterozoic metamorphic event in South China. Precambrian Research, v.151:p.265-288.
Zhang, S.B., Zheng, Y.F., Zhao, Z.F., Wu, Y.B., Yuan, H.L., and Wu, F.Y.,2008, Neoproterozoic anatexis of Archean lithosphere:Geochemical evidence from felsic to mafic intrusions at Xiaofeng in the Yangtze Gorge, South China. Precambrian Research, v.163:p.210-238.
Zhang S.B., Zheng Y.F., Zhao Z.F., Wu Y.B., Yuan H.L., and Wu, F.Y.,2009, Origin of TTG-like rocks from anatexis of ancient lower crust:Geochemical evidence from Neoproterozoic granitoids in South China. Lithos, v.113:p.347-368.
Zhou, J.X.,1999, Geochemistry and petrogenesis of igneous rocks containing amphibole and mica: A case study of plate collision involving Scotland and Himalayas. New York and Beijing, Science Press, p.41-72.
Zhou, X.M., and Li, W.X.,2000, Origin of Late Mesozoic igneous rocks in Southeastern China: implications for lithosphere subduction and underplating of mafic magmas. Tectonophysics, v. 326:p.269-287.
Zhou, X.M., Sun, T., Shen, W.Z., Shu, L.S., and Niu, Y.L.,2006, Petrogenesis of Mesozoic granitoids and volcanic rocks in South China:a response to tectonic evolution. Episodes, v.29, p.26-33.
陈江峰,郭新生,汤加富,等,1999,中国东南地壳增长与Nd同位素模式年龄.南京大学学报,(自然科学),v.35,p.649-658.
陈民扬,李耀菘,1997,铜矿床同位素地球化学.北京：科学出版社,p.376-378.
陈志广,张连昌,吴华英,等,2008,内蒙古西拉木伦成矿带碾子沟钼矿区A型花岗岩地球化学和构造背景.岩石学报,v.24,p.879-889.
代军治,毛景文,杜安道,等,辽西肖家营子钼(铁)矿床Re-Os年龄及其地质意义.地质学报,2007,v.81,p.917-923.
邓晋福,赵海玲,莫宣学,等,1995,扬子大陆的陆内俯冲与大陆换缩小-由白云母(二云母)花岗岩推导.高校地质学报,v.1,p.50-57.
杜安道,何红蓼,殷宁万,等,1994,辉钼矿的铼—锇同位素地质年龄测定方法研究.地质学报,v.66,p.339-347.
杜安道,赵敦敏,王淑贤,等,2001, Carius管溶样-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,v.20,p.247-252.
丰成友,许建祥,曾载淋,等,2007a,赣南天门山—红桃岭钨锡矿田成岩成矿时代精细测定及其地质意义.地质学报,v.81,p.952-963.
丰成友,丰耀东,许建祥,等,2007b,赣南张天堂地区岩体型钨矿晚侏罗世成岩成矿的同位素年代学证据.中国地质,v.34,p.642-650.
高剑峰,陆建军,赖鸣远,等,2003,岩石样品中微量元素的高分辨率等离子质谱分析.南京大学学报(自然科学),v.39,p.844-850.
郭新生,季克俭,黄耀生,等,1999,德兴斑岩铜矿成矿热液来源及其演化——花岗闪长斑岩的氧同位素制约.高校地质学报,v.5,p.260-268
侯可军,李延河,邹天人,等,2007, LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报,23(10)：2595-2604.
侯增谦,曲晓明,王淑贤,等,2003,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),v.33,p.609-618.
侯增谦,2004.斑岩Cu-Mo-Au矿床：新认识与新进展.地学前缘,v.11,p.131-144.
华仁民,李晓峰,陆建军,等,2000,德兴大型铜金矿集区构造环境和成矿流体研究进展.地球科学进展,v.15,p.525-533.
华仁民,陈培荣,张文兰,等,2003,华南中、新生代与花岗岩类有关的成矿系统.中国科学(D辑),v.33,p.335-343.
华仁民,陈培荣,张文兰,等,2005,论华南地区中生代3次大规模成矿作用.矿床地质.v.24,p.99-107.
黄典豪,吴澄宇,聂凤军,1987,陕西金堆城斑岩钼矿床地质特征及成因探讨·矿床地质,v.6,p. 22-34.
黄典豪,吴澄宇,杜安道,等,1994,东秦岭地区钼矿床的铼-锇同位素年龄及其意义.矿床地质,v.13,p.221-230.
黄定堂,2003,灵山岩体演化特征及其与稀有金属的成矿关系.地质与勘探,v.39,p.35-40.
季克俭,吴学汉,张国柄,1989,热液矿床的矿源、水源和热源及矿床分布规律.北京,北京科学技术出版社.
蒋少涌,赵葵东,姜耀辉,等,2008,十杭带湘南-桂北段中生代A型花岗岩带成岩成矿特征及成因讨论.高校地质学报.v.14,p.496-509.
金章东,朱金初.1998,关于德兴斑岩铜矿成矿物质来源—与梁祥济研究员商榷.地质论评,v.44,p.464-469.
金章东,朱金初,李福春,2002,德兴斑岩铜矿成矿过程的氧、锶、钕同位素证据.矿床地质,v.21,p.342-350.
李红艳,毛景文,孙亚莉,等,1996,柿竹园钨多金属矿床的Re-Os同位素等时线年龄研究.地质论评,v.42,p.261-267.
李晓峰,Watanabe Y,华仁民,等,2008,华南地区中生代Cu-(Mo)-W-Sn矿床成矿作用与洋岭／转换断层俯冲.地质学报,v.82,p.625-640.
李永峰,毛景文,刘敦一,等,2006,豫西雷门沟斑岩钼矿SHRIMP锆石U-Pb和辉钼矿Re-Os测年及其地质意义.地质论评,v.52,p.122-131.
梁华英,孙卫东,苏文超,等,2009,斑岩型铜(金)矿床成矿元素大规模堆积制约机制研究.矿物学报,v.S1,p.182-183
梁祥济,1995,江西德兴斑岩铜矿成矿物质来源的实验研究.地质论评,v.41,p.463-471.
刘姤群,杨世义,张秀兰,等.1983,德兴斑岩铜矿斑岩和围岩蚀变特征及斑岩和成矿物质来源的讨论.中国地质科学院宜昌地质矿产研究所所刊,v.7,p.77-95.
卢树东,高文亮,汪石林,等,2005,江西张十八铅锌矿铅同位素组成特征及其成因意义.矿物岩石,v.25,p.64-69.
毛景文,胡瑞忠,陈毓川,等,2006,大规模成矿作用与大型矿集区.北京：地质出版社,p.1-1030.
聂凤军,张万益,杜安道等.2007,内蒙古小东沟斑岩型钼矿床辉钼矿铼-锇同位素年龄及地质意义.地质学报,v.81,p.898-905.
钱鹏,陆建军,姚春亮,2003,德兴斑岩铜矿成矿流体演化与来源的流体包裹体研究.南京大学学报(自然科学),v.39,p.319-326.
钱鹏,陆建军,刘风香,2006,江西德兴斑岩铜矿成矿物质来源同位素示踪.世界地质,v.25,p.135-140.
秦克章,李光明,赵俊兴,等,2008,西藏首例独立钼矿——冈底斯沙让大型斑岩钼矿的发现及其意义.中国地质,v.35,p.1101-1112.
芮宗瑶,黄崇轲,齐国明,等,1984,中国斑岩铜(钼)矿床.北京：地质出版社,p.1-140.
芮宗瑶,张洪涛,陈仁义,等,2006,斑岩铜矿研究中若干问题探讨.矿床地质,v.25,p.491-500.
唐仁鲤,罗怀松,1995,西藏玉龙斑岩铜(钼)矿带地质.北京：地质出版社,p.1-310.
王德滋,沈渭洲,2003,中国东南部花岗岩成因与地壳演化.地学前缘,v.10,p.209-220.
王强,赵振华,简平,等,2004,德兴花岗闪长斑岩SHRIMP锆石U-Pb年代学和Nd-Sr同位素地球化学.岩石学报,v.20,p.315-324.
王永磊,裴荣富,李进文,等,2009,湘东南将军寨钨矿花岗岩地球化学特征及铼-锇同位素定年.岩矿测试,v.28,p.274-278.
吴澄宇,刘孝善,1989,南泥湖钼(钨)矿化花岗岩体的成因特征·南京大学学报.v.25,p.333-346.
徐夕生,谢听,2005,中国东南部晚中生代—新生代玄武岩与壳幔作用,高校地质学报,v.11,p.318-334.
姚春亮,2006,德兴斑岩铜矿含矿岩体特征和矿化机制.博士论文,p.1-89.
姚军明,华仁民,屈文俊,等,2007,湘南黄沙坪铅锌钨钼多金属矿床辉钼矿的Re-Os同位素定年及其意义.中国科学(D辑),v.37,p.471-477.
叶会寿,毛景文,李永峰,等,2006,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.地质学报,v.80,p.1078-1088.
叶松,叶德隆,莫宣学,等.深源岩浆作用与江西德兴大型矿集区成矿关系.高校地质学报.1999,5(4)：395-404.
曾载淋,张永忠,朱详培,等,2009,赣南崇义地区茅坪钨锡矿床铼-锇同位素定年及其地质意义.岩矿测试,v.28,p.209-214.
张洪涛,陈仁义,韩芳林,2004,重新认识中国斑岩铜矿的成矿地质条件.矿床地质,v.23,p.
150-163.
张理刚,1992,铅同位素地质研究现状及展望.地质与勘探,v.28,p.21-29.
张理刚,刘敬秀,陈振胜,等,1996,江西德兴铜厂铜矿水-岩体系氢氧同位素演化.地质科学,v.31,p.250-263.
张振亮,2003,德兴铜厂铜矿非常温常压条件下的流体包裹体拉曼光谱特征及其成矿意义.硕士论文,p.1-98.
张作伦,曾庆栋,屈文俊,等,2009,内蒙碾子沟钼矿床辉钼矿Re-Os同位素年龄及其地质 意义.岩石学报,v.25,p.212-218.
周珂,叶会寿,毛景文,等,2009,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.矿床地质,v.28,p.170-184.
周耀华,梅占魁,王传松,等,1981,德兴斑岩铜矿物质来源之刍议.江西地质科技,v.1,p.32-41.
朱金初,沈渭洲,刘昌实,等,1990,华南中生代同熔系列花岗岩类的Nd-Sr同位素特征及成因讨论.岩石矿物学杂志,v.9,p.97-104.
朱金初,金章东,饶冰,等,2002,德兴铜厂斑岩铜矿流体过程.南京大学学报(自然科学),v.38,p.418-434.
朱训,黄崇轲,芮宗瑶,等,1983,德兴斑岩铜矿.北京：地质出版社,p.1-336.
朱永峰,宋彪,2006,新疆天格尔糜棱岩化花岗岩的岩石学及其SHRIMP年代学研究：兼论花岗岩中热液锆石边的定年.岩石学报,v.22,p.135-144.
Alt, J.C.B., and Urdett, J.W.,1992, Sulphur in Pacific deep-sea sediments (Leg 129) and implications for cycling of sediment in subduction zones. Proceedings ODP Science Research, v.129, p.283-294.
Andersen, T.,2002, Correction of common Pb in U-Pb analyses that do not report 204Pb. Chemical Geology, v.192, p.59-79.
Barra, F., Ruiz, J., Valencia V.A., Ochoa-Landin, L., Chesley, J.T., and Zurcher, L.,2005, Laramide Porphyry Cu-Mo Mineralization in Northern Mexico:Age Constraints from Re-Os Geochronology in Molybdenite. Economic Geology, v.100, p.1605-1616.
Barry, T. L., Saunders, A. D., Kempton, P. D., Windley, B. F., Pringle, M. S., Dorjnamjaa, D., and Saandar, S.,2003, Petrogenesis of Cenozoic basalts from Mongolia:Evidence for the role of asthenospheric versus metasomatized lithospheric mantle sources. Journal of Petrology, v.44, p. 55-91.
Black, L.P. and Gulson, B.L.,1978, The age of the Mud Tank carbonatite, Strangways Range, Northern Territory. BMR Journal of Australian Geology and Geophysics, v.3, p.227-232.
Blichert-Toft, J., and Albarede, F.,1997, The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system. Earth and Planetary Science Letters, v.148, p.243-258.
Bodnar, R.J.,1993, Revised equation and table for determining the freezing point depression of H2O-NaCl solutions. Geochimica et Cosmochimica Aeta, v.57, p.683-684.
Bourdon, E., Eissen, J.P., Monzier, M., Robin, C., Martin, H., Cotton, J., and Hall, M.L.,2002, Adakite-like lavas from Antisana volcano (Ecuador):evidence for slab melt metasomatism beneath the Andean Northern Volcanic Zone. Journal of Petrology, V.43, p.199-217.
Boynton, W.V.,1984, Cosmochemistry of the earth elements. meteorite studies. In:Henderson, R. (ed.) Rare Earth Element Geochemistry. Developments in Geochemistry 2, Amsterdam, Elsevier, p.89-92.
Burnham, C.W., and Ohmoto, H.,1980, Late-stage processes of felsic magmatism. Mining Geology Special Issue, v.8, p.1-11.
Carroll, M., and Rutherford, M.J.,1985, Sulfide and sulfate saturation hydrous silicate melts. Journal of Geophysics, v.90, p. C601-C612.
Carroll, M., and Rutherford, J.M.,1987, The stability of igneous anhydrite experimental results and implications for sulfur behavior in the 1982 El Chichon trachyandesite and other evolved magmas., Journal of Petrology, v.28, p.781-801.
Carter, A., Roques, D., Bristow, C., and Kinny, P.,2001, Understanding Mesozoic accretion in Southeast Asia:Significance of Triassic thermotectonism (Indosinian orogeny) in Vietnam. Geology, v.29, p.211-214.
Charvet, J., Lapierre, H., and Yu, Y.,1994, Geodynamic significance of the Mesozoic volcanism of southeastern China. Journal of Southeast Asian Earth Sciences, v.68, p.387-396.
Chaussidon, M., Albarede, F., and Sheppard, S.M.F.,1987, Sulphur isotope heterogeneity in the mantle from ion microprobe measurements of sulphide inclusions in diamond, Nature, v.330, p. 242-244.
Chaussidon, M., Albarede, F., and Sheppard, S.M.F.,1989, Sulphur isotope variation in the mantle from ion microprobe analyses of mic-sulphide inclusion. Earth Planet. Sci. Lett., v.92, p. 144-156.
Chaussidon, M., and Lorand, J.P.,1990, Sulphur isotope composition of orogenic spinel lherzolite massifs from Ariege (North-Eastern Pyrenees, France):an ion microprobe study. Geochim. Cosmochim. Acta, v.54, p.2835-2846.
Chen, J.F.& Jahn, B.M.,1998, Crustal evolution of Southeast China:Nd and Sr isotopic evidence. Tectonophysics, v.284, p.101-133.
Chiaradia, M., Vallance, J., Fontbote, L., Stein, H., Schaltegger, U., Coder, J., Richards, J., Villeneuve, M., and Gendall,I.,2009, U-Pb, Re-Os, and 40Ar/39Ar geochronology of the Nambija Au-skarn and Pangui porphyry Cu deposits, Ecuador:implications for the Jurassic metallogenic belt of the Northern Andes. Miner Deposita, v.44, p.371-387.
Claoue-Long, J.C., King, R.W., Kerrich, R.,1990, Archaean hydrothermal zircon in the Abitibi greenstone belt:Constraintson the timing of gold mineralization. Earth and Planetary Science Letters, v.98, p.109-128.
Condie, K.C.,1976, Plate Tectonics and Crustal Evolutionsecond ed:Pergamon Press, New York.
Cooke, D.R., Hollings, P., and Walsh, J.L.,2005, Giant porphyry deposits:Characteristics, distribution, and tectonic controls. Economic Geology, v.100, p.801-818.
Defant, M.J., and Drummond, M.S.,1990, Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, v.347, p.662-665.
de Hoog, J.C.M., Mason, P.R.O., and van Bergen, M,J,,2001, Sulfur and chalcophile elements in Subduction zones:Constraint from a laser ablation ICP-MS study of melt inclusions from Galunggung volcano, Indonesia. Geochimica et Cosmochimica Aeta, v.65, p.3147-3167.
Dubinska, E., Bylina, P., Kozlowski, A., Dorr, W., Nejbert, K., Schastok, J., and Kulicki, C.,2004, U-Pb dating of serpentinization:hydrothermal zircon from a metasomatic rodingite shell (Sudetic ophiolite, SW Poland). Chemical Geology, v.203, p.183-203.
Eldridge, C.S., Compston, W., Williams, I.S., Harris, J.W., and Bristow, J.W.,1991, Isotopic evidence for the involvement of recycled sediments in diamond formation. Nature, v.353, p. 649-653.
Force, E.R.,1998, Laramide alteration of Proterozoic diabase:A likely contributor of copper to porphyry systems in the Dripping Spring mountains area, southeastern Arizona. Economic Geology, v.93, p.171-183.
Fu, B., Mernagh, T.P., Kita, N.T., Kemp, A.I.S., and Valley, J.W.,2009, Distinguishing magmatic zircon from hydrothermal zircon:A case study from the Gidginbung high-sulphidation Au-Ag-(Cu) deposit, SE Australia. Chemical Geology 259 (2009) 131-142.
Gammons, C.H., Bloom, M.S., and Yu, Y.,1992, Experimental investigation of the hydrothermal geochemistry platinum and palladium,1, Solubility of platinum and palhdlum sulphide minerals in NaCl/H2SO4 solutions at 300℃. Geochimica et Cosmochimica Aeta, v.56, p.3881-3894.
Gao, Y.F., Hou, Z.Q., and Wei, R.H.,2003, Post-collisional adakitic porphyries in Tibet: Geochemical and Sr-Nd-Pb isotopic constraints on partial melting of oceanic lithosphere and crust-mantle inter action. Acta Geologica Sinica, v.77, p.123-135.
Gao, S, Liu, X.M., Yuan, H.L., Hattendorf, B., Gunther, D., Chen, L., and Hu, S.H.,2002, Determination of forty two major and trace elements in USGS and NIST SRM glasses by laser ablation-inductively coupled plasma-mass spectrometry. Geostandards Newsletter, v.26, p. 181-195.
Gao, Y.F., Wei, R.H., Hou, Z.Q., Tian, S.H., Zhao, R.S.,2008, Eocene high-MgO volcanism in southern Tibet:New constraints for mantle source characteristics and deep processes. Lithos, v. 105, p.63-72.
Cathles, L.M., Guber, A.L., and Lenagh, T.C., et al.,1983, Kuroko-type massive sulfide deposits of Japan:Products of an aborted island arc rift. Economic Geology, v.78, p.96-114.
Gerstenberger, H., and Haase, G.,1997, A highly effective emitter substance for mass spectrometric Pb isotope ratio determinations. Chemical Geology, v.136, p.309-312.
Gilder, S.A., Keller, G.R., Luo, M., and Goodell, P.C.,1991, Timing and spatial distribution of rifting in China. Tectonophysics, v.197, p.225-243.
Gilder, S. A., Gill, J., Coe, R. S., Zhao, X., Liu, Z., and Wang, G.,1996, Isotopic and paleomagnetic constraints on the Mesozoic tectonic evolution of south China. Journal of Geophysical Research, v.101, p.16137-16154.
Gomez-Tuena A., Langmuir C.H., Goldstein S.L., et al.,2007, Geochemical Evidence for Slab Melting in theTrans-Mexican Volcanic Belt. Journal of Petrology, v.48, p.537-562.
Gutscher, M.A., Maury, R.., Eissen, J.P., and Bourdon, E.,2000, Can slab melting be caused by flat subduction? Geology, v.28, p.535-538.
Haeussler, P.J., Bradley, D., Goldfarb, R., Snee, L., and Taylor, C.,1995, Link between ridge subduction and gold mineralization in Southern Alaska. Geology, v.23, p.995-998.
Hall, D.L., Sterner, S.M., and Bodnar, R.J.,1988, Freezing point depression of NaCl-KCl-H2O solutions. Economic Geology, v.83, p.197-202.
Han, C.M., Xiao, W.J., Zhao, G.H., Mao, J.W., Yang, J.M., Wang, Z.L., Yan, Z., and Mao, Q.G.,
2006, Geological characteristics and genesis of the Tuwu porphyry copper deposit, Hami, Xinjiang, Central Asia. Ore Geology Reviews, v.29, p.77-94.
He, W., Zhengyu, B., Tieping, L.,1999, One-dimensional reactive transport models of alteration in the Tongchang porphyry copper deposit, Dexing district, Jiangxi Province, China. Economic Geology, v.94, p.307-323.
Hermann, J., and Spandler, C.,2008, Sediment melts at sub-arc depths:an experimental study. Journal of Petrology, v.49,717-740.
Hintenberger, W., Herr, W., and Voshage, H.,1954, Radiogenic osmium from rhenium-containing molybdenite. Phys Rev, v.95, p.1690-1694.
Hoskin, P.W.O.,2005, Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills, Australia. Geochimica et Cosmochimica Acta,69 (3): 637-648.
Hou, M.L., Jiang, Y.H., Jiang, S.Y., Ling, H.F., and Zhao, K.D.,2007, Contrasting origins of late Mesozoic adakitic granitoids from the northwestern Jiaodong Peninsula, east China: implications for crustal thickening to delamination. GeologicalMagazine, v.144, p.619-631.
Hou, Z.Q., Ma, H.W., Zaw,K., Zhang, Y.Q., Wang, M.J., Wang, Z., Pan, G.T., and Tang, R.L. 2003, The Himalayan Yulong porphyry copper belt:Produced by large-scale strike-slip faulting at eastern Tibet. Economic Geology, v.98, p.125-145.
Hou, Z.Q., Gao, Y.F., Qu, X.M., Rui, Z.Y., and Mo, X.X.,2004, Origin of adakitic intrusives generated during mid-Miocene east-west extension in southern Tibet. Earth and Planetary Science Letters, v.220, p.139-155.
Hou, Z.Q, Yang, Z.M., Qu, X.M., Meng, X.J., Li, Z.Q., Beaudoin, G., Rui, Z.Y., and Gao, Y.F., 2009. The Miocene gangdese porphyry Cu belt:Generated during post-collisional extension in the Tibetan orogen. Ore Geology Review, v.36, p.25-51.
Hou, Z.Q, Zhang, H.R., Pan, X.F., and Yang, Z.M.,2011, Porphyry Cu (-Mo-Au) deposits related to melting of thickened mafic lower crust:Examples from the eastern Tethyan metallogenic domain. Ore Geology Reviews, v.39, p.21-45.
Hu, F.F., Fan, H.R., Yang, J.H., et al,2004, Mineralizing age of the Rushan lode gold deposit in t he Jiaodong Peninsula:SHRIMP U-Pb dating on hydrothermal zircon. Chinese Science Bulletin, v.49, p.1629-1636.
Huang, F., Li, S.G., Dong, F., Li, Q.L., Chen, F.K., Wang, Y., and Yang, W.,2007, Recycling of deeply subducted continental crust in the Dabie Mountains, central China. Lithos, v.96:p. 151-169.
Imai, A., Listanco, E.L., and Fujii, T.,1993, Petrologic and sulfur isotopic significance of highly oxidized and sulfur-rich magma of Mount Pinatubo, Philippines. Geology, v.21, p.699-702.
Imai, A.,2002, Metallogenesis of porphyry Cu deposits of the western Luzon arc, Philippines: K-Ar ages, SO3 contents of microphenocrystic apatite and significance of intrusive rocks. Resource Geology, v.52, p.147-161.
Imai, A.,2004, Variation of Cl and SO3 contents of microphenocrystic apatite in intermediate to silicic igneous rocks of Cenozoic Japanese island arcs:Implications for porphyry Cu metallogenesis in the Western Pacific Island arcs. Resource Geology, v.54, p.357-372.
Ishihara, S.,1977, The magnetite-series and ilmentite-series granitic rocks. Mining Geology, v.27, p.293-305.
Isozaki Y.,1997, Jurassic accretion tectonics of Japan. The Island Arc, v.6, p.25-51.
Jackson, S.E., Pearson, N.J., Griffin, W.L. and Belousova, E.A.,2004, The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology. Chemical Geology, v.211:p.47-69.
Jahn, B.M., Zhou, X.H., and Li, J.L.,1990, Formation and tectonic evolution of southeastern China and Taiwan:Isotopic and geochemical constraints. Tectonophysics, v.183, p.145-160.
Jahn, B.M., Wu, F.Y., and Lo, C.H.,1999, Crust-mantle interaction induced by deep subduction of the continental crust:geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie Complex, Central China. Chemical Geology, v.157, p.119-146.
Jiang, Y.H., Ling, H.F., Jiang, S.Y., Fan, H.H., Shen, W.Z., and Ni, P.,2005, Petrogenesis of a Late Jurassic peraluminous volcanic complex and its high-Mg, potassic, quenched enclaves at Xiangshan, Southeast China. Journal of Petrology, v.46, p.1121-1154.
Jiang, Y.H., Jiang, S.Y., Zhao, K.D., Ling, H.F., and Dai, B.Z.,2006. Low-degree melting of a metasomatized lithospheric mantle for the origin of Cenozoic Yulong monzogranite-porphyry, east Tibet:Geochemical and Sr-Nd-Pb-Hf isotopic constraints. Earth and Planetary Science Letters, v.241:p.617-633.
Jiang, Y.H., Jiang, S.Y., Dai, B.Z., and Ling, H.F.,2008, Discrimination of ore-bearing and barren porphyries in the Yulong porphyry copper ore belt, east Tibet. International Geology Review, v. 50:p.583-595.
Jiang, Y.H., Jiang, S.Y., Dai, B.Z., Liao, S. Y., Zhao, K.D., and Ling, H.F.,2009, Middle to Late Jurassic felsic and mafic magmatism in southern Hunan Province, Southeast China: implications for a continental arc to rifting. Lithos, v.107, p.185-204.
Jiang, Y.H., Jin, G.D., Liao, S.Y., Zhou, Q., and Zhao, P.,2010a, Geochemical and Sr-Nd-Hf isotopic constraints on the origin of Late Triassic granitoids from the Qinling orogen, central China:implications for a continental arc to continent-continent collision. Lithos, v.117, p. 183-197.
Jiang, Y.H., Zhao, P., Zhou, Q., Liao, S.Y., and Jin, G.D.,2011, Petrogenesis and tectonic implications of Early Cretaceous S-and A-type granites in the northwest of the Gan-Hang rift, SE China. Lithos, v.121, p.55-73.
Jin, Z.D., Zhu, J.C., Ji, J.F., Lu, X.W., and Li, F.C.,2001, Ore-forming fluid constraints on illite crystallinity (IC) at Dexing porphyry copper deposit, Jiangxi Province. Science in China (Series D), v.44, p.177-184.
Jin, Z.D., Zhu, J.C., Ji, J.F., Li, F.C., and Lu, X.W.,2002, Two origins of illite at the Dexing porphyry Cu deposit, East China:implications for ore-forming fluid constraint on illite crystallinity. Clays and Clay Minerals, v.50, p.381-387.
Kay, R.W.J.,1978, Aleutian magnesium andesites:melts from subducted Pacific oceanic crust. Jour Volcan Geotherm Res, v,4, p.117-132.
Kay, S.M., Ramos, V.A., and Marquez, M.,1993, Evidence in Cerro Pampa volcanic rocks of slab melting prior to ridge trench collision in southern South America. Journal of Geology, v.101, p. 703-714.
Keleman, B.P.,1995, Genesis of high Mg# andesites and the continental crust. Contribute to Mineralogy and Petrology, v.120, p.1-19.
Kerrich R.,1993, Hydrothermal zircon and baddeleyite in Val-d'Or Archean mesothermal gold deposits:Characteristics, compositions, and fluid inclusion properties, wit h implications for timing of primary gold mineralization. Canadia Journal of Earth Sciences, v.30, p.2334-2351.
Kerich, R., Goldfarb, R., and Groves, D., et al.,2000, The characteristics, origins, and geodynamic settings of supergiant gold metallogenic provinces. Science in China, v.43, p.12-68.
Kirkham, R.V., and Sinclair, W.D.,1995, Porphyry copper, gold, molybdenum, tungsten, tin, silver. In:Eckstrand OR, Sinclair WD, Thorpe RI (eds) Geology of Canadian mineral deposit types. Geological Survey of Canada, Ottawa, p.421-446.
Lang, J.R., and Titley, S.R.,1998, Isotopic and geochemical characteristics of Laramide magmatic systems in Arizona and implications for the genesis of porphyry copper deposits. Economic Geology, v.93, p.138-170.
Lapierre, H., Jahn, B.M., Charvet, J.,1997. Mesozoic magmatism in Zhejiang Province and its relation with the tectonic activities in SE China. Tectonophysics, v.274, p.321-338.
Lee C.A.,2005. Trace Element Evidence for Hydrous Metasomatism at the Base of the North American Lithosphere and Possible Association with Laramide Low-Angle Subduction. The Journal of Geology, v.113, p.673-685.
Lepvrier, C., Maluski, H., Tich V.V., Leyerloup, A., Phan T.P., and Nguyen V.V.,2004, The Early Triassic Indosinian orogeny in Vietnam (Truong Son Belt and Kontum Massif: implications for the geodynamic evolution of Indochina. Tectonophysics, v.393, p.87-118.
Li, S.G., Chen, Y., Cong, B.L., Zhang, Z., Zhang, Y., Liou, D.L., Hart, S.A., and Ge, N.,1993, Collision of the North China and Yangtze Blocks and formation of coesite-bearing eclogites: timing and processes. Chemical Geology, v.109, p.80-89.
Li, X.F., and Sasaki, M.,2007, Hydrothermal Alteration and Mineralization of Middle Jurassic Dexing Porphyry Cu-Mo Deposit, Southeast China. Resource Geology, v.57, p.409-426.
Li, X.H., and McCulloch, M.T.,1996, Secular variation in the Nd isotopic composition of Neoproterozoic sediments from the southern margin of the Yangtze block:evidence for a Proterozoic continental collision in southeast China. Precambrian Research,v.76, p.67-76.
Li, X.H., Li, Z.X., Li, W.X., Liu, Y., Yuan, C., Wei, G., and Qi, C.,2007, U-Pb zircon, geochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I-and A-type granites from central Guangdong, SE China:A major igneous event in response to foundering of a subducted flat-slab? Lithos, v.96, p.186-204.
Li, X.H., Li, W.X., Wang, X.C., Li, Q.L., Liu, Y., Tang, G.Q., Gao, Y.Y., and Wu, F.Y.,2010, SIMS U-Pb zircon geochronology of porphyry Cu-Au-(Mo) deposits in the Yangtze River Metallogenic Belt, eastern China: Magmatic response to early Cretaceous lithospheric extension. Lithos,v.119, p.427-438.
Li, Z.X., and Li, X.H.,2007, Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China:a flat-slab subduction model. Geology, v.35:p.179-182.
Liang, H.Y., Sun, W.D., Su, W.C., and Zartman, R.E.,2009, Porphyry Copper-Gold Mineralization at Yulong, China, Promoted by Decreasing Redox Potential during Magnetite Alteration. Economic Geology, v.104, p.587-596.
Ling, M.X., Wang, F.Y., Ding, X., Hu, Y.H., Zhou, J.B., Zartman, R.E., Yang, X.Y., Sun, W.D., 2009. Cretaceous ridge subduction along the lower Yangtze River belt, eastern China. Economic Geology 104,303-321.
Livingston, D.E,1978, A plate tectonic hypothesis for the genesis of porphyry copper deposits of the southern Basin and Range Province. Earth Planetary Science Letters, v.20, p.171-179.
Lowell, J.D., and Gnilbert, J.M.,1970, Lateral and vertical alteration-mineralization zoning in porphyry ore deposits. Economic Geology, v.65, p.373-408.
Lu, J.J., Hua, R.M., Jiang, S.Y., Chen, X.M., and Gao, J.F.,2004. A study on copper isotope compositions of Dexing porphyry Cu-Au deposit of Jiangxi, China. Geochimica et Cosmochimica Acta, v.68, p. A302.
Ludwig, K.R.,1999, Isoplot/Ex, Version 2.0:A geochrological toolkit for Microsoft excel. Berkeley. Geochronology Center.
Ludwig, K.R.,2001, Using Isoplot/EX, version 2.49. In:A geolocronolgical toolkit for Microsoft excel, Berkeley Geochronological Center Special Publication, Berkeley, p.1-55.
Luhr, J.F.,1990, Experimental phase relations of water-and-sulfur-saturated arc magmas and the 1982 eruptions of El Chichon volcano. Journal of Petrology, v.31, p.1071-1114.
Mao J.W., Zhang Z.C., Zhang Z.H., and Du A.D.,1999, Re-Os isotopic dating of molybdenites in the Xiaoliugou W (Mo) deposit in the northern Qilian mountains and its geological significance. Geochimica et Cosmochimica Acta, v.63:p.1815-1818.
Mao, J.W., Xie, G.Q., Bierlein, F., Qu, W.J., Du, A.D., Ye, H.S., Pirajno, F., Li, H.M., Guo, B.J., Li, Y.F. and Yang, Z.Q.,2008,Tectonic implications from Re-Os dating of Mesozoic molybdenum deposits in the East Qinling-Dabie orogenic belt. Geochimica et Cosmochimica Acta, v.72:p.4607-4626.
Martin, H., Bonin, B., and Capdevila, R.,1994, The Kuiqi peralkaline granitic complex (SE China):petrology and geochemistry:Journal of Petrology, v.35, p.983-1015.
Martin, H., Smithies, R.H., Rapp, R., Moyen, J.F., and Champion, D.,2005, An overview of adakite, tonalite-trondhjemite-granodiorite (TTG), and sanukitoid:relationships and some implications for crustal evolution. Lithos, v.79, p.1-24.
Masterman, G.J., Cooke, D. R., Berry, R.F., Clark, A.H., Archibald, D.A., Mathur, R., Walshe, J.L., and Uuran, M.,2004, 40Ar/39Ar and Re-Os Geochronology of Porphyry Copper-Molybdenum Deposits and Related Copper-Silver Veins in the Collahuasi District, Northern Chile. Economic Geology, v.99:p.673-690.
Mathes, E.A.,1976, Sulfur solubility and magmatic sulfides in submarine basalt glass. Journal of Ceophyslell Research, v.81, p.4269-4276.
Mavrogenes, J.A., and O'Neill, H.S.C.,1999, The relative effects of pressure, temperature and oxygen fugacity on the solubility of sulfide in mafic magmas. Geochimica et Cosmochimica Aeta, v.63, p.1173-1180.
McDonough, W.F., and Sun, S.S.,1985, Isotopic and geochemical systematics in Tertiary-Recent basalts from southeastern Australia and implication for the sub-continental lithosphere. Geochimica et Cosmochimica Acta, v.49, p.2051-2067.
McInnes, B.I.A., and Cameron, E.M.,1994, Carbonated, alkaline hybridizing melts from a sub-arc environment:mantle wedge samples from the Tabar Lihir-tanga-Feni arc, Papua New Guinea. Earth and Planetary Science Letters, v.122, p.125-141.
Meyer, C., and Hemley, J.J.,1967, Wall rock alteration:in Geochemistry of Hydrothermal Ore Deposits. Barnes, H.L., ed., Holt, Rinehart and Winston, New York, p.166-235.
Mitchell, A.H.G., and Garson, M.S.,1972, Relationship of porphyry copper and circum-Pacific tin deposits to palaeo-Benioff zones. Institute of Mining and Metallurgy Transactions, v.81, p. B10-B25.
Mitchell, A. H. G.,1973, Metallogenic belt and angle of dip of Benioff zones. Nature, v.245, p. 49-52.
Mungall, J.E.,2002, Roasting the mantle:Slab melting and the genesis of major Au and Au-rich Cu deposits. Geology, v.30, p.915-918.
Mysen, B.O., and Popp, R.K.,1981, Solubility of sulfur in CaMgSi2O6 and NaAlSi3O8 melts at high pressure and temperature with controlled. American Journal of Science, v.280, p.78-92.
Oyarzun, R., Marquez, A., Lillo, J., Lopez, I., and Rivera, S.,2001, Giant versus small porphyry copper deposits of Cenozoic age in northern Chile. Adakitic versus normal calc-alkaline magmatism:Mineralium Deposita, v.36, p.794-798.
Oyarzun, R., Marquez, A., Lillo, J., Lopez, I., and Rivera, S.,2002, Reply to discussion on "Giant versus small porphyry copper deposits of Cenozoic age in northern Chile:Adakitic versus normal calc-alkaline magmatism" by Oyarzun, R., Marquez, A., Lillo, J., Lopez, I., and Rivera, S.,2001, Mineralium Deposita, v.36, p.794-798. Mineral Depos, v.37, p.795-799.
Pasteris, J.D.,1996, Mount Pinatubo volcano and "negative" porphyry copper deposits. Geology, v.24, p.1075-1078.
Patino Douce, A.E., Johnston, A.D.,1991, Phase equilibria and melt productivity in the pelitic system:implications for the origin of peraluminous granitoids and aluminous granulites. Contributions to Mineralogy and Petrology, v.107, p.202-218.
Pearce, J.A., and Norry, M.J.,1979, Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks. Contribution to Mineralogy and Petrology, v.69, p.33-47.
Pearce, J.A., Harris, N.B.W. and Tindle, A.G.,1984, Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology, v.25, p.956-983.
Pelleter, E., Cheilletz, A., Gasquet, D., Mouttaqi, A., Annich, M., Hakour, A.E., Deloule, E., and Feraud, G.,2007, Hydrothermal zircons:A tool for ion microprobe U-Pb dating of gold mineralization (Tamlalt-Menhouhou gold deposit-Morocco). Chemical Geology, v.245, p. 135-161.
Peng, G., Luhr, J.F., and MeGee, J.J.,1997, Factors control ling sulfur concentrations in volcanic apatite. American Mineralogist, v.82, p.1210-1224.
Peng, J.T., Zhou, M.F., Hu, R.Z., Shen, N.P., Yuan, S.D., Bi, X.W., Du, A.D., and Qu, W.J.,2006, Precise molybdenite Re-Os and mica Ar-Ar dating of the Mesozoic Yaogangxian tungsten deposit, central Nanling district, South China. Miner Deposita, v.41:p.661-669.
Perello, J.,1994, Geology, porphyry Cu-Au,and epithermal Cu-Au-Ag mineralization of the Tombuliato district, North Sulawesi, Indonesia. Jour Geochem Explor, v.50, p.221-256.
Petford, N. and Atherton, M.,1996, Na-rich partial melts from newly underplated basaltic crust: the Cordillera Blanca Batholith, Peru. Journal of Petrology, v.37, p.1491-1521.
Pettke T., Lee D.C., Halliday, A.N., Rea D.K.,2002, Radiogenic Hf isotopic compositions of continental eolian dust from Asia, its variability and its implications for seawater. Earth and Planetary Science Letters, v.202:p.453-464.
Pettke, T., Audetat, A., Schaltegger, U., and Heinrich, C.A.,2005, Magmatic-to-hydrothermal crystallization in the W-Sn mineralized Mole Granite (NSW, Australia) Part Ⅱ:Evolving zircon and thorite trace element chemistry. Chemical Geology, v.220, p.191-213.
Plank T., and Langmuir C.H.,1998, The chemical composition of subducting sediment and its consequences for the crust and mantle. Chemical Geology, v.145, p.325-394.
Polt, A., and Kerrich, R.,2002, Nd-isotope systematics of-2.7 Ga adakites, magnesian andesites, and arc basalts, Superior Province:evidence for shallow crustal recycling at Archean subduction zones. Earth and Planetary Science Letters, v.202, p.345-360.
Qiu, Y.M., Gao, S., McNaughton, N.J., Groves, D.I., and Ling, W.L.,2000, First evidence of N3.2 Ga continental crust in the Yangtze craton of South China and its implications for Archean crustal evolution and phanerozoic tectonics. Geology, v.28, p.11-14.
Qu X.M., Hou Z.Q., and Li, Y.G.,2004, Melt components derived from a subducted slab in late orogenic ore-bearing porphyries in the Gangdese copper belt, southern Tibetan plateau. Lithos, v.74, p.131-148.
Qu X.M., Hou Z.Q., Zaw, K., and Li, Y.G.,2007, Characteristics and genesis of Gangdese porphyry copper deposits in the southern Tibetan Plateau:Preliminary geochemical and geochronological results. Ore Geology Reviews, v.31, p.205-223.
Rapp, R.P., and Watson, E.B.,1995, Dehydration melting of metabasalt at 8-32 kbar:implications for continental growth and crust-mantle recycling. Journal of Petrology, v.36, p.891-931.
Ratschbacher, L., Hacker, B.R., Calvert, A, Webb, L.E., Grimmer, J.C., McWilliams, M.O., Ireland, T., Dong, S.W., and Hu, J.M.,2003, Tectonics of the Qinling (central China): Tectonostratigraphy, geochronology, and deformation history. Tectonophysics, v.366, p.1-53.
Reich, M., Parada, M.A,, Palacios C., et al. Adakite-like signature of Late Miocene intrusions at the Los Pelambres giant porphyry copper deposit in the Andes of central Chile:Metallogenic implications. Mineral Deposit,2003,38:876-885.
Richards, J.P.,2003, Tectono-magmatic precursors for porphyry Cu-(Mo-Au) deposit formation. Economic Geology, v.98, p.1515-1533.
Robb, L.,2005, Introduction to ore-forming process. Oxford:Blackwell, p.153-166.
Roedder, E.,1992, Fluid inclusion evidence for immiscibility in magmatic differentiation. Geochimica et Cosmochimica Aeta, v.56, p.5-20.
Sajona, F.G., Naury, R.C., Pubellier, M., Leterrier, J., Bellon, H. and Cotton, J.,2000, Magmatic source enrichment by slab-derived melts in a young post-collision setting, central Mindanao (Philippines). Lithos, v.54, p.173-206.
Schmidt, M.W., Vielzeuf, D., and Auzanneau, E.,2004, Melting and dissolution of subducting crust at high pressures:the key role of white mica. Earth and Planetary Science Letters, v.228, p.65-84.
Selby, D., and Creaser, R.A.,2001, Late and mid-Cretaceous mineralization in the northern Canadian Cordillera:constraints from Re-Os molybdenite dates. Economic Geology, v.96:p. 1461-1467.
Shimoda G., Tatsumi Y., Nohda S., Ishizakaa K., and Jahn B.M.,1998, Setouchi high-Mg andesites revisited:geochemical evidence for melting of subducting sediments. Earth and Planetary Science Letters. V.160, p.479-492.
Shimoda G., and Tatsumi Y.,1999, Generation of rhyolite magmas by melting of subducting sediments in Shodo-Shima island, Southwest Japan, and its bearing on the origin of high-Mg andesites. The Island Arc, v.8, p.383-392.
Shirey, S.B., and Walker R.J.,1995, Carius tube digestion for low-blank rhenium-osmium analyses. Analytical Chemistry, v.67:p.2136-2141
Sillitoe, R.H.,1972, A Plate Tectonic Model for the Origin of Porphyry Copper Deposits. Economic Geology, v.67, p.184-197.
Sillitoe, R.H.,1988, Epochs of intrusion-related copper mineralization in the Andes. Jour South Am Ear Sci, v.1, p.89-108.
Sillitoe, R.H.,1993, Gold-rich porphyry copper deposits: geological model and exploration implication. Mineral Deposit Modeling, Geological Association of Canada Special Paper, v.40, p.465-478.
Sillitoe, R.H.,1997, Characteristics and controls of the largest porphyry copper-gold and epithermal gold deposits in the circum-Pacific region. Australian Journal of Earth Sciences, v. 44, p.373-388.
Simon, A.C., Pettke, T., Candela, P.A., Piccoli, P.M., and Heinrich, C.A.,2004, Magnetite solubility and iron transport in magmatic-hydrothermal environments Geochimica et Cosmochimica Acta,2004, v.68, p.4905-4914.
Sisson, T.W., Ratajeski, K., Hankins, W.B., Glazner, A.F.,2005, Voluminous granitic magmas from common basaltic sources. Contributions to Mineralogy and Petrology, v.148, p.635-661.
Smith, R.E. and Smith, S.E.,1976, Comments on the use of Ti, Zr, Y, Sr, K, P and Na in classification of basaltic magmas. Earth and Planetary Science Letters, v.32, p.114-120.
Smoliar, M.I., Walker, R.J., and Morgan, J.W.,1996, Re-Os ages of group IIA, IIIA, IVA and VIB iron meteorites. Science, v.271, p.1099-1102.
Solomon,1990, Subduction, arc reversal, and the origin of porphyry copper-gold deposits in island arcs. Geology, v.18, p.630-633.
Stein, H.J., Markey, R.J., Morgan, J.W., Du, A., and Sun, Y.,1997, Highly Precise and Accurate Re-Os Ages for Molybdenite from the East Qinling Molybdenum Belt, Shanxi Province, China. Economic Geology, v.92, p.827-835.
Streck, M.J., and Dilles, J.H.,1998, Sulfur evolution of oxidized arc magmas as recorded in apatite from a porphyry copper batholith. Geology, v.26, p.523-526.
Sun, W.D., Arculus, R.J., Kamenetsky, V.S., and Binns, R.A.,2004, Release of gold-bearing fluids in convergent margin magmas prompted by magnetite crystallization:Nature, v.431, p. 975-978.
Sun W.D., Ding X., and Hu Y.H.,2007, The golden transformation of the Cretaceous plate subduction in the west Pacific. Earth and Planetary Science Letters, v.262, p.533-542.
Sun, W.D., Ling, M.X., Yang, X.Y., Fan, W.M., Ding, X., Liang, H.,2010. Ridge subduction and porphyry copper-gold mineralization:an overview. Science China Series Dearth Science 53, 475-484.
Tarkian, M., and Stribrny, B.,1999, Platinum-gToup dements in porphyry copper deposit, a reconnaissance study. Mineralogy and Petrology, v.65, p.161-183.
Tatsumi, Y.,1986, Formation of the volcanic from:in sumuction zones. Geophysical Research Letters, v.17, p.717-720.
Tatsumi Y,2001, Geochemical modeling of partial melting of subducting sediments and subsequent melt-mantle interaction:Generation of high-Mg andesites in the Setouchi volcanic belt, southwest Japan. Geological Society of America, v.29, p.323-326.
Todt W., Cliff R.A., and Hanser A.,1996, Evaluation of a 202Pb-205Pb double spike for high-precision lead isotope analyses. Geophys. Monogr., v.95, p.429-437.
Tosdal, R.M., Richards, J.P.,2001, Magmatic and structural controls on the development of porphyry Cu±Mo±Au deposits. In:Richards JP, Tosdal RM (eds) Structural controls on ore genesis. Reviews in Economic Geology, v.14, p.157-181.
Uyeda, S., and Kanamori, H.,1979, Back-arc opening and the model of subduction. Journal of Geophysical Research, v.84, p.1040-1061.
Valencia, V.A., Ruiz, J., and Barra, F.,2005, U-Pb zircon and Re-Os molybdenite geochronology from La Caridad porphyry copper deposit: Insights for the duration of magmatism and mineralization in the Nacozari district, Sonora, Mexico. Mineralium Deposita, v.40, p. 175-191.
Vervoort, J.D., Blichert-Toft, J., Patchett, P.J., and Albarede, F.,1999, Relationships between Lu-Hf and Sm-Nd isotopic systems in the global sedimentary system. Earth and Planetary Science Letters, v.168, p.79-99.
Wang, Q., Xu, J.F., Jian, P., Bao, Z.W., Zhao, Z.H., Li, C.F., Xiong, X.L., and Ma, J.L.,2006, Petrogenesis of Adakitic Porphyries in an Extensional Tectonic Setting, Dexing, South China: Implications for the Genesis of Porphyry Copper Mineralization. Journal of Petrology, v.47, p. 119-144.
Watson, E.B., Cherniak, D.J., Hanchar, J.M., Harrison, T.M. and Wark, D.A.,1997, The incorporation of Pb into zircon. Chemical Geology, v.141, p.19-31.
Wendlandt, R.F.,1982, Sulfur saturation of basalt and andesite melts at high pressures and temperatures. American Mineralogist, v.67, p.877-885.
Whitney, J.A., and Stomer, J.C.,1983, Igneous sulfides in the Fish canyon tuff and the role of S in calc-alkaline. Geology, v.11, p.99-102.
Whitney, J.A.,1984, Fugacities of sulfurous gases in pyrrhotite-bearing magmas. American Mineralogist, v.60, p.69-78.
Williams, I.S., Buick, A., and Cartwright, I.,1996, An extended episode of early Mesoproterozoic metamorphic fluid flow in the Reynold Region, central Australia. Journal of Metamorphic Geology, v.14, p.29-47.
Winchester, J.A. and Floyd, P.A.,1977, Geochemical discrimination of different magma series and their differentiation products using immobile elements:Chemical Geology,20, p.325-343.
Wu, F.Y., Yang, Y.H., Xie, L.W. Yang, J.H., and Xu, P.,2006, Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology. Chemical Geology, v.234:p. 105-126.
Wyman, D.A., Ayer, J.A., and Devaney, J.R.,2000, Niobium-enriched basalts from the Wabigoon subprovince, Canada:evidence for adakitic metasomatism above an Archean subduction zone. Earth and Planetary Science Letters, v.179, p.21-30.
Xiong, Y.L., and Wood, S.A.,2001, Hydrothermal transport and deposition of rhenium under subcritical conditions (up to 200℃) in light of experimental studies. Economic Geology, v.96, p.1429-1444.
Xiong, Y.L., and Wood, S.A.,2002, Hydrothermal solubility of ReS2 and the Re-ReO2 buffer assemblage and transport of rhenium under supercritical conditions. Geochemical Transactions, v.3, p.1-10.
Xiong, Y.L., Wood, S.A., and Kruszewski J,2006, Hydrothermal transport and deposition of Rhenium under subcritical conditions revisited. Economic Geology, v.101, p.471-478
Xu, J.F., Shinjo, R., Defant, M.J., Wang, Q., and Rapp, R.P.,2002, Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China:partial melting of delaminated lower continental crust. Geology, v.30, p.1111-1114.
Yao J.M., Hua R.M., Qu W.J., Qi H.R., Lin J.F., and Du A.D.,2007, Re-Os isotope dating of molybdenites in the Huangshaping Pb-Zn-W-Mo polymetallic deposit, Hunan province, South China and its geological significance. Science in China (Series D), v.50, p.519-526.
Yan, M.Z., and Hu, K.,1980, Geological characteristics of the Dexing porphyry copper deposits, Jiangxi, China. Mining Geology, Special Issue v.8, p.197-203.
Yogodzinski G. M., Kay R. W., Volynets O. N., and Koloskov A. V.,1995, Magnesian andesite in the western Aleutian Komandorsky region:Implications for slab melting and processes in the mantle wedge. GSA Bulletin, v.107, p.505-519.
Zartman, R.E., and Doe, B.R.,1981, Plumb tectonics-The model tectonophys. Tectonophys, v.75, p.125-177.
Zaw K., Peters S.G., Cromie P., et al.,2007, Nature, diversity of deposit types and metallogenic relations of South China. Ore Geology Reviews, v.31, p.3-47.
Zhai, Y., Deng, J., and Peng, R.,1997, Some major mineral deposits in China:their tectonic setting and deposit model characteristics. Proceeding,30th International Geology Congress, v.9, p.367-379.
Zhang, Z.M., Hou, Z.Q., White, N.C., Chang, Z.S., Li, Z.Q., and Song, Y.C.,2009, Geology of the post-collisional porphyry copper-molybdenum deposit at Qulong, Tibet. Ore Geology Reviews, v.36, p.133-159.
Zhang, S.B., Zheng, Y.F., Wu, Y.B., Zhao, Z.F, Gao, S., and Wu, Y.,2006, Zircon U-Pb age and Hf-O isotope evidence for Paleoproterozoic metamorphic event in South China. Precambrian Research, v.151:p.265-288.
Zhang, S.B., Zheng, Y.F., Zhao, Z.F., Wu, Y.B., Yuan, H.L., and Wu, F.Y.,2008, Neoproterozoic anatexis of Archean lithosphere:Geochemical evidence from felsic to mafic intrusions at Xiaofeng in the Yangtze Gorge, South China. Precambrian Research, v.163:p.210-238.
Zhang S.B., Zheng Y.F., Zhao Z.F., Wu Y.B., Yuan H.L., and Wu, F.Y.,2009, Origin of TTG-like rocks from anatexis of ancient lower crust:Geochemical evidence from Neoproterozoic granitoids in South China. Lithos, v.113:p.347-368.
Zhou, J.X.,1999, Geochemistry and petrogenesis of igneous rocks containing amphibole and mica: A case study of plate collision involving Scotland and Himalayas. New York and Beijing, Science Press, p.41-72.
Zhou, X.M., and Li, W.X.,2000, Origin of Late Mesozoic igneous rocks in Southeastern China: implications for lithosphere subduction and underplating of mafic magmas. Tectonophysics, v. 326:p.269-287.
Zhou, X.M., Sun, T., Shen, W.Z., Shu, L.S., and Niu, Y.L.,2006, Petrogenesis of Mesozoic granitoids and volcanic rocks in South China:a response to tectonic evolution. Episodes, v.29, p.26-33.
陈江峰,郭新生,汤加富,等,1999,中国东南地壳增长与Nd同位素模式年龄.南京大学学报,(自然科学),v.35,p.649-658.
陈民扬,李耀菘,1997,铜矿床同位素地球化学.北京：科学出版社,p.376-378.
陈志广,张连昌,吴华英,等,2008,内蒙古西拉木伦成矿带碾子沟钼矿区A型花岗岩地球化学和构造背景.岩石学报,v.24,p.879-889.
代军治,毛景文,杜安道,等,辽西肖家营子钼(铁)矿床Re-Os年龄及其地质意义.地质学报,2007,v.81,p.917-923.
邓晋福,赵海玲,莫宣学,等,1995,扬子大陆的陆内俯冲与大陆换缩小-由白云母(二云母)花岗岩推导.高校地质学报,v.1,p.50-57.
杜安道,何红蓼,殷宁万,等,1994,辉钼矿的铼—锇同位素地质年龄测定方法研究.地质学报,v.66,p.339-347.
杜安道,赵敦敏,王淑贤,等,2001, Carius管溶样-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,v.20,p.247-252.
丰成友,许建祥,曾载淋,等,2007a,赣南天门山—红桃岭钨锡矿田成岩成矿时代精细测定及其地质意义.地质学报,v.81,p.952-963.
丰成友,丰耀东,许建祥,等,2007b,赣南张天堂地区岩体型钨矿晚侏罗世成岩成矿的同位素年代学证据.中国地质,v.34,p.642-650.
高剑峰,陆建军,赖鸣远,等,2003,岩石样品中微量元素的高分辨率等离子质谱分析.南京大学学报(自然科学),v.39,p.844-850.
郭新生,季克俭,黄耀生,等,1999,德兴斑岩铜矿成矿热液来源及其演化——花岗闪长斑岩的氧同位素制约.高校地质学报,v.5,p.260-268
侯可军,李延河,邹天人,等,2007, LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报,23(10)：2595-2604.
侯增谦,曲晓明,王淑贤,等,2003,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),v.33,p.609-618.
侯增谦,2004.斑岩Cu-Mo-Au矿床：新认识与新进展.地学前缘,v.11,p.131-144.
华仁民,李晓峰,陆建军,等,2000,德兴大型铜金矿集区构造环境和成矿流体研究进展.地球科学进展,v.15,p.525-533.
华仁民,陈培荣,张文兰,等,2003,华南中、新生代与花岗岩类有关的成矿系统.中国科学(D辑),v.33,p.335-343.
华仁民,陈培荣,张文兰,等,2005,论华南地区中生代3次大规模成矿作用.矿床地质.v.24,p.99-107.
黄典豪,吴澄宇,聂凤军,1987,陕西金堆城斑岩钼矿床地质特征及成因探讨·矿床地质,v.6,p. 22-34.
黄典豪,吴澄宇,杜安道,等,1994,东秦岭地区钼矿床的铼-锇同位素年龄及其意义.矿床地质,v.13,p.221-230.
黄定堂,2003,灵山岩体演化特征及其与稀有金属的成矿关系.地质与勘探,v.39,p.35-40.
季克俭,吴学汉,张国柄,1989,热液矿床的矿源、水源和热源及矿床分布规律.北京,北京科学技术出版社.
蒋少涌,赵葵东,姜耀辉,等,2008,十杭带湘南-桂北段中生代A型花岗岩带成岩成矿特征及成因讨论.高校地质学报.v.14,p.496-509.
金章东,朱金初.1998,关于德兴斑岩铜矿成矿物质来源—与梁祥济研究员商榷.地质论评,v.44,p.464-469.
金章东,朱金初,李福春,2002,德兴斑岩铜矿成矿过程的氧、锶、钕同位素证据.矿床地质,v.21,p.342-350.
李红艳,毛景文,孙亚莉,等,1996,柿竹园钨多金属矿床的Re-Os同位素等时线年龄研究.地质论评,v.42,p.261-267.
李晓峰,Watanabe Y,华仁民,等,2008,华南地区中生代Cu-(Mo)-W-Sn矿床成矿作用与洋岭／转换断层俯冲.地质学报,v.82,p.625-640.
李永峰,毛景文,刘敦一,等,2006,豫西雷门沟斑岩钼矿SHRIMP锆石U-Pb和辉钼矿Re-Os测年及其地质意义.地质论评,v.52,p.122-131.
梁华英,孙卫东,苏文超,等,2009,斑岩型铜(金)矿床成矿元素大规模堆积制约机制研究.矿物学报,v.S1,p.182-183
梁祥济,1995,江西德兴斑岩铜矿成矿物质来源的实验研究.地质论评,v.41,p.463-471.
刘姤群,杨世义,张秀兰,等.1983,德兴斑岩铜矿斑岩和围岩蚀变特征及斑岩和成矿物质来源的讨论.中国地质科学院宜昌地质矿产研究所所刊,v.7,p.77-95.
卢树东,高文亮,汪石林,等,2005,江西张十八铅锌矿铅同位素组成特征及其成因意义.矿物岩石,v.25,p.64-69.
毛景文,胡瑞忠,陈毓川,等,2006,大规模成矿作用与大型矿集区.北京：地质出版社,p.1-1030.
聂凤军,张万益,杜安道等.2007,内蒙古小东沟斑岩型钼矿床辉钼矿铼-锇同位素年龄及地质意义.地质学报,v.81,p.898-905.
钱鹏,陆建军,姚春亮,2003,德兴斑岩铜矿成矿流体演化与来源的流体包裹体研究.南京大学学报(自然科学),v.39,p.319-326.
钱鹏,陆建军,刘风香,2006,江西德兴斑岩铜矿成矿物质来源同位素示踪.世界地质,v.25,p.135-140.
秦克章,李光明,赵俊兴,等,2008,西藏首例独立钼矿——冈底斯沙让大型斑岩钼矿的发现及其意义.中国地质,v.35,p.1101-1112.
芮宗瑶,黄崇轲,齐国明,等,1984,中国斑岩铜(钼)矿床.北京：地质出版社,p.1-140.
芮宗瑶,张洪涛,陈仁义,等,2006,斑岩铜矿研究中若干问题探讨.矿床地质,v.25,p.491-500.
唐仁鲤,罗怀松,1995,西藏玉龙斑岩铜(钼)矿带地质.北京：地质出版社,p.1-310.
王德滋,沈渭洲,2003,中国东南部花岗岩成因与地壳演化.地学前缘,v.10,p.209-220.
王强,赵振华,简平,等,2004,德兴花岗闪长斑岩SHRIMP锆石U-Pb年代学和Nd-Sr同位素地球化学.岩石学报,v.20,p.315-324.
王永磊,裴荣富,李进文,等,2009,湘东南将军寨钨矿花岗岩地球化学特征及铼-锇同位素定年.岩矿测试,v.28,p.274-278.
吴澄宇,刘孝善,1989,南泥湖钼(钨)矿化花岗岩体的成因特征·南京大学学报.v.25,p.333-346.
徐夕生,谢听,2005,中国东南部晚中生代—新生代玄武岩与壳幔作用,高校地质学报,v.11,p.318-334.
姚春亮,2006,德兴斑岩铜矿含矿岩体特征和矿化机制.博士论文,p.1-89.
姚军明,华仁民,屈文俊,等,2007,湘南黄沙坪铅锌钨钼多金属矿床辉钼矿的Re-Os同位素定年及其意义.中国科学(D辑),v.37,p.471-477.
叶会寿,毛景文,李永峰,等,2006,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.地质学报,v.80,p.1078-1088.
叶松,叶德隆,莫宣学,等.深源岩浆作用与江西德兴大型矿集区成矿关系.高校地质学报.1999,5(4)：395-404.
曾载淋,张永忠,朱详培,等,2009,赣南崇义地区茅坪钨锡矿床铼-锇同位素定年及其地质意义.岩矿测试,v.28,p.209-214.
张洪涛,陈仁义,韩芳林,2004,重新认识中国斑岩铜矿的成矿地质条件.矿床地质,v.23,p.
150-163.
张理刚,1992,铅同位素地质研究现状及展望.地质与勘探,v.28,p.21-29.
张理刚,刘敬秀,陈振胜,等,1996,江西德兴铜厂铜矿水-岩体系氢氧同位素演化.地质科学,v.31,p.250-263.
张振亮,2003,德兴铜厂铜矿非常温常压条件下的流体包裹体拉曼光谱特征及其成矿意义.硕士论文,p.1-98.
张作伦,曾庆栋,屈文俊,等,2009,内蒙碾子沟钼矿床辉钼矿Re-Os同位素年龄及其地质 意义.岩石学报,v.25,p.212-218.
周珂,叶会寿,毛景文,等,2009,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.矿床地质,v.28,p.170-184.
周耀华,梅占魁,王传松,等,1981,德兴斑岩铜矿物质来源之刍议.江西地质科技,v.1,p.32-41.
朱金初,沈渭洲,刘昌实,等,1990,华南中生代同熔系列花岗岩类的Nd-Sr同位素特征及成因讨论.岩石矿物学杂志,v.9,p.97-104.
朱金初,金章东,饶冰,等,2002,德兴铜厂斑岩铜矿流体过程.南京大学学报(自然科学),v.38,p.418-434.
朱训,黄崇轲,芮宗瑶,等,1983,德兴斑岩铜矿.北京：地质出版社,p.1-336.
朱永峰,宋彪,2006,新疆天格尔糜棱岩化花岗岩的岩石学及其SHRIMP年代学研究：兼论花岗岩中热液锆石边的定年.岩石学报,v.22,p.135-144.
© 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 |