粤西阳春盆地多金属矿床成矿系列及动力学背景
|
摘要
粤西阳春盆地为广东省重要的多金属矿集区之一,主要包括矽卡岩型、斑岩-矽卡岩型和热液脉型3类多金属矿床。阳春盆地发育多种矿化元素,矿种以Cu、Fe、Pb、Zn、Ag、W、Sn为主,Au、Mo、Bi次之。文章在梳理前人工作成果的基础上,将阳春盆地的多金属矿床厘定为一个成矿系列和3个成矿亚系列:即与燕山期侵入岩有关的Fe-Cu-Pb-Zn-W-Sn多金属矿床成矿系列,包括与中侏罗世侵入岩有关的铁铜多金属矿床成矿亚系列(Ⅰ)、与早白垩世中酸性侵入岩有关的铜钼铅锌多金属矿床成矿亚系列(Ⅱ)和与晚白垩世花岗岩有关的W-Sn多金属矿床成矿亚系列(Ⅲ)。Ⅰ和Ⅱ成矿亚系列主要沿阳春盆地的边缘坳陷带分布,受NE-NNE向构造及EW向构造复合控制,成矿岩体主要为花岗闪长岩、二长花岗斑岩以及二长花岗岩等,来源于相对深部,为壳幔同熔的产物,成因类型主要包括矽卡岩型和斑岩-矽卡岩型;Ⅲ成矿亚系列主要产于隆起区与坳陷带接壤部位及坳陷带中局部隆起地段,受隐伏的NW向构造控制,与成矿有关的花岗岩类属弱过铝质-准铝质花岗岩,由地壳物质重熔而形成,也可能有少量的地幔物质加入,矿床类型以石英脉型和斑岩-矽卡岩型-热液脉型为主。大量的高精度测年数据表明:Ⅰ亚系列成矿时代主要集中在170~160 Ma,Ⅱ亚系列成矿年龄主要集中在110~98 Ma,而Ⅲ亚系列成矿年龄为85~76 Ma,前一成矿亚系列对应的成矿动力学背景为太平洋板块的俯冲环境,而Ⅱ和Ⅲ成矿亚系列则处于燕山晚期的拉张伸展环境并伴随强烈的壳幔相互作用,其可能与135 Ma之后太平洋板块的运动方向发生转向有关。
The Yangchun Basin, one of the important polymetallic ore concentration areas in Guangdong Province, mainly possesses skarn, porphyry-skarn and vein type deposits. Yangchun Basin has developed multiple ore-forming elements, mainly Cu, Fe, Pb, Zn, Ag, W, Sn and subordinately Au, Mo, Bi. Based on previous researches,the authors hold that these deposits belong to one metallogenic series, i. e., Fe-Cu-Pb-Zn-W-Sn polymetallic ore-deposit minerogenetic series related to Yanshanian intrusion, which can be subdivided into three subseries of ore deposits. The major subseries are composed of Fe-Cu polymetallic deposit subseries( Ⅰ)associated with Middle Juarassic intrusive rocks, Cu-Mo-Pb-Zn polymetallic deposit subseries( Ⅱ) related to Early Cretaceous intermediate-acid intrusive rocks and W-Sn polymetallic deposit subseries( Ⅲ) associated with Late Cretaceous granite. Ⅰ and Ⅱ subseries are distributed along the marginal depression of Yangchun Basin and controlled by the composite part of NE-NNE trending structures and EW structures. Metallogenic rock bodies are mainly granodiorite, monzogranite-porphyry and monzonite granite, which were derived from the relatively deep part and formed by the melting of the crust and the mantle, and the genetic types of ore deposits are mainly of porphyry and porphyry-skarn types; deposits of Ⅲ subseries are controlled by buried NW-trending structures, and occur in the contact part of uplifting area and hollow zone as well as parts of uplifting areas of the hollow zone. Granitoids associated with mineralization are mainly weak-intermediate peraluminous granites, which were formed by the melting of crustal substances, with the probable addition of a small amount of mantle substances. The deposit genetic types are mostly of vein type and porphyry-skarn-vein type. A large number of high-precision dating data show that deposits ofⅠ subseries have ages of 170 ~ 160 Ma, and those of Ⅱ and Ⅲ subseries have ages of 110~ 98 Ma and 85 ~ 76 Ma, respectively. In conclusion, the metallogenic geodynamical settings of Ⅰsubseries corresponded to the Pacific plate subduction environment, and the metallogenic geodynamical settings of Ⅱ and Ⅲ subseries might have been related to late Yanshanian pull-apart and stretching environment accompanied by strong crust-mantle interaction, which was probably caused by the change of the movement direction of the Pacific Plate after 135 Ma.
The Yangchun Basin, one of the important polymetallic ore concentration areas in Guangdong Province, mainly possesses skarn, porphyry-skarn and vein type deposits. Yangchun Basin has developed multiple ore-forming elements, mainly Cu, Fe, Pb, Zn, Ag, W, Sn and subordinately Au, Mo, Bi. Based on previous researches,the authors hold that these deposits belong to one metallogenic series, i. e., Fe-Cu-Pb-Zn-W-Sn polymetallic ore-deposit minerogenetic series related to Yanshanian intrusion, which can be subdivided into three subseries of ore deposits. The major subseries are composed of Fe-Cu polymetallic deposit subseries( Ⅰ)associated with Middle Juarassic intrusive rocks, Cu-Mo-Pb-Zn polymetallic deposit subseries( Ⅱ) related to Early Cretaceous intermediate-acid intrusive rocks and W-Sn polymetallic deposit subseries( Ⅲ) associated with Late Cretaceous granite. Ⅰ and Ⅱ subseries are distributed along the marginal depression of Yangchun Basin and controlled by the composite part of NE-NNE trending structures and EW structures. Metallogenic rock bodies are mainly granodiorite, monzogranite-porphyry and monzonite granite, which were derived from the relatively deep part and formed by the melting of the crust and the mantle, and the genetic types of ore deposits are mainly of porphyry and porphyry-skarn types; deposits of Ⅲ subseries are controlled by buried NW-trending structures, and occur in the contact part of uplifting area and hollow zone as well as parts of uplifting areas of the hollow zone. Granitoids associated with mineralization are mainly weak-intermediate peraluminous granites, which were formed by the melting of crustal substances, with the probable addition of a small amount of mantle substances. The deposit genetic types are mostly of vein type and porphyry-skarn-vein type. A large number of high-precision dating data show that deposits ofⅠ subseries have ages of 170 ~ 160 Ma, and those of Ⅱ and Ⅲ subseries have ages of 110~ 98 Ma and 85 ~ 76 Ma, respectively. In conclusion, the metallogenic geodynamical settings of Ⅰsubseries corresponded to the Pacific plate subduction environment, and the metallogenic geodynamical settings of Ⅱ and Ⅲ subseries might have been related to late Yanshanian pull-apart and stretching environment accompanied by strong crust-mantle interaction, which was probably caused by the change of the movement direction of the Pacific Plate after 135 Ma.
引文
Cai M,Peng S B,Meng X J and Liu G Q.2001.Study on Mesozoic metallogenic regularity and dynamical mechanism in east Guangxi-westGuangdong area[J].Geology and Mineral Resources of South China,(2):35-42(in Chinese with English abstract).
Cai M H,Zhan M G,Peng S B,Meng X J and Liu G Q.2002.Study ofMesozoic metallogenic geological setting and dynamic mechanism inYunkai area[J].Mineral Deposits,21(3):254-269(in Chinesewith English abstract).
Charvet J,Faure M,Fabbri O,Cluzel D and Lapierre H.1990.Accretion and collision during East-Asian margin building:A new insighton the Peri-Pacific orogenies[A].In:Wiley T J,Howell D G andWong F L,eds.Terrane ana lysis of China and the Pacific Rim[C].Circum-Pacific Council for Energy and Mineral Resources,EarthScience Series,13:161-190.
Chen F W,Li H Q and Mei Y P.2008.Zircon SHRIMP U-Pb chronology of diagenetic mineralization of the Longtoushan porphyry goldorefield,Gui County,Guangxi[J].Acta Geologica Sinica,82(7):921-926(in Chinese with English abstract).
Chen Y C,Pei R F and Zhang H L.1990.The Geology of nonferrous andrare metal deposits related to Mesozoic Granitoids in the Nanling region,China[J].Bulletin of the Chinese Academy of GeologicalSciences,20:79-85(in Chinese with English abstract).
Chen Y C,Wang P A,Qin K L,Zhao D H and Mao J W.1994.Metallgenic series of main ore deposits and regional metallogeny in theQinling area[J].Mineral Deposits,13(4):289-298(in Chinesewith English abstract).
Chen Y C,Wang D H,Xu Z G and Zhu M Y.2006.Preliminary study ofChinese mineralization system[J].Mineral Deposits,25(2):155-163(in Chinese with English abstract).
Chen Y C,Wang D H,Zhu Y S,Xu Z G,Zhai Y S,Chang Y F,TangZ L,Pei R F,Teng J W,Deng J F,Hu Y Z,Ren T X,Shen B F,Wang S C,Xiao K Y,Peng R M,Qian Z Z,Mei Y X,Du J G,ShiJ F,Zhang X H,Zhu M Y,Xu Y and Xue C J.2007.Chinesemineralizaiton system and assessment of rigional mineralization[M].Beijing:Geological Publishing House.1-462(in Chinese).
Chen Y C,Liu D Q,Tang Y L,Wang D H,Dong L H,Xu X and WangX D.2008.Mineral resources and mineralization system in Tianshan,China[M].Beijing:Geological Publishing House.1-1061(in Chinese).
Chen Y C,Wang D H,Xu Z G and Huang F.2014.Outline of regionametallogeny of ore deposits associated with the Mesozoic magmatism inSouth China[J].Geotectonica et Metallogenia,38(2):219-229(inChinese with English abstract).
Chen Z H,Chen Y C and Wang D H.2009.The demonstration studiesfor assessment of mineral resources potential[M].Beijing:GeologicaPublishing House.1-195(in Chinese).
Chen Z Z.1988.Geology-goehemistry charaeteristies of Xishan granitebody in Yangehun,Guangdong[J].Acta Scientiarum NaturaliumUniversitatis Sunyatseni,(01):1-12(in Chinese with English abstract).
Deng P,Shu L S,Yu X Q,Wang B,Tan Z Z and Sun Y.2004.EarlyMiddle Jurassic Basins and features of igneous rocks in the westernFujian-southern Jiangxi region[J].Acta Petrologica Sinica,20(3):521-532(in Chinese with English abstract).
Dong S W,Zhang Y Q,Long C X,Yang Z Y,Ji Q,Hu J M and Chen XH.2007.Jurassic tectonic revolution in China and new interpretationof the Yanshan movement[J].Acta Geologica Sinica,81(11):1449-1461(in Chinese with English abstract).
Faure M and Ishida K.1990.The Mid-Upper Jurassic olistostrome of thewest Philippines:A distinctive key-maker for the Palawan Block[J].J.Southeast Asian Earth Sci.,4:61-67.
Foley S F and Peccerillo A.1992.Potassic and ultrapotassic magmas andtheir origin[J].Lithos,28:181-185.
Fukao Y,Obayashi M,Inoue H and Nenbai M.1992.Subducting slabsstagnant in the Mantle Transition Zone[J].Journal of GeophysicaResearch,97:4809-4822.
Geng H Y,Xu X S,O'Reilly S Y,Zhao M and Sun T.2006.Cretaceousvolcanic-intrusive magmatism in western Guangdong and its geologicasignificance[J].Science in China(Series D),36(7):601-617(inChinese).
Geological Construction Engineering Institute of Guangdong Province.2008.Geological survey report in Yangchun copper-polymetallic orefield,Guangdong Province[R].(in Chinese).
Geology Bureau for Nonferrous Metals of Guangdong Province.2014.General design of critical fundermental geological research in Yangchuncopper polmetallic ore exploration area,Guangdong Province[R].(in Chinese).
Goldfarbl R J,Hart C,Davis G and Geoves D.2007.East Asian gold:Deciphering the anomaly of phanerozoic gold in Precambrian Cratons[J].Econ.Geol.,102:341-345.
Hider T W C.1976.Tectonic history of the western Pacific[A].In:Drake C L,ed.Geodynamics:Progress and prospects[C].Washington DC.American Geophysical Union.
Hua R M,Chen P R,Zhang W L,Liu X D,Lu J J,Lin J F,Yao J,M,Qi H W,Zhang Z S and Gu C Y.2003.Metallogenic systems relatedto Cenozoic and Mesozoic granitoids in South China[J].Science inChina(Series D),33(4):335-343(in Chinese).
Hua R M,Chen P R,Zhang W L and Lu J J.2005.Three major metallogenic events in Mesozoic in South China[J].Mineral Deposits,24(2):99-107(in Chinese with English abstract).
Huang H Y,Li X H,Li Z X and Li X W.2013.Intraplate crustalremelting as the genesis of Jurassic high-K granites in the coastal region of the Guangdong Province,SE China[J].Journal of AsianEarth Sciences 74,280-302.
Isozaki Y.1997.Jurassic accretion tectonics of Japan[J].The IslandArc,6:25-51.
Jia J T,Wang P J and Wan X Q.2008.Chronostratigraphy of theyingcheng formation in the Songliao Basin,Cretaceous,NE China[J].Geological Review,54(4):439-448(in Chinese with Englishabstract).
Lan T G,Fan H R,Santosh M,Hu F F,Yang K F,Yang Y H and LiuY S.2012.Early Jurassic high-K calc-alkaline and shoshonitic rocksfrom the Tongshi intrusive complex,eastern North China Craton:Implication for crust-mantle interaction and post-collisional magmatism[J].Lithos 140-141,183-199.
Li L,Zhong D L,Shi X P,Tang Z B,Gong H B and Hu Q Y.2008.Late Mesozoic extensional structure and its constrains on mineralizationin western Shandong[J].Geological Review,54(4):449-458(inChinese with English abstract).
Li X F,Yasushi W,Hua R M and Mao J W.2008.Mesozoic Cu-Mo-WSn mineralization and ridge/triple subduction in South China[J].Acta Geologica Sinica,82(5):625-640(in Chinese with English abstract).
Li X H,Zhou H W,Liu Y,Li J Y,Chen Z H,Yu J S and Gui X T.2000.Mesozoic shoshonitic intrusives in the Yangchun Basin,westernGuangdong,and their tectonic significance:I.Petrology and isotopegeochronology[J].Geochimica,29(6):513-520(in Chinese withEnglish abstract).
Li X H,Zhou H W,Liu Y,Li J Y,Chen Z H,Yu J S and Gui X T.2001.Mesozoic shoshonitic intrusives in Yangchun Basin,westernGuangdong,and their tectonic significance:Ⅱ.Trace elements andSr-Nd isotopes[J].Geochimica,30(1):57-65(in Chinese withEnglish abstract).
Liu X D and Hua R M.2005.40Ar/39Ar Dating of adularia from the Bitian gold-silver-copper deposit,Fujian Province[J].Geological Review,51(2):151-155(in Chinese with English abstract).
Ma D Q,Zhao Z J,Lin H K and Zhang X H.1985.Petrographical studyof the enclaves from the Gangwei-Shilu-type granitoids in YangchunBasin of Guangdong and adiscussion in their genesis[J].Bull.Yichang Inst.Geol.Mineral Resoures CAGS,10:59-72(in Chinesewith English abstract).
Ma D S and Chen P R.2006.The Mesozoic thermal-uplift metallogenesisand passive up-welling of asthenosphere in South China[A].In:ChenJ,ed.Press in geological and geochemical researches[C].Nanjing:Press of Nanjing University.224-235(in Chinese).
Mao J R,Xu N Z,Hu Q,Xing G F and Yang Z L.2004.The Mesozoicrock-forming and ore-forming processes and tectonic environment evolusion in Shanghang-Datian region,Fujian[J].Acta Petrologica Sinica,20(2):285-296(in Chinese with English abstract).
Mao J W,Xie G Q,Li X F,Zhang C Q and Mei Y X.2004a.Mesozoiclarge scale mineralization and multiple lithospheric extension in SouthChina[J].Earth Science Frontiers,11(1):45-55(in Chinese withEnglish abstract).
Mao J W,Stein H,Du A D,Zhou T F,Mei Y X,Li Y F,Zang W Q andLi J W.2004b.Molybdenite Re-Os precise dating for molybdenite from Cu-Au-Mo deposits in the middle-lower reaches of YangtzeRiver Belt and its implications for mineralization[J].Acta GeologicaSinica,78(1):121-131(in Chinese with English abstract).
Mao J W,Xie G Q,Zhang Z H,Li X F,Wang Y T,Zhang C Q and LiY F.2005.Mesozoic large-scale metallogenic pulses in North Chinaand corresponding geodynamic settings[J].Acta Petrologica Sinica,21(1):169-188(in Chinese with English abstract).
Mao J W,Wang Y T,Lehmann B,Yu J J,Du A D,Mei Y X,Li Y F,Zang W S,Stein H J and Zhou T F.2006.Molybdenite Re-Os andalbite40Ar/39Ar dating of Cu-Au-Mo and magnetite porphyry systemsin the Yangtze River Valley and metallogenic implications[J].OreGeology Reviews,29:307-324.
Mao J W,Xie G Q,Guo C L and Chen Y C.2007.Large-scale tungstentin mineralization in the Nanling region,South China:Metallogenic ages and corresponding geodynamic processes[J].Acta PetrologicaSinica,23(10):2329-2338(in Chinese with English abstract).
Mao J W,Xie G Q,Guo C L,Yuan S D,Cheng Y B and Chen Y C.2008.Spatial-Temporal distribution of Mesozoic ore deposits in SouthChina and their metallogenic settings[J].Geological Journal of ChinaUniversities,14(4):510-526(in Chinese with English abstract).
Mao J W,Xie G Q,Bierlein F,Ye H S,Qu W J,Du A D,Pirajno F,LH M,Guo B J,Li Y F and Yang Z Q.2008a.Tectonic implicationsfrom Re-Os dating of Mesozoic molybdenum deposits in the East Qinling-Dabie Orogenic Belt[J].Geochim.Cosmochim.Acta,72:4607-4626.
Mao J W,Wang Y T,Li H M,Pirajno F,Zhang C Q and Wang R T.2008b.The relationship of mantle-derived fluids to gold metallogenesis in the Jiaodong Peninsula:Evidence from D-O-C-S isotope systematic[J].Ore Geology Reviews,33:361-381.
Mao J W,Xie G Q,Cheng Y B and Chen Y C.2009.Mineral deposimodels of Mesozoic ore deposits in South China[J].Geological Review,55(3):347-354(in Chinese with English abstract).
Mao J W,Pirajno F and Cook N.2011.Mesozoic metallogeny in EasChina and corresponding geodynamic settings-An introduction to thespecial issue[J].Ore Geology Reviews,43:1-7.
Mao J W,Chen M H,Yuan S D and Guo C L.2011.Geological characteristics of the Qinhang(or Shihang)Metallogenic Belt in SouthChina and spatial-temporal distribution regularity of mineral deposits[J].Acta Geologica Sinica,85(5):636-658(in Chinese with English abstract).
Mao J W,Cheng Y B,Chen M H and Pirajno F.2013.Major types andtime-space distribution of Mesozoic ore deposits in South China andtheir geodynamic settings[J].Miner Deposita,48:267-294.
Mao J W,Pirajno F,Lehmann B,Luo M C and Berzina A.2014.Distribution of porphyry deposits in the Eurasian continent and their corresponding tectonic settings[J].Journal of Asian Earth Sciences,79:576-584.
Maruyama S and Seno T.1986.Orogeny and relative plate motion:Example of the Japanese Islands[J].Tectonophysics,127:305-329.
Mei Y P,Yang H M,Duan R C,Zhang L G,Cai Y X,Tong X R,TanJ J,Liu C P and Lu S S.2013.Diagenetic and metallogenic geochronlogy study of the Xishan W-Sn ore deposit in Yangchuang oGuangdong Province[J].Acta Geologica Sinica,87(9):1370-1376(in Chinese with English abstract).
Moore C W.1989.Mesozoic and Cenozoic paleographic development othe Pacific region[J].Abstract,28th IGC(2),Washington DC.USA:GAS Press.455-456.
Morrison G W.1980.Characteristics and tectonic setting of the shoshoniterock association[J].Lithos,13:97-108.
Muller D and Groves D I.1995.Potassic igneous rocks and associatedgold-copper mineralization[M].Berlin:Springer-Verlag.1-210.
Niu B G,He Z J,Song B and Ren J S.2003.SHRIMP dating of theZhangjiakou volcanic series and its significance[J].Geological Bulletin of China,22(2):140-141.
No.704 Geological Team of Guangdong Province.2011.Internal detailedsurvey report of Tiantang polymetallic orefield exploration area[R].(in Chinese).
Peng J T,Hu R Z,Bi X W,Dai T M,Li Z L,Li X M,Shuang Y,YuanS D and Liu S R.2007.40Ar/39Ar isotopic dating of tinmineralization in Furong deposit of Hunan Province and its geologicalsignificance[J].Mineral Deposits,26(3):237-248(in Chinesewith English abstract).
Peng J T,Hu R Z,Yuan S D,Bi X W and Shen N P.2008.The timeranges of granitoid emplacement and related nonferrous metallicmineralization in southern Hunan[J].Geological Review,54(5):1-9(in Chinese with English abstract).
Shen R W,Hai T and Liu C M.2010.Analysis of potential polymetallicdeposits in the Yangchun Basin in Guangdong Province[J].Geologyand Exploration(Suppl.),46:1249-1255(in Chinese with Englishabstract).
Shu L S,Zhou X M,Deng P,Yu X Q,Wang B and Zu F P.2004.Geological features and tectonic evolution of Meso-Cenozoic Basins insoutheastern China[J].Grological Bulletin of China,23(9-10):876-884(in Chinese with English abstract).
Shu L S and Wang D Z.2006a.A comparison study of Basin and rangetectonics in the western North America and southeastern China[J].Geological Journal of China Universities,12(1):1-13(in Chinesewith English abstract).
Shu L S,Zhou X M,Deng P and Yu X Q.2006b.Principal geologicalfeatures of Nanling tectonic belt,South China[J].Geological Review,52(2):251-265(in Chinese with English abstract).
Si T H,Zheng C N and Huang D X.2004.The geological characteristicsand prospecting prospect of Tiantang chalcopyrite polymetallic deposit[J].West-China Exploration Engineering,(5):76-77.
Stein H J,Markey R J,Morgan J W,Du A D and Sun Y L.1997.Highly precise and accurate Re-Os ages for molybdenite from the East Qinling molybdenum belt,Shaanxi Province,China[J].Econ.Geol.,92:827-835.
Sun X M,Chen W,Wang M,Xue T,Sun K and Chen B H.2003.Dating of sediment hosted disseminated-type gold deposit by using40Ar/39Ar laser probe:A case study of Changkeng large-scale golddeposit,China[J].Chinese Sci.Bull.,48(12):1355-1358(inChinese).
Taira A.2001.Tectonic evolution of the Japanese island arc system[J].Annual Review of Earth and Planet Sciences,29:109-134.
Tang J X,Wang D H,Wang X W,Zhong K H,Ying L J,Zheng W B,Li F J,Guo N,Qin Z P,Yao X F,Li L,Wang Y and Tang X Q.2010.Geological features and metallogenic model of the Jiama copperpolymetallic deposit in Tibet[J].Acta Geoscientica Sinica,31(4):495-506(in Chinese with English abstract).
The National Geological Isotopic Ages Album Editing Group.1983.Thenational geological isotopic ages album(the third)[M].Beijing:Geological Publishing House.1-748(in Chinese).
Wan T F.1993.Studies on intraplate deformation and structural stressfield during the Mesozoic-Cenozoic era in eastern China and its application[M].Beijing:Geological Publishing House.1-103(in Chinese).
Wan T F and Zhu H.2002.Tectonics and environment change of mesocenozoic in China continent and its adjacent areas[J].Geoscience,16(2):107-120(in Chinese with English abstract).
Wang B,Shu L S and Yang Z Y.2006.Study of the early-middle Jurassic tectono-stratigraphy in the Jiangxi-Guangdong region,SE China[J].Journal of stratigraphy,30(1):42-49(in Chinese with Englishabstract).
Wang D H and Chen Y C.2001.A preliminary study on the metallogenicseries type of Fe-Cu-Pb-Zn ore deposits related to submarine volcanism and its origin[J].Mineral Deposits,20(2):112-118(in Chinese with English abstract).
Wang D H,Chen Y C,Xu Z G,Chen Z H,Shen B F,Tang Z L and PeiR F.2011a.Advance in the study of mineralization system and its application to assessment of mineral resources[J].Acta GeoscienticaSinica,32(4):385-395(in Chinese with English abstract).
Wang D H,Chen F W,Zhang Y Z,Lei Z H,Liang T,Wei L M,ChenZ H,Liu S B,Wang C H,Li H Q,Xu Y M,Zeng Z L,Xu J X,FuX J,Fan S K,Chen X Y,Jia B H and Yao G H.2011b.Mineralization potential of non-ferrous and precious metals and casestudy of comprehensive prospecting technology in Nanling[M].Beijing:Geological Publishing House.1-472(in Chinese).
Wang L K,Tan M T,Liu S X,Huang Z L and Li F C.2001.Copperand gold ore-controlling conditions of the Wuchuan-Sihui fracture beltand metallogenic prognosis[M].Beijing:Geological PublishingHouse.32-74.
Wang Y and Deng J F.2003.Geodynamic implication of petrochemicalfeatures of Yanshanian strongly peralumdious granitoids in WuchuanSihui fracture belt of Guangdong[J].Geotecionica et Metallogenia,27(1):56-63(in Chinese with English abstract).
Xu J X,Zeng Z L,Li X Q,Liu J S,Chen Z H,Liu S B,Guo C L andWang C H.2007.Geological characteristics and mineralization age ofthe Tongkengzhang molybdenum deposit in Xunwu County,southJiangxi Province,China[J].Acta Geologica Sinica,81(7):924-928(in Chinese with English abstract).
Xu X S.2008.Several problems worthy to be noticed in the research ofgranites and volcanic rocks in SE China[J].Geological Journal ofChina Universities,14(3):283-294(in Chinese with English abstract).
Yu J S,Gui X T and Li P Z.1988.Isotope and trace elementgeochemistry of granitoid plutons in Yangchun Basin,Guangdong[J].Guangdong Geology,13:1-10(in Chinese with English abstract).
Yuan S D,Peng J T,Hu R Z,Li H M,Shen N P and Zhang D L.2008.A precise U-Pb age on cassiterite from the Xianghualing tinpolymetallic deposit(Hunan,South China)[J].Mineralium Deposita,43:375-382.
Yuan S D,Peng J T,Hao S,Li H M,Geng J Z and Zhang D L.2011.In situ LA-MC-ICP-MS and ID-TIMS U-Pb geochronology of cassiteritein the giant Furong tin deposit,Hunan Province,South China:Newconstraints on the timing of tin-polymetallic mineralization[J].OreGeology Reviews,43:235-242.
Zhang D Q,Feng C Y,Li D X,She H Q and Dong Y J.2003.40Ar-39Ardating of adularia from Bitian sericite-adularia type epithermal Ag-Audeposit in Fujian Province and its geological significance[J].MineralDeposits,22(4):360-365(in Chinese with English abstract).
Zhang J J,Mei Y P,Wang D H and Li H Q.2008.Isochronology studyon the Xianglushan scheelite deposit in north Jiangxi Province and itsgeological significance[J].Acta Geologica Sinica,82(7):927-931(in Chinese with English abstract).
Zhang Q,Zhang B G,Pan J Y,Cao Y B,Hong D H and Yang Q J.1993.An isotopic tracing study of the materal source of the Chadongsilver-gold polymetallic deposit in western Guangdong Province[J].Mineral Deposits,12(4):349-357(in Chinese with English abstract).
Zhang Q Z.2010.Uperficial analysis on deposit-forming and mineralenrichment of veined W-Sn deposit in Xishan,Guangdong Province[J].China Science and Technology Information,(10):30-31(in Chinesewith English abstract).
Zhao D P.2004.Global tomographic images of mantle plumes and sub-ducting slabs:Insight into deep earth dynamics[J].Physics of theEarth and Planetary Interiors,146:3-34.
Zhao H J.2010.The mineralization mechanism and geochemistry of theTonglushan skarn Cu-Fe deposit,southeastern Hubei,China[D].Beijing:Thesis,Chinese Academy of Geological Sciences.66-79.
Zhao H J,Zheng W,Yu C F,Hu Y G and Tian Y.2012.Re-Os datingof molybdenite from the Shilu Cu(Mo)deposit in western GuangdongProvince and its geological implications[J].Geology in China,39(6):1604-1613(in Chinese with English abstract).
Zhao Z J,Ma D Q,Lin H K and Zhang X H.1985.Rebidium-Strontiumand oxygen isotopic composition of the two types of granitoids in Yangchun area,Guangdong province and discussion on their origin[J].Bull.Yichaag Iast.Geol.,Mineral Resources CAGS,89-97(in Chinese with English abstract).
Zheng W,Chen M H,Zhao H J,Hao H D,Luo D L,Hu Y G and ZhaoX M.2012.Characteristics of sulfides and S-Pb isotope compositionin the Tiantang Cu-Pb-Zn polymetallic deposit of Guangdong Provinceand their geological implications[J].Geology in China,39(6):1838-1854(in Chinese with English abstract).
Zheng W,Chen M H,Xu L G,Zhao H J,Ling S B,Wu Y,Hu Y G,Tian Y and Wu X D.2013a.Rb-Sr isochron age of Tiantang Cu-PbZn polymetallic deposit in Guangdong province and its geological significance[J].Mineral Deposits,32(2):259-272(in Chinese withEnglish abstract).
Zheng W,Chen M H,Zhao H J,Zhang D Y,Xu L G,Ling S B,Yao L,Yu M and Chang L Z.2013b.Skarn mineral characteristics of theTiantang Cu-Pb-Zn polymetallic deposi in Guangdong Province andtheir geological significance[J].Acta Petrologica et Mineralogica,32(1):23-40(in Chinese with English abstract).
Zheng W,Zhao H J,Chen M H,Xu L G,Liu J X,Luo D L and Hu YG.2013c.Re-Os isotopic dating of molybdenites from the YingwulingPolymetallic deposit in Guangdong province and its geological significance[J].Joural of Mineralogy and Petrology,33(3):38-46(inChinese with English abstract).
Zheng W,Chen M H,Zhao H J,Zhao C S,Hou K J,Li X M and ChangL Z.2013d.Zircon U-Pb geochronological and Hf isotopic constraintson petrogenesis of Yingwuling to tungsten polymetallic deposit inGuangdong Province and its geological significance[J].Acta Petrologica Sinica,29(12):4121-4135(in Chinese with English abstract).
Zheng W,Mao J W,Pirajno F,Zhao H J,Zhao C S,Mao Z H and WangY J.2015.Geochronology and geochemistry of the Shilu Cu-Mo de-posit in the Yunkai area,Guangdong Province,South China and itsimplication[J].Ore Geology Reviews,67:382-398.
Zhong J Q.2011.The geological characteristics of Yingwuling polymetallic ore deposit in Yangchun of Guangdong Province[J].Science&Technology Association Forum,2:98-99(in Chinese with Englishabstract).
Zhou T F,Fan Y and Yuan F.2008.Advances on petrogensis andmetallogeny study of the mineralizatlon belt of the middle and lowerreaches of the Yangtze River area[J].Acta Petrologica Sinica,24(8):1665-1678.(in Chinese with English abstract).
Zhou X M,Sun T,Shen W Z,Shu L S and Niu Y L.2006.Petrogenesisof Mesozoic granitoids and volcanic rocks in South China:A responseto tectonic evolution[J].Episodes,29:26-21.
蔡明海,彭松柏,孟祥金,刘国庆.2001.桂东-粤西地区中生代成矿规律及动力学机制探讨[J].华南地质与矿产,(2):35-42.
蔡明海,战明国,彭松柏,孟祥金,刘国庆.2002.云开地区中生代成矿地质背景及成矿动力学机制研究[J].矿床地质,21(3):254-269.
陈富文,李华芹,梅玉萍.2008.广西龙头山斑岩型金矿成岩成矿锆石SHRIMP U-Pb年代学研究[J].地质学报,82(7):921-926.
陈毓川,裴荣富,张宏良.1990.南岭地区与中生代花岗岩类有关的有色、稀有金属矿床地质[J].中国地质科学院院报,第20号:79-85.
陈毓川,王平安,秦克令,赵东宏,毛景文.1994.秦岭地区主要金属矿床成矿系列的划分及区域成矿规律探讨[J].矿床地质,13(4):289-298.
陈毓川,王登红,徐志刚,朱明玉.2006.对中国成矿体系的初步探讨[J].矿床地质,25(2):155-163.
陈毓川,王登红,朱裕生,徐志刚,任纪舜,翟裕生,常印佛,汤中立,裴荣富,滕吉文,邓晋福,胡云中,任天祥,沈保丰,王世称,肖克炎,彭润民,钱壮志,梅燕雄,杜建国,施俊法,张晓华,朱明玉,徐珏,薛春纪.2007.中国成矿体系与区域成矿评价[M].北京:地质出版社.
陈毓川,刘德权,唐延龄,王登红,董连慧,徐新,王晓地.2008.中国天山矿产及成矿体系[M].北京:地质出版社.1-1061.
陈毓川,王登红,徐志刚,黄凡.2014.华南区域成矿和中生代岩浆成矿规律概要[J].大地构造与成矿,38(2):219-229.
陈郑辉,陈毓川,王登红.2009.矿产资源潜力评价示范研究———以南岭东段钨矿资源潜力评价为例[M].北京:地质出版社.1-195
陈志中.1988.广东阳春锡山岩体的地质地球化学特征[J].中山大学学报(自然科学版),(01):1-12.
邓平,舒良树,余心起,王彬,谭正中,孙岩.2004.闽西-赣南早、中侏罗世盆地及其火山岩特征[J].岩石学报,20(3):521-532.
董树文,张岳桥,龙长兴,杨振宇,季强,胡建民,陈宣化.2007.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报,81(11):1449-1461.
耿红燕,徐夕生,O'Reilly S Y,赵明,孙涛.2006.粤西白垩纪火山-侵入岩浆活动及其地质意义[J].中国科学(D辑),36(7):601-617.
广东省704地质队.2011.天堂多金属矿内部详查报告[R].
广东省地质建设工程勘察院.2008.广东省阳春市鹦鹉岭铜多金属矿普查地质报告[R].
广东省有色金属地质局.2014.广东阳春铜多金属矿整装勘查区关键基础地质研究项目总体设计[R].
华仁民,陈培荣,张文兰,刘晓东,陆建军,林锦富,姚军明,戚华文,张展适,顾晟彦.2003.华南中、新生代与花岗岩类有关的成矿系统[J].中国科学(D辑),33(4):335-343.
华仁民,陈培荣,张文兰,陆建军.2005.论华南地区中生代3次大规模成矿作用[J].矿床地质,24(2):99-107.
贾军涛,王璞君,万晓樵.2008.松辽盆地断陷期白垩纪营城组的时代归属[J].地质论评,54(4):439-448.
李理,钟大赉,时秀朋,唐智博,宫红波,胡秋媛.2008.鲁西地区晚中生代以来伸展构造及其控矿作用[J].地质论评,54(4):449-458.
李献华,周汉文,刘颖,李寄,陈正宏,于津生,桂训唐.2000.粤西阳春中生代钾玄质侵入岩及其构造意义:Ⅰ.岩石学和同位素地质年代学[J].地球化学,29(6):513-520.
李献华,周汉文,刘颖,李寄,陈正宏,于津生,桂训唐.2001.粤西阳春中生代钾玄质侵入岩及其构造意义:Ⅱ.微量元素和SrNd同位素地球化学[J].地球化学,30(1):57-65.
李晓峰,Watanabe Y,华仁民,毛景文.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[J].矿床地质,82(5):625-640.
刘晓东,华仁民.2005.福建碧田金银铜矿床冰长石的40Ar-39Ar年龄[J].地质论评,51(2):151-155.
马大铨,赵子杰,林惠坤.1985.广东阳春盆地岗美-石型花岗岩类中包体的岩石特征及其成因[J].中国地质科学院宜昌地质矿产研究所所刊,10:59-72.
马东升,陈培荣.2006.华南中生代热隆起成矿与软流圈被动上涌[A].主编:陈骏.地质与地球化学研究进展[C].南京:南京大学出版社.224-235.
毛建仁,许乃政,胡青,邢光福,杨祝良.2004.福建省上杭-大田地区中生代成岩成矿作用与构造环境演化[J].岩石学报,20(2):285-296.
毛景文,谢桂青,李晓峰,张长青,梅燕雄.2004a.华南地区中生代大规模成矿作用与岩石圈多阶段伸展[J].地学前缘,11(1):45-55.
毛景文,Stein H,杜安道,周涛发,梅燕雄,李永峰,藏文栓,李进文.2004b.长江中下游地区铜金(钼)矿Re-Os年龄测定及其对成矿作用的指示[J].地质学报,78(1):121-131.
毛景文,谢桂青,张作衡,李晓峰,王义天,张长青,李永峰.2005.中国北方中生代大规模成矿作用的期次及其地球动力学背景[J].岩石学报,21(1):169-188.
毛景文,谢桂青,郭春丽,陈毓川.2007.南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景[J].岩石学报,23(10):2329-2338.
毛景文,谢桂青,郭春丽,袁顺达,程彦博,陈毓川.2008.华南地区中生代主要金属矿床时空分布规律和成矿环境[J].高校地质学报,14(4):510-526.
毛景文,谢桂青,程彦博,陈毓川.2009.华南地区中生代主要金属矿床模型[J].地质论评,55(3):347-354.
毛景文,陈懋弘,袁顺达,郭春丽.2011.华南地区钦杭成矿带地质特征和矿床时空分布规律[J].地质学报,85(5):636-658.
梅玉萍,杨红梅,段瑞春,张利国,蔡应雄,童喜润,谭娟娟,刘重芃,卢山松.2013.广东阳春锡山钨锡矿床成岩成矿年代学研究[J].地质学报,87(9):1370-1376.
牛宝贵,和政军,宋彪,任纪舜.2003.张家口组火山岩SHRIMP定年及其重大意义[J].地质通报,22(2):140-141.
彭建堂,胡瑞忠,毕献武,戴谟,李兆丽,李晓敏,双燕,袁顺达,刘世荣.2007.湖南芙蓉锡矿床40Ar/39Ar同位素年龄及地质意义[J].矿床地质,26(3):237-248.
彭建堂,胡瑞忠,袁顺达,毕献武,沈能平.2008.湘南中生代花岗质岩石成岩成矿的时限[J].地质论评,54(5):1-9.
全国同位素地质年龄数据汇编小组.1983.全国同位素地质年龄数据汇编(第三集)[M].北京:地质出版社.1-748.
沈睿文,海涛,刘昌明.2010.广东阳春盆地多金属找矿潜力浅析[J].地质与勘探,46(增刊):1249-1255.
舒良树,周新民,邓平,余心起,王彬,祖辅平.2004.中国东南部中、新生代盆地特征与构造演化[J].地质通报,23(9-10):876-884.
舒良树,王德滋.2006a.北美西部与中国东南部盆岭构造对比研究[J].高校地质学报,12(1):1-13.
舒良树,周新民,邓平,余心起.2006b.南岭构造带的基本地质特征[J].地质论评,52(2):251-265.
司徒宏,郑昌能,黄德鑫.2004.天堂铜多金属矿地质特征与找矿前景[J].西部探矿工程,(5):76-77.
孙晓明,陈文,王敏,薛婷,孙凯,陈炳辉.2003.微细浸染型金矿激光微区40Ar/39Ar等时线年龄测定:以长坑大型金矿为例[J].科学通报,48(12):1355-1358.
唐菊兴,王登红,汪雄武,钟康惠,应立娟,郑文宝,黎枫佶,郭娜,秦志鹏,姚晓峰,李磊,王友,唐晓倩.2010.西藏甲玛铜多金属矿矿床地质特征及其矿床模型[J].地球学报,31(4):495-506.
万天丰.1993.中国东部中、新生代板内变形,构造应力场及其应用[M].北京:地质出版社.1-103.
万天丰,朱鸿.2002.中国大陆及邻区中生代—新生代大地构造与环境变迁[J].现代地质,16(2):107-120.
汪洋,邓晋福.2003.广东吴川-四会断裂带燕山期强过铝质花岗岩岩石化学特征的地球动力学意义[J].大地构造与成矿学,27(1):56-63.
王彬,舒良树,杨振宇.2006.赣闽粤地区早、中侏罗世构造地层研究[J].地层学杂志,30(1):42-49.
王登红,陈毓川.2001.与海相火山作用有关的铁-铜-铅-锌矿床成矿系列类型及成因初探[J].矿床地质,20(2):112-118.
王登红,陈毓川,徐志刚,陈郑辉,沈保丰,汤中立,裴荣富.2011a.成矿体系的研究进展及其在成矿预测中的应用[J].地球学报,32(4):385-395.
王登红,陈富文,张永忠,雷泽恒,梁婷,韦龙明,陈郑辉,刘善宝,王成辉,李华芹,许以明,曾载淋,许建祥,傅旭杰,范森葵,陈祥云,贾宝华,姚根华.2011b.南岭地区有色-贵重金属成矿潜力及综合探测技术示范研究[M].北京:地质出版社.1-472.
王联魁,覃慕陶,刘师先,黄智龙,李富才.2001.吴川-四会断裂带铜金矿控矿条件和成矿预测[M].北京:地质出版社.32-74.
徐夕生.2008.华南花岗岩-火山岩成因研究的几个问题[J].高校地质学报,14(3):283-294.
许建祥,曾载淋,李雪琴,李雪琴,刘俊生,陈郑辉,刘善宝,郭春丽,王成辉.2007.江西寻乌铜坑嶂钼矿床地质特征及其成矿时代[J].地质学报,81(7);924-928.
于津生,桂训唐,李培忠.1988.广东阳春盆地花岗岩类同位素、微量元素地球化学研究[J].广东地质,13:1-10.
张德全,丰成友,李大新,佘宏全,董英君.2003.福建碧田矿床冰长石的40Ar-39Ar年龄及其地质意义[J].矿床地质,22(4):360-365.
张家菁,梅玉萍,王登红,李华芹.2008.赣北香炉山白钨矿床的同位素年代学研究及其地质意义[J].地质学报,82(7):927-931.
张乾,张宝贵,潘家永,曹裕波,洪笃豪,杨谦举.1993.粤西茶洞银金矿床矿质来源的同位素示踪研究[J].矿床地质,12(4):349-357.
张求知.2010.广东锡山矿区脉状钨锡矿床矿化富集规律及矿床成因浅析[J].中国科技信息,(10):30-31.
赵海杰.2010.湖北铜绿山夕卡岩型铜铁矿床地球化学及成矿机制[D].北京:中国地质科学院博士论文.66-79.
赵海杰,郑伟,余长发,胡耀国,田云.2012.粤西石铜钼矿床Re-Os同位素年龄及其地质意义[J].中国地质,39(6):1604-1613.
赵子杰,马大铨,林惠坤,张小豪.1985.广东阳春地区两类花岗岩类的铷-锶、氧同位素组成及其成因探讨[J].中国地质科学院宜昌地质矿产研究所,10:89-97.
郑伟,陈懋弘,赵海杰,郝宏达,罗大略,胡耀国,赵辛敏.2012.广东天堂铜铅锌多金属矿床矿物学、硫化物S-Pb同位素特征[J].中国地质,39(6):1838-1854.
郑伟,陈懋弘,徐林刚,赵海杰,凌世彬,吴越,胡耀国,田云,吴晓东.2013a.广东天堂铜铅锌多金属矿床Rb-Sr等时线年龄及其地质意义[J].矿床地质,32(2):259-272.
郑伟,陈懋弘,赵海杰,张东阳,徐林刚,凌世彬,姚磊,于淼,常利忠.2013b.广东省天堂铜铅锌多金属矿床矽卡岩矿物学特征及其地质意义[J].岩石矿物学杂志,32(1):23-40.
郑伟,赵海杰,陈懋弘,徐林刚,刘建新,罗大略,胡耀国.2013c广东鹦鹉岭多金属矿床辉钼矿的Re-Os同位素定年及其意义[J].矿物岩石,33(3):38-46.
郑伟,陈懋弘,赵海杰,赵财胜,侯可军,刘建新,李学孟,常利忠2013d.广东鹦鹉岭钨多金属矿床中黑云母花岗岩LA-ICP-MS锆石U-Pb定年和Hf同位素特征及其地质意义[J].岩石学报,29(12):4121-4135.
钟建桥.2011.广东阳春市鹦鹉岭多金属矿床地质特征[J].科协论坛,(2):98-99.
周涛发,范裕,袁峰.2008.长江中下游成矿带成岩成矿作用研究进展[J].岩石学报,24(8):1665-1678.
Cai M H,Zhan M G,Peng S B,Meng X J and Liu G Q.2002.Study ofMesozoic metallogenic geological setting and dynamic mechanism inYunkai area[J].Mineral Deposits,21(3):254-269(in Chinesewith English abstract).
Charvet J,Faure M,Fabbri O,Cluzel D and Lapierre H.1990.Accretion and collision during East-Asian margin building:A new insighton the Peri-Pacific orogenies[A].In:Wiley T J,Howell D G andWong F L,eds.Terrane ana lysis of China and the Pacific Rim[C].Circum-Pacific Council for Energy and Mineral Resources,EarthScience Series,13:161-190.
Chen F W,Li H Q and Mei Y P.2008.Zircon SHRIMP U-Pb chronology of diagenetic mineralization of the Longtoushan porphyry goldorefield,Gui County,Guangxi[J].Acta Geologica Sinica,82(7):921-926(in Chinese with English abstract).
Chen Y C,Pei R F and Zhang H L.1990.The Geology of nonferrous andrare metal deposits related to Mesozoic Granitoids in the Nanling region,China[J].Bulletin of the Chinese Academy of GeologicalSciences,20:79-85(in Chinese with English abstract).
Chen Y C,Wang P A,Qin K L,Zhao D H and Mao J W.1994.Metallgenic series of main ore deposits and regional metallogeny in theQinling area[J].Mineral Deposits,13(4):289-298(in Chinesewith English abstract).
Chen Y C,Wang D H,Xu Z G and Zhu M Y.2006.Preliminary study ofChinese mineralization system[J].Mineral Deposits,25(2):155-163(in Chinese with English abstract).
Chen Y C,Wang D H,Zhu Y S,Xu Z G,Zhai Y S,Chang Y F,TangZ L,Pei R F,Teng J W,Deng J F,Hu Y Z,Ren T X,Shen B F,Wang S C,Xiao K Y,Peng R M,Qian Z Z,Mei Y X,Du J G,ShiJ F,Zhang X H,Zhu M Y,Xu Y and Xue C J.2007.Chinesemineralizaiton system and assessment of rigional mineralization[M].Beijing:Geological Publishing House.1-462(in Chinese).
Chen Y C,Liu D Q,Tang Y L,Wang D H,Dong L H,Xu X and WangX D.2008.Mineral resources and mineralization system in Tianshan,China[M].Beijing:Geological Publishing House.1-1061(in Chinese).
Chen Y C,Wang D H,Xu Z G and Huang F.2014.Outline of regionametallogeny of ore deposits associated with the Mesozoic magmatism inSouth China[J].Geotectonica et Metallogenia,38(2):219-229(inChinese with English abstract).
Chen Z H,Chen Y C and Wang D H.2009.The demonstration studiesfor assessment of mineral resources potential[M].Beijing:GeologicaPublishing House.1-195(in Chinese).
Chen Z Z.1988.Geology-goehemistry charaeteristies of Xishan granitebody in Yangehun,Guangdong[J].Acta Scientiarum NaturaliumUniversitatis Sunyatseni,(01):1-12(in Chinese with English abstract).
Deng P,Shu L S,Yu X Q,Wang B,Tan Z Z and Sun Y.2004.EarlyMiddle Jurassic Basins and features of igneous rocks in the westernFujian-southern Jiangxi region[J].Acta Petrologica Sinica,20(3):521-532(in Chinese with English abstract).
Dong S W,Zhang Y Q,Long C X,Yang Z Y,Ji Q,Hu J M and Chen XH.2007.Jurassic tectonic revolution in China and new interpretationof the Yanshan movement[J].Acta Geologica Sinica,81(11):1449-1461(in Chinese with English abstract).
Faure M and Ishida K.1990.The Mid-Upper Jurassic olistostrome of thewest Philippines:A distinctive key-maker for the Palawan Block[J].J.Southeast Asian Earth Sci.,4:61-67.
Foley S F and Peccerillo A.1992.Potassic and ultrapotassic magmas andtheir origin[J].Lithos,28:181-185.
Fukao Y,Obayashi M,Inoue H and Nenbai M.1992.Subducting slabsstagnant in the Mantle Transition Zone[J].Journal of GeophysicaResearch,97:4809-4822.
Geng H Y,Xu X S,O'Reilly S Y,Zhao M and Sun T.2006.Cretaceousvolcanic-intrusive magmatism in western Guangdong and its geologicasignificance[J].Science in China(Series D),36(7):601-617(inChinese).
Geological Construction Engineering Institute of Guangdong Province.2008.Geological survey report in Yangchun copper-polymetallic orefield,Guangdong Province[R].(in Chinese).
Geology Bureau for Nonferrous Metals of Guangdong Province.2014.General design of critical fundermental geological research in Yangchuncopper polmetallic ore exploration area,Guangdong Province[R].(in Chinese).
Goldfarbl R J,Hart C,Davis G and Geoves D.2007.East Asian gold:Deciphering the anomaly of phanerozoic gold in Precambrian Cratons[J].Econ.Geol.,102:341-345.
Hider T W C.1976.Tectonic history of the western Pacific[A].In:Drake C L,ed.Geodynamics:Progress and prospects[C].Washington DC.American Geophysical Union.
Hua R M,Chen P R,Zhang W L,Liu X D,Lu J J,Lin J F,Yao J,M,Qi H W,Zhang Z S and Gu C Y.2003.Metallogenic systems relatedto Cenozoic and Mesozoic granitoids in South China[J].Science inChina(Series D),33(4):335-343(in Chinese).
Hua R M,Chen P R,Zhang W L and Lu J J.2005.Three major metallogenic events in Mesozoic in South China[J].Mineral Deposits,24(2):99-107(in Chinese with English abstract).
Huang H Y,Li X H,Li Z X and Li X W.2013.Intraplate crustalremelting as the genesis of Jurassic high-K granites in the coastal region of the Guangdong Province,SE China[J].Journal of AsianEarth Sciences 74,280-302.
Isozaki Y.1997.Jurassic accretion tectonics of Japan[J].The IslandArc,6:25-51.
Jia J T,Wang P J and Wan X Q.2008.Chronostratigraphy of theyingcheng formation in the Songliao Basin,Cretaceous,NE China[J].Geological Review,54(4):439-448(in Chinese with Englishabstract).
Lan T G,Fan H R,Santosh M,Hu F F,Yang K F,Yang Y H and LiuY S.2012.Early Jurassic high-K calc-alkaline and shoshonitic rocksfrom the Tongshi intrusive complex,eastern North China Craton:Implication for crust-mantle interaction and post-collisional magmatism[J].Lithos 140-141,183-199.
Li L,Zhong D L,Shi X P,Tang Z B,Gong H B and Hu Q Y.2008.Late Mesozoic extensional structure and its constrains on mineralizationin western Shandong[J].Geological Review,54(4):449-458(inChinese with English abstract).
Li X F,Yasushi W,Hua R M and Mao J W.2008.Mesozoic Cu-Mo-WSn mineralization and ridge/triple subduction in South China[J].Acta Geologica Sinica,82(5):625-640(in Chinese with English abstract).
Li X H,Zhou H W,Liu Y,Li J Y,Chen Z H,Yu J S and Gui X T.2000.Mesozoic shoshonitic intrusives in the Yangchun Basin,westernGuangdong,and their tectonic significance:I.Petrology and isotopegeochronology[J].Geochimica,29(6):513-520(in Chinese withEnglish abstract).
Li X H,Zhou H W,Liu Y,Li J Y,Chen Z H,Yu J S and Gui X T.2001.Mesozoic shoshonitic intrusives in Yangchun Basin,westernGuangdong,and their tectonic significance:Ⅱ.Trace elements andSr-Nd isotopes[J].Geochimica,30(1):57-65(in Chinese withEnglish abstract).
Liu X D and Hua R M.2005.40Ar/39Ar Dating of adularia from the Bitian gold-silver-copper deposit,Fujian Province[J].Geological Review,51(2):151-155(in Chinese with English abstract).
Ma D Q,Zhao Z J,Lin H K and Zhang X H.1985.Petrographical studyof the enclaves from the Gangwei-Shilu-type granitoids in YangchunBasin of Guangdong and adiscussion in their genesis[J].Bull.Yichang Inst.Geol.Mineral Resoures CAGS,10:59-72(in Chinesewith English abstract).
Ma D S and Chen P R.2006.The Mesozoic thermal-uplift metallogenesisand passive up-welling of asthenosphere in South China[A].In:ChenJ,ed.Press in geological and geochemical researches[C].Nanjing:Press of Nanjing University.224-235(in Chinese).
Mao J R,Xu N Z,Hu Q,Xing G F and Yang Z L.2004.The Mesozoicrock-forming and ore-forming processes and tectonic environment evolusion in Shanghang-Datian region,Fujian[J].Acta Petrologica Sinica,20(2):285-296(in Chinese with English abstract).
Mao J W,Xie G Q,Li X F,Zhang C Q and Mei Y X.2004a.Mesozoiclarge scale mineralization and multiple lithospheric extension in SouthChina[J].Earth Science Frontiers,11(1):45-55(in Chinese withEnglish abstract).
Mao J W,Stein H,Du A D,Zhou T F,Mei Y X,Li Y F,Zang W Q andLi J W.2004b.Molybdenite Re-Os precise dating for molybdenite from Cu-Au-Mo deposits in the middle-lower reaches of YangtzeRiver Belt and its implications for mineralization[J].Acta GeologicaSinica,78(1):121-131(in Chinese with English abstract).
Mao J W,Xie G Q,Zhang Z H,Li X F,Wang Y T,Zhang C Q and LiY F.2005.Mesozoic large-scale metallogenic pulses in North Chinaand corresponding geodynamic settings[J].Acta Petrologica Sinica,21(1):169-188(in Chinese with English abstract).
Mao J W,Wang Y T,Lehmann B,Yu J J,Du A D,Mei Y X,Li Y F,Zang W S,Stein H J and Zhou T F.2006.Molybdenite Re-Os andalbite40Ar/39Ar dating of Cu-Au-Mo and magnetite porphyry systemsin the Yangtze River Valley and metallogenic implications[J].OreGeology Reviews,29:307-324.
Mao J W,Xie G Q,Guo C L and Chen Y C.2007.Large-scale tungstentin mineralization in the Nanling region,South China:Metallogenic ages and corresponding geodynamic processes[J].Acta PetrologicaSinica,23(10):2329-2338(in Chinese with English abstract).
Mao J W,Xie G Q,Guo C L,Yuan S D,Cheng Y B and Chen Y C.2008.Spatial-Temporal distribution of Mesozoic ore deposits in SouthChina and their metallogenic settings[J].Geological Journal of ChinaUniversities,14(4):510-526(in Chinese with English abstract).
Mao J W,Xie G Q,Bierlein F,Ye H S,Qu W J,Du A D,Pirajno F,LH M,Guo B J,Li Y F and Yang Z Q.2008a.Tectonic implicationsfrom Re-Os dating of Mesozoic molybdenum deposits in the East Qinling-Dabie Orogenic Belt[J].Geochim.Cosmochim.Acta,72:4607-4626.
Mao J W,Wang Y T,Li H M,Pirajno F,Zhang C Q and Wang R T.2008b.The relationship of mantle-derived fluids to gold metallogenesis in the Jiaodong Peninsula:Evidence from D-O-C-S isotope systematic[J].Ore Geology Reviews,33:361-381.
Mao J W,Xie G Q,Cheng Y B and Chen Y C.2009.Mineral deposimodels of Mesozoic ore deposits in South China[J].Geological Review,55(3):347-354(in Chinese with English abstract).
Mao J W,Pirajno F and Cook N.2011.Mesozoic metallogeny in EasChina and corresponding geodynamic settings-An introduction to thespecial issue[J].Ore Geology Reviews,43:1-7.
Mao J W,Chen M H,Yuan S D and Guo C L.2011.Geological characteristics of the Qinhang(or Shihang)Metallogenic Belt in SouthChina and spatial-temporal distribution regularity of mineral deposits[J].Acta Geologica Sinica,85(5):636-658(in Chinese with English abstract).
Mao J W,Cheng Y B,Chen M H and Pirajno F.2013.Major types andtime-space distribution of Mesozoic ore deposits in South China andtheir geodynamic settings[J].Miner Deposita,48:267-294.
Mao J W,Pirajno F,Lehmann B,Luo M C and Berzina A.2014.Distribution of porphyry deposits in the Eurasian continent and their corresponding tectonic settings[J].Journal of Asian Earth Sciences,79:576-584.
Maruyama S and Seno T.1986.Orogeny and relative plate motion:Example of the Japanese Islands[J].Tectonophysics,127:305-329.
Mei Y P,Yang H M,Duan R C,Zhang L G,Cai Y X,Tong X R,TanJ J,Liu C P and Lu S S.2013.Diagenetic and metallogenic geochronlogy study of the Xishan W-Sn ore deposit in Yangchuang oGuangdong Province[J].Acta Geologica Sinica,87(9):1370-1376(in Chinese with English abstract).
Moore C W.1989.Mesozoic and Cenozoic paleographic development othe Pacific region[J].Abstract,28th IGC(2),Washington DC.USA:GAS Press.455-456.
Morrison G W.1980.Characteristics and tectonic setting of the shoshoniterock association[J].Lithos,13:97-108.
Muller D and Groves D I.1995.Potassic igneous rocks and associatedgold-copper mineralization[M].Berlin:Springer-Verlag.1-210.
Niu B G,He Z J,Song B and Ren J S.2003.SHRIMP dating of theZhangjiakou volcanic series and its significance[J].Geological Bulletin of China,22(2):140-141.
No.704 Geological Team of Guangdong Province.2011.Internal detailedsurvey report of Tiantang polymetallic orefield exploration area[R].(in Chinese).
Peng J T,Hu R Z,Bi X W,Dai T M,Li Z L,Li X M,Shuang Y,YuanS D and Liu S R.2007.40Ar/39Ar isotopic dating of tinmineralization in Furong deposit of Hunan Province and its geologicalsignificance[J].Mineral Deposits,26(3):237-248(in Chinesewith English abstract).
Peng J T,Hu R Z,Yuan S D,Bi X W and Shen N P.2008.The timeranges of granitoid emplacement and related nonferrous metallicmineralization in southern Hunan[J].Geological Review,54(5):1-9(in Chinese with English abstract).
Shen R W,Hai T and Liu C M.2010.Analysis of potential polymetallicdeposits in the Yangchun Basin in Guangdong Province[J].Geologyand Exploration(Suppl.),46:1249-1255(in Chinese with Englishabstract).
Shu L S,Zhou X M,Deng P,Yu X Q,Wang B and Zu F P.2004.Geological features and tectonic evolution of Meso-Cenozoic Basins insoutheastern China[J].Grological Bulletin of China,23(9-10):876-884(in Chinese with English abstract).
Shu L S and Wang D Z.2006a.A comparison study of Basin and rangetectonics in the western North America and southeastern China[J].Geological Journal of China Universities,12(1):1-13(in Chinesewith English abstract).
Shu L S,Zhou X M,Deng P and Yu X Q.2006b.Principal geologicalfeatures of Nanling tectonic belt,South China[J].Geological Review,52(2):251-265(in Chinese with English abstract).
Si T H,Zheng C N and Huang D X.2004.The geological characteristicsand prospecting prospect of Tiantang chalcopyrite polymetallic deposit[J].West-China Exploration Engineering,(5):76-77.
Stein H J,Markey R J,Morgan J W,Du A D and Sun Y L.1997.Highly precise and accurate Re-Os ages for molybdenite from the East Qinling molybdenum belt,Shaanxi Province,China[J].Econ.Geol.,92:827-835.
Sun X M,Chen W,Wang M,Xue T,Sun K and Chen B H.2003.Dating of sediment hosted disseminated-type gold deposit by using40Ar/39Ar laser probe:A case study of Changkeng large-scale golddeposit,China[J].Chinese Sci.Bull.,48(12):1355-1358(inChinese).
Taira A.2001.Tectonic evolution of the Japanese island arc system[J].Annual Review of Earth and Planet Sciences,29:109-134.
Tang J X,Wang D H,Wang X W,Zhong K H,Ying L J,Zheng W B,Li F J,Guo N,Qin Z P,Yao X F,Li L,Wang Y and Tang X Q.2010.Geological features and metallogenic model of the Jiama copperpolymetallic deposit in Tibet[J].Acta Geoscientica Sinica,31(4):495-506(in Chinese with English abstract).
The National Geological Isotopic Ages Album Editing Group.1983.Thenational geological isotopic ages album(the third)[M].Beijing:Geological Publishing House.1-748(in Chinese).
Wan T F.1993.Studies on intraplate deformation and structural stressfield during the Mesozoic-Cenozoic era in eastern China and its application[M].Beijing:Geological Publishing House.1-103(in Chinese).
Wan T F and Zhu H.2002.Tectonics and environment change of mesocenozoic in China continent and its adjacent areas[J].Geoscience,16(2):107-120(in Chinese with English abstract).
Wang B,Shu L S and Yang Z Y.2006.Study of the early-middle Jurassic tectono-stratigraphy in the Jiangxi-Guangdong region,SE China[J].Journal of stratigraphy,30(1):42-49(in Chinese with Englishabstract).
Wang D H and Chen Y C.2001.A preliminary study on the metallogenicseries type of Fe-Cu-Pb-Zn ore deposits related to submarine volcanism and its origin[J].Mineral Deposits,20(2):112-118(in Chinese with English abstract).
Wang D H,Chen Y C,Xu Z G,Chen Z H,Shen B F,Tang Z L and PeiR F.2011a.Advance in the study of mineralization system and its application to assessment of mineral resources[J].Acta GeoscienticaSinica,32(4):385-395(in Chinese with English abstract).
Wang D H,Chen F W,Zhang Y Z,Lei Z H,Liang T,Wei L M,ChenZ H,Liu S B,Wang C H,Li H Q,Xu Y M,Zeng Z L,Xu J X,FuX J,Fan S K,Chen X Y,Jia B H and Yao G H.2011b.Mineralization potential of non-ferrous and precious metals and casestudy of comprehensive prospecting technology in Nanling[M].Beijing:Geological Publishing House.1-472(in Chinese).
Wang L K,Tan M T,Liu S X,Huang Z L and Li F C.2001.Copperand gold ore-controlling conditions of the Wuchuan-Sihui fracture beltand metallogenic prognosis[M].Beijing:Geological PublishingHouse.32-74.
Wang Y and Deng J F.2003.Geodynamic implication of petrochemicalfeatures of Yanshanian strongly peralumdious granitoids in WuchuanSihui fracture belt of Guangdong[J].Geotecionica et Metallogenia,27(1):56-63(in Chinese with English abstract).
Xu J X,Zeng Z L,Li X Q,Liu J S,Chen Z H,Liu S B,Guo C L andWang C H.2007.Geological characteristics and mineralization age ofthe Tongkengzhang molybdenum deposit in Xunwu County,southJiangxi Province,China[J].Acta Geologica Sinica,81(7):924-928(in Chinese with English abstract).
Xu X S.2008.Several problems worthy to be noticed in the research ofgranites and volcanic rocks in SE China[J].Geological Journal ofChina Universities,14(3):283-294(in Chinese with English abstract).
Yu J S,Gui X T and Li P Z.1988.Isotope and trace elementgeochemistry of granitoid plutons in Yangchun Basin,Guangdong[J].Guangdong Geology,13:1-10(in Chinese with English abstract).
Yuan S D,Peng J T,Hu R Z,Li H M,Shen N P and Zhang D L.2008.A precise U-Pb age on cassiterite from the Xianghualing tinpolymetallic deposit(Hunan,South China)[J].Mineralium Deposita,43:375-382.
Yuan S D,Peng J T,Hao S,Li H M,Geng J Z and Zhang D L.2011.In situ LA-MC-ICP-MS and ID-TIMS U-Pb geochronology of cassiteritein the giant Furong tin deposit,Hunan Province,South China:Newconstraints on the timing of tin-polymetallic mineralization[J].OreGeology Reviews,43:235-242.
Zhang D Q,Feng C Y,Li D X,She H Q and Dong Y J.2003.40Ar-39Ardating of adularia from Bitian sericite-adularia type epithermal Ag-Audeposit in Fujian Province and its geological significance[J].MineralDeposits,22(4):360-365(in Chinese with English abstract).
Zhang J J,Mei Y P,Wang D H and Li H Q.2008.Isochronology studyon the Xianglushan scheelite deposit in north Jiangxi Province and itsgeological significance[J].Acta Geologica Sinica,82(7):927-931(in Chinese with English abstract).
Zhang Q,Zhang B G,Pan J Y,Cao Y B,Hong D H and Yang Q J.1993.An isotopic tracing study of the materal source of the Chadongsilver-gold polymetallic deposit in western Guangdong Province[J].Mineral Deposits,12(4):349-357(in Chinese with English abstract).
Zhang Q Z.2010.Uperficial analysis on deposit-forming and mineralenrichment of veined W-Sn deposit in Xishan,Guangdong Province[J].China Science and Technology Information,(10):30-31(in Chinesewith English abstract).
Zhao D P.2004.Global tomographic images of mantle plumes and sub-ducting slabs:Insight into deep earth dynamics[J].Physics of theEarth and Planetary Interiors,146:3-34.
Zhao H J.2010.The mineralization mechanism and geochemistry of theTonglushan skarn Cu-Fe deposit,southeastern Hubei,China[D].Beijing:Thesis,Chinese Academy of Geological Sciences.66-79.
Zhao H J,Zheng W,Yu C F,Hu Y G and Tian Y.2012.Re-Os datingof molybdenite from the Shilu Cu(Mo)deposit in western GuangdongProvince and its geological implications[J].Geology in China,39(6):1604-1613(in Chinese with English abstract).
Zhao Z J,Ma D Q,Lin H K and Zhang X H.1985.Rebidium-Strontiumand oxygen isotopic composition of the two types of granitoids in Yangchun area,Guangdong province and discussion on their origin[J].Bull.Yichaag Iast.Geol.,Mineral Resources CAGS,89-97(in Chinese with English abstract).
Zheng W,Chen M H,Zhao H J,Hao H D,Luo D L,Hu Y G and ZhaoX M.2012.Characteristics of sulfides and S-Pb isotope compositionin the Tiantang Cu-Pb-Zn polymetallic deposit of Guangdong Provinceand their geological implications[J].Geology in China,39(6):1838-1854(in Chinese with English abstract).
Zheng W,Chen M H,Xu L G,Zhao H J,Ling S B,Wu Y,Hu Y G,Tian Y and Wu X D.2013a.Rb-Sr isochron age of Tiantang Cu-PbZn polymetallic deposit in Guangdong province and its geological significance[J].Mineral Deposits,32(2):259-272(in Chinese withEnglish abstract).
Zheng W,Chen M H,Zhao H J,Zhang D Y,Xu L G,Ling S B,Yao L,Yu M and Chang L Z.2013b.Skarn mineral characteristics of theTiantang Cu-Pb-Zn polymetallic deposi in Guangdong Province andtheir geological significance[J].Acta Petrologica et Mineralogica,32(1):23-40(in Chinese with English abstract).
Zheng W,Zhao H J,Chen M H,Xu L G,Liu J X,Luo D L and Hu YG.2013c.Re-Os isotopic dating of molybdenites from the YingwulingPolymetallic deposit in Guangdong province and its geological significance[J].Joural of Mineralogy and Petrology,33(3):38-46(inChinese with English abstract).
Zheng W,Chen M H,Zhao H J,Zhao C S,Hou K J,Li X M and ChangL Z.2013d.Zircon U-Pb geochronological and Hf isotopic constraintson petrogenesis of Yingwuling to tungsten polymetallic deposit inGuangdong Province and its geological significance[J].Acta Petrologica Sinica,29(12):4121-4135(in Chinese with English abstract).
Zheng W,Mao J W,Pirajno F,Zhao H J,Zhao C S,Mao Z H and WangY J.2015.Geochronology and geochemistry of the Shilu Cu-Mo de-posit in the Yunkai area,Guangdong Province,South China and itsimplication[J].Ore Geology Reviews,67:382-398.
Zhong J Q.2011.The geological characteristics of Yingwuling polymetallic ore deposit in Yangchun of Guangdong Province[J].Science&Technology Association Forum,2:98-99(in Chinese with Englishabstract).
Zhou T F,Fan Y and Yuan F.2008.Advances on petrogensis andmetallogeny study of the mineralizatlon belt of the middle and lowerreaches of the Yangtze River area[J].Acta Petrologica Sinica,24(8):1665-1678.(in Chinese with English abstract).
Zhou X M,Sun T,Shen W Z,Shu L S and Niu Y L.2006.Petrogenesisof Mesozoic granitoids and volcanic rocks in South China:A responseto tectonic evolution[J].Episodes,29:26-21.
蔡明海,彭松柏,孟祥金,刘国庆.2001.桂东-粤西地区中生代成矿规律及动力学机制探讨[J].华南地质与矿产,(2):35-42.
蔡明海,战明国,彭松柏,孟祥金,刘国庆.2002.云开地区中生代成矿地质背景及成矿动力学机制研究[J].矿床地质,21(3):254-269.
陈富文,李华芹,梅玉萍.2008.广西龙头山斑岩型金矿成岩成矿锆石SHRIMP U-Pb年代学研究[J].地质学报,82(7):921-926.
陈毓川,裴荣富,张宏良.1990.南岭地区与中生代花岗岩类有关的有色、稀有金属矿床地质[J].中国地质科学院院报,第20号:79-85.
陈毓川,王平安,秦克令,赵东宏,毛景文.1994.秦岭地区主要金属矿床成矿系列的划分及区域成矿规律探讨[J].矿床地质,13(4):289-298.
陈毓川,王登红,徐志刚,朱明玉.2006.对中国成矿体系的初步探讨[J].矿床地质,25(2):155-163.
陈毓川,王登红,朱裕生,徐志刚,任纪舜,翟裕生,常印佛,汤中立,裴荣富,滕吉文,邓晋福,胡云中,任天祥,沈保丰,王世称,肖克炎,彭润民,钱壮志,梅燕雄,杜建国,施俊法,张晓华,朱明玉,徐珏,薛春纪.2007.中国成矿体系与区域成矿评价[M].北京:地质出版社.
陈毓川,刘德权,唐延龄,王登红,董连慧,徐新,王晓地.2008.中国天山矿产及成矿体系[M].北京:地质出版社.1-1061.
陈毓川,王登红,徐志刚,黄凡.2014.华南区域成矿和中生代岩浆成矿规律概要[J].大地构造与成矿,38(2):219-229.
陈郑辉,陈毓川,王登红.2009.矿产资源潜力评价示范研究———以南岭东段钨矿资源潜力评价为例[M].北京:地质出版社.1-195
陈志中.1988.广东阳春锡山岩体的地质地球化学特征[J].中山大学学报(自然科学版),(01):1-12.
邓平,舒良树,余心起,王彬,谭正中,孙岩.2004.闽西-赣南早、中侏罗世盆地及其火山岩特征[J].岩石学报,20(3):521-532.
董树文,张岳桥,龙长兴,杨振宇,季强,胡建民,陈宣化.2007.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报,81(11):1449-1461.
耿红燕,徐夕生,O'Reilly S Y,赵明,孙涛.2006.粤西白垩纪火山-侵入岩浆活动及其地质意义[J].中国科学(D辑),36(7):601-617.
广东省704地质队.2011.天堂多金属矿内部详查报告[R].
广东省地质建设工程勘察院.2008.广东省阳春市鹦鹉岭铜多金属矿普查地质报告[R].
广东省有色金属地质局.2014.广东阳春铜多金属矿整装勘查区关键基础地质研究项目总体设计[R].
华仁民,陈培荣,张文兰,刘晓东,陆建军,林锦富,姚军明,戚华文,张展适,顾晟彦.2003.华南中、新生代与花岗岩类有关的成矿系统[J].中国科学(D辑),33(4):335-343.
华仁民,陈培荣,张文兰,陆建军.2005.论华南地区中生代3次大规模成矿作用[J].矿床地质,24(2):99-107.
贾军涛,王璞君,万晓樵.2008.松辽盆地断陷期白垩纪营城组的时代归属[J].地质论评,54(4):439-448.
李理,钟大赉,时秀朋,唐智博,宫红波,胡秋媛.2008.鲁西地区晚中生代以来伸展构造及其控矿作用[J].地质论评,54(4):449-458.
李献华,周汉文,刘颖,李寄,陈正宏,于津生,桂训唐.2000.粤西阳春中生代钾玄质侵入岩及其构造意义:Ⅰ.岩石学和同位素地质年代学[J].地球化学,29(6):513-520.
李献华,周汉文,刘颖,李寄,陈正宏,于津生,桂训唐.2001.粤西阳春中生代钾玄质侵入岩及其构造意义:Ⅱ.微量元素和SrNd同位素地球化学[J].地球化学,30(1):57-65.
李晓峰,Watanabe Y,华仁民,毛景文.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[J].矿床地质,82(5):625-640.
刘晓东,华仁民.2005.福建碧田金银铜矿床冰长石的40Ar-39Ar年龄[J].地质论评,51(2):151-155.
马大铨,赵子杰,林惠坤.1985.广东阳春盆地岗美-石型花岗岩类中包体的岩石特征及其成因[J].中国地质科学院宜昌地质矿产研究所所刊,10:59-72.
马东升,陈培荣.2006.华南中生代热隆起成矿与软流圈被动上涌[A].主编:陈骏.地质与地球化学研究进展[C].南京:南京大学出版社.224-235.
毛建仁,许乃政,胡青,邢光福,杨祝良.2004.福建省上杭-大田地区中生代成岩成矿作用与构造环境演化[J].岩石学报,20(2):285-296.
毛景文,谢桂青,李晓峰,张长青,梅燕雄.2004a.华南地区中生代大规模成矿作用与岩石圈多阶段伸展[J].地学前缘,11(1):45-55.
毛景文,Stein H,杜安道,周涛发,梅燕雄,李永峰,藏文栓,李进文.2004b.长江中下游地区铜金(钼)矿Re-Os年龄测定及其对成矿作用的指示[J].地质学报,78(1):121-131.
毛景文,谢桂青,张作衡,李晓峰,王义天,张长青,李永峰.2005.中国北方中生代大规模成矿作用的期次及其地球动力学背景[J].岩石学报,21(1):169-188.
毛景文,谢桂青,郭春丽,陈毓川.2007.南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景[J].岩石学报,23(10):2329-2338.
毛景文,谢桂青,郭春丽,袁顺达,程彦博,陈毓川.2008.华南地区中生代主要金属矿床时空分布规律和成矿环境[J].高校地质学报,14(4):510-526.
毛景文,谢桂青,程彦博,陈毓川.2009.华南地区中生代主要金属矿床模型[J].地质论评,55(3):347-354.
毛景文,陈懋弘,袁顺达,郭春丽.2011.华南地区钦杭成矿带地质特征和矿床时空分布规律[J].地质学报,85(5):636-658.
梅玉萍,杨红梅,段瑞春,张利国,蔡应雄,童喜润,谭娟娟,刘重芃,卢山松.2013.广东阳春锡山钨锡矿床成岩成矿年代学研究[J].地质学报,87(9):1370-1376.
牛宝贵,和政军,宋彪,任纪舜.2003.张家口组火山岩SHRIMP定年及其重大意义[J].地质通报,22(2):140-141.
彭建堂,胡瑞忠,毕献武,戴谟,李兆丽,李晓敏,双燕,袁顺达,刘世荣.2007.湖南芙蓉锡矿床40Ar/39Ar同位素年龄及地质意义[J].矿床地质,26(3):237-248.
彭建堂,胡瑞忠,袁顺达,毕献武,沈能平.2008.湘南中生代花岗质岩石成岩成矿的时限[J].地质论评,54(5):1-9.
全国同位素地质年龄数据汇编小组.1983.全国同位素地质年龄数据汇编(第三集)[M].北京:地质出版社.1-748.
沈睿文,海涛,刘昌明.2010.广东阳春盆地多金属找矿潜力浅析[J].地质与勘探,46(增刊):1249-1255.
舒良树,周新民,邓平,余心起,王彬,祖辅平.2004.中国东南部中、新生代盆地特征与构造演化[J].地质通报,23(9-10):876-884.
舒良树,王德滋.2006a.北美西部与中国东南部盆岭构造对比研究[J].高校地质学报,12(1):1-13.
舒良树,周新民,邓平,余心起.2006b.南岭构造带的基本地质特征[J].地质论评,52(2):251-265.
司徒宏,郑昌能,黄德鑫.2004.天堂铜多金属矿地质特征与找矿前景[J].西部探矿工程,(5):76-77.
孙晓明,陈文,王敏,薛婷,孙凯,陈炳辉.2003.微细浸染型金矿激光微区40Ar/39Ar等时线年龄测定:以长坑大型金矿为例[J].科学通报,48(12):1355-1358.
唐菊兴,王登红,汪雄武,钟康惠,应立娟,郑文宝,黎枫佶,郭娜,秦志鹏,姚晓峰,李磊,王友,唐晓倩.2010.西藏甲玛铜多金属矿矿床地质特征及其矿床模型[J].地球学报,31(4):495-506.
万天丰.1993.中国东部中、新生代板内变形,构造应力场及其应用[M].北京:地质出版社.1-103.
万天丰,朱鸿.2002.中国大陆及邻区中生代—新生代大地构造与环境变迁[J].现代地质,16(2):107-120.
汪洋,邓晋福.2003.广东吴川-四会断裂带燕山期强过铝质花岗岩岩石化学特征的地球动力学意义[J].大地构造与成矿学,27(1):56-63.
王彬,舒良树,杨振宇.2006.赣闽粤地区早、中侏罗世构造地层研究[J].地层学杂志,30(1):42-49.
王登红,陈毓川.2001.与海相火山作用有关的铁-铜-铅-锌矿床成矿系列类型及成因初探[J].矿床地质,20(2):112-118.
王登红,陈毓川,徐志刚,陈郑辉,沈保丰,汤中立,裴荣富.2011a.成矿体系的研究进展及其在成矿预测中的应用[J].地球学报,32(4):385-395.
王登红,陈富文,张永忠,雷泽恒,梁婷,韦龙明,陈郑辉,刘善宝,王成辉,李华芹,许以明,曾载淋,许建祥,傅旭杰,范森葵,陈祥云,贾宝华,姚根华.2011b.南岭地区有色-贵重金属成矿潜力及综合探测技术示范研究[M].北京:地质出版社.1-472.
王联魁,覃慕陶,刘师先,黄智龙,李富才.2001.吴川-四会断裂带铜金矿控矿条件和成矿预测[M].北京:地质出版社.32-74.
徐夕生.2008.华南花岗岩-火山岩成因研究的几个问题[J].高校地质学报,14(3):283-294.
许建祥,曾载淋,李雪琴,李雪琴,刘俊生,陈郑辉,刘善宝,郭春丽,王成辉.2007.江西寻乌铜坑嶂钼矿床地质特征及其成矿时代[J].地质学报,81(7);924-928.
于津生,桂训唐,李培忠.1988.广东阳春盆地花岗岩类同位素、微量元素地球化学研究[J].广东地质,13:1-10.
张德全,丰成友,李大新,佘宏全,董英君.2003.福建碧田矿床冰长石的40Ar-39Ar年龄及其地质意义[J].矿床地质,22(4):360-365.
张家菁,梅玉萍,王登红,李华芹.2008.赣北香炉山白钨矿床的同位素年代学研究及其地质意义[J].地质学报,82(7):927-931.
张乾,张宝贵,潘家永,曹裕波,洪笃豪,杨谦举.1993.粤西茶洞银金矿床矿质来源的同位素示踪研究[J].矿床地质,12(4):349-357.
张求知.2010.广东锡山矿区脉状钨锡矿床矿化富集规律及矿床成因浅析[J].中国科技信息,(10):30-31.
赵海杰.2010.湖北铜绿山夕卡岩型铜铁矿床地球化学及成矿机制[D].北京:中国地质科学院博士论文.66-79.
赵海杰,郑伟,余长发,胡耀国,田云.2012.粤西石铜钼矿床Re-Os同位素年龄及其地质意义[J].中国地质,39(6):1604-1613.
赵子杰,马大铨,林惠坤,张小豪.1985.广东阳春地区两类花岗岩类的铷-锶、氧同位素组成及其成因探讨[J].中国地质科学院宜昌地质矿产研究所,10:89-97.
郑伟,陈懋弘,赵海杰,郝宏达,罗大略,胡耀国,赵辛敏.2012.广东天堂铜铅锌多金属矿床矿物学、硫化物S-Pb同位素特征[J].中国地质,39(6):1838-1854.
郑伟,陈懋弘,徐林刚,赵海杰,凌世彬,吴越,胡耀国,田云,吴晓东.2013a.广东天堂铜铅锌多金属矿床Rb-Sr等时线年龄及其地质意义[J].矿床地质,32(2):259-272.
郑伟,陈懋弘,赵海杰,张东阳,徐林刚,凌世彬,姚磊,于淼,常利忠.2013b.广东省天堂铜铅锌多金属矿床矽卡岩矿物学特征及其地质意义[J].岩石矿物学杂志,32(1):23-40.
郑伟,赵海杰,陈懋弘,徐林刚,刘建新,罗大略,胡耀国.2013c广东鹦鹉岭多金属矿床辉钼矿的Re-Os同位素定年及其意义[J].矿物岩石,33(3):38-46.
郑伟,陈懋弘,赵海杰,赵财胜,侯可军,刘建新,李学孟,常利忠2013d.广东鹦鹉岭钨多金属矿床中黑云母花岗岩LA-ICP-MS锆石U-Pb定年和Hf同位素特征及其地质意义[J].岩石学报,29(12):4121-4135.
钟建桥.2011.广东阳春市鹦鹉岭多金属矿床地质特征[J].科协论坛,(2):98-99.
周涛发,范裕,袁峰.2008.长江中下游成矿带成岩成矿作用研究进展[J].岩石学报,24(8):1665-1678.