右江褶皱带东南缘西大明山矿集区燕山期长英质岩浆锆石SHRIMP原位氧同位素组成与地质意义
|
摘要
右江褶皱带晚白垩世岩浆岩的物质来源和成因机制及其相关的大规模Sn-W多金属成矿作用是目前研究的热点和前沿问题之一。本文在已获得锆石U-Pb年龄及Hf同位素基础上,对广西西大明山地区酸性岩浆进行了锆石SHRIMP氧同位素研究。石英斑岩δ~(18)O_(Zrn)值为5.31‰~9.31‰(平均值为7.61±2.17‰)、绢英岩化黑云母花岗岩δ~(18)O_(Zrn)值为7.11‰~9.79‰(平均值为8.36±1.33‰)、细粒黑云母花岗岩δ~(18)O_(Zrn)值为5.06‰~9.27‰(平均值为7.73±2.23‰)、中粒黑云母花岗岩δ~(18)O_(Zrn)值为5.06‰~9.27‰(平均值为7.73±2.23‰)二长花岗岩δ~(18)O_(Zrn)值为5.48‰~10.99‰(平均值为7.55±2.77‰)。测试结果显示广西西大明山地区酸性岩浆锆石氧同位素普遍具有双峰式分布特征且Hf-O同位素组成构成负相关性,暗示地壳组份和富集地幔两端元混合的特征。Hf-O同位素特征指示酸性岩浆岩源主要来自古老的地壳,并混有部分幔源物质。地幔物质的存在暗示了同时期来自地幔的物质不仅参与右江褶皱带晚白垩世岩浆作用的形成,可能为的地壳部分熔融,花岗岩岩浆的形成提供了热能。西大明山地区酸性岩浆具有高δ~(18)O_(Zrn)值和低ε_(Hf)(t)值且低Ce(Ⅳ)/Ce(Ⅲ)比值(即低氧逸度),显示出有利于形成大型以Pb-Zn为主的矽卡岩型矿床特征。本文研究结果表明,锆石O-Hf同位素综合研究能限定幔源岩浆参与花岗岩形成中的作用能帮助更加准确的限定岩浆源区。同时锆石氧同位素可以作为成矿规律研究的有效途径之一。
The source and petrogenesis of the Late Cretaceous magmatism and associated Sn-W mineralization in the South China are yet well documented. This paper reports the oxygen isotope compositions of previously analyzed zircons from the Yanshanian felsic intrusions in the Xidamingshan cluster,along the southeastern margin of the Youjiang fold belt,Guangxi,South China. Zircon( Zrn)δ~(18) O for quartz porphyry ranges from 5. 31‰ to 9. 31‰,VSMOW,averaging at 7. 61 ± 2. 17‰. δ~(18) O_(Zrn)for beresitization biotite granite,fine biotite granite and medium biotite granite range from 7. 11‰ to 9. 79‰( average = 8. 36 ± 1. 33‰),from 5. 06‰ to9. 27‰( average = 7. 73 ± 2. 23‰) and from 6. 27‰ to 9. 77‰( average = 8. 04 ± 1. 75‰),respectively. Monzonitic granite records a wide range in δ~(18) O_(Zrn)(5. 48‰ ~ 10. 99‰) with average of 7. 55 ± 2. 77‰. The majorities are greater than the"mantle-like"values(δ~(18) O: 5. 3 ± 0. 6‰,2σ). Except beresitization biotite granite,five samples have bimodal or multi-modal distribution characteristics and Hf-O plots of zircons have a negative correlation,indicating a crust-mantle interaction. Hf-O isotopic compositions suggest that the source of the magma was mainly derived from partial melting of crustal material with input of mantle-derived components. The mantlederived melts imply that these melts not only provided necessary heat energy for crust partial melting,but also put got involved in the generation of granitic melts. Low oxygen fugacity as indicated by low Ce( Ⅳ)/Ce( Ⅲ) ratios may be responsible for formation of large Pb-Zn-dominated skarn deposits. Our current research illustrates that combination of zircon Hf-O isotope could more accurately trace the source of magma through distinguish juvenile components and parental magmas derived from reworking of pre-existing crustal material. And zircon O isotope is one of the most efficient techniques to study the metallogenetic regularity.
The source and petrogenesis of the Late Cretaceous magmatism and associated Sn-W mineralization in the South China are yet well documented. This paper reports the oxygen isotope compositions of previously analyzed zircons from the Yanshanian felsic intrusions in the Xidamingshan cluster,along the southeastern margin of the Youjiang fold belt,Guangxi,South China. Zircon( Zrn)δ~(18) O for quartz porphyry ranges from 5. 31‰ to 9. 31‰,VSMOW,averaging at 7. 61 ± 2. 17‰. δ~(18) O_(Zrn)for beresitization biotite granite,fine biotite granite and medium biotite granite range from 7. 11‰ to 9. 79‰( average = 8. 36 ± 1. 33‰),from 5. 06‰ to9. 27‰( average = 7. 73 ± 2. 23‰) and from 6. 27‰ to 9. 77‰( average = 8. 04 ± 1. 75‰),respectively. Monzonitic granite records a wide range in δ~(18) O_(Zrn)(5. 48‰ ~ 10. 99‰) with average of 7. 55 ± 2. 77‰. The majorities are greater than the"mantle-like"values(δ~(18) O: 5. 3 ± 0. 6‰,2σ). Except beresitization biotite granite,five samples have bimodal or multi-modal distribution characteristics and Hf-O plots of zircons have a negative correlation,indicating a crust-mantle interaction. Hf-O isotopic compositions suggest that the source of the magma was mainly derived from partial melting of crustal material with input of mantle-derived components. The mantlederived melts imply that these melts not only provided necessary heat energy for crust partial melting,but also put got involved in the generation of granitic melts. Low oxygen fugacity as indicated by low Ce( Ⅳ)/Ce( Ⅲ) ratios may be responsible for formation of large Pb-Zn-dominated skarn deposits. Our current research illustrates that combination of zircon Hf-O isotope could more accurately trace the source of magma through distinguish juvenile components and parental magmas derived from reworking of pre-existing crustal material. And zircon O isotope is one of the most efficient techniques to study the metallogenetic regularity.
引文
Ballard JR,Palin MJ and Campbell IH.2002.Relative oxidation states of magmas inferred from Ce(Ⅳ)/Ce(Ⅲ)in zircon:Application to porphyry copper deposits of northern Chile.Contributions to Mineralogy and Petrology,144(3):347-364
Belousova EA,Griffin WL and O'Reilly SY.2006.Zircon crystal morphology,trace element signatures and Hf isotope composition as a tool for petrogenetic modelling:Examples from eastern Australian granitoids.Journal of Petrology,47(2):329-353
Bindeman IN and Valley JW.2000.Formation of low-δ18O rhyolites after caldera collapse at Yellowstone,Wyoming,USA.Geology,28(8):719-722
Bindeman IN and Valley JW.2001.Low-δ18O rhyolites from Yellowstone:Magmatic evolution based on analyses of zircons and individual phenocrysts.Journal of Petrology,42(8):1491-1517
Bindeman IN,Ponomareva VV,Bailey JC and Valley JW.2004.Volcanic arc of Kamchatka:A province with high-δ18O magma sources and large-scale18O/16O depletion of the upper crust.Geochimica et Cosmochimica Acta,68(4):841-865
Bindeman IN.2008.Oxygen isotopes in mantle and crustal magmas as revealed by single crystal analysis.Reviews in Mineralogy and Geochemistry,69(1):445-478
Bindeman IN,Gurenko A,Carley T,Miller C,Martin E and Sigmarsson O.2012.Silicic magma petrogenesis in Iceland by remelting of hydrothermally altered crust based on oxygen isotope diversity and disequilibria between zircon and magma with implications for MORB.Terra Nova,24(3):227-232
Black LP,Kamo SL,Allen CM,Davis DW,Aleinikoff JN,Valley JW,Mundil R,Campbell IH,Korsch RJ,Williams IS and Foudoulis C.2004.Improved206Pb/238U microprobe geochronology by the monitoring of a trace-element-related matrix effect:SHRIMP,ID-TIMS,ELA-ICP-MS and oxygen isotope documentation for a series of zircon standards.Chemical Geology,205(1-2):115-140
Booth AL,Kolodny Y,Chamberlain CP,Mc Williams M,Schmitt AK and Wooden J.2005.Oxygen isotopic composition and U-Pb discordance in zircon.Geochimica et Cosmochimica Acta,69(20):4895-4905
Bureau of Geology and Mineral Resources of Guangxi Zhuang Autonomous Region.1985.Regional Geology of the Guangxi Zhuang Autonomous Region.Beijing:Geological Publishing House,1-853(in Chinese)
Cai JX and Zhang KJ.2009.A new model for the Indochina and South China collision during the Late Permian to the Middle Triassic.Tectonophysics,467(1-4):35-43
Cai MH,He LQ,Liu GQ,Wu DC and Huang HM.2006.SHRIMPzircon U-Pb dating of the intrusive rocks in the Dachang tinpolymetallic ore field,Guangxi and their geological significance.Geological Review,52(3):409-414(in Chinese with English abstract)
Charoy B and Barbey P.2008.Ferromagnesian silicate association in S-type granites:The Darongshan granitic complex(Guangxi,South China).Bulletin de la SociétéGéologique de France,179(1):13-27
Chen CH,Hsieh PS,Lee CY and Zhou HW.2011.Two episodes of the Indosinian thermal event on the South China Block:Constraints from LA-ICPMS U-Pb zircon and electron microprobe monazite ages of the Darongshan S-type granitic suite.Gondwana Research,19(4):1008-1023
Chen MH,Lu G and Li XH.2012.Muscovite40Ar/39Ar dating of the quartz porphyry veins from Northwest Guangxi,China,and its geological significance.Geological Journal of China Universities,18(1):106-116(in Chinese with English abstract)
Chen XC,Hu RZ,Bi XW,Zhong H,Lan JB,Zhao CH and Zhu JJ.2015.Zircon U-Pb ages and Hf-O isotopes,and whole-rock Sr-Nd isotopes of the Bozhushan granite,Yunnan province,SW China:Constraints on petrogenesis and tectonic setting.Journal of Asian Earth Sciences,99:57-71
Chen ZC,Lin W,Faure M,Lepvier C,van Vuong N and van Tich V.2014.Geochronology and isotope analysis of the Late Paleozoic to Mesozoic granitoids from northeastern Vietnam and implications for the evolution of the South China block.Journal of Asian Earth Sciences,86:131-150
Cheng YB and Mao JW.2010.Age and geochemistry of granites in Gejiu area,Yunnan Province,SW China:Constraints on their petrogenesis and tectonic setting.Lithos,120(3-4):258-276
Cheng YB,Mao JW and Spandler C.2013.Petrogenesis and geodynamic implications of the Gejiu igneous complex in the western Cathaysia block,South China.Lithos,175-176:213-229
Cheng YB,Mao JW and Liu P.2016.Geodynamic setting of Late Cretaceous Sn-W mineralization in southeastern Yunnan and northeastern Vietnam.Solid Earth Sciences,1(3):79-88
Dang Y,Chen MH,Fu B,Mao JW,Fanning CM and Li ZY.2018.Petrogenesis of the Yupo W-bearing and Dali Mo-bearing granitoids in the Dayaoshan area,South China:Constraints of geochronology and geochemistry.Ore Geology Reviews,92:643-655
Davies JHFL,Stern RA,Heaman LM,Rojas X and Walton EL.2015.Resolving oxygen isotopic disturbance in zircon:A case study from the lowδ18O Scourie dikes,NW Scotland.American Mineralogist,100(8-9):1952-1966
Deng J,Wang QF,Yang SJ,Liu XF,Zhang QZ,Yang LQ and Yang YH.2010.Genetic relationship between the Emeishan plume and the bauxite deposits in western Guangxi,China:Constraints from U-Pb and Lu-Hf isotopes of the detrital zircons in bauxite ores.Journal of Asian Earth Sciences,37(5-6):412-424
Deng J,Wang QF,Li GJ and Santosh M.2014a.Cenozoic tectonomagmatic and metallogenic processes in the Sanjiang region,southwestern China.Earth-Science Reviews,138:168-299
Deng J,Wang QF,Li GJ,Li CS and Wang CM.2014b.Tethys tectonic evolution and its bearing on the distribution of important mineral deposits in the Sanjiang region,SW China.Gondwana Research,26(2):419-437
Deng J,Wang QF and Li GJ.2017.Tectonic evolution,superimposed orogeny,and composite metallogenic system in China.Gondwana Research,50:216-266
Fu B,Zheng YF,Wang ZR,Xiao YL,Gong B and Li SG.1999.Oxygen and hydrogen isotope geochemistry of gneisses associated with ultrahigh pressure eclogites at Shuanghe in the Dabie Mountains.Contributions to Mineralogy and Petrology,134(1):52-66
Fu B,Br9cker M,Ireland T,Holden P and Kinsley LPJ.2015.Zircon U-Pb,O,and Hf isotopic constraints on Mesozoic magmatism in the Cyclades,Aegean Sea,Greece.International Journal of Earth Sciences,104(1):75-87
Gao P,Zheng YF,Chen YX,Zhao ZF and Xia XP.2018.Relict zircon U-Pb age and O isotope evidence for reworking of Neoproterozoic crustal rocks in the origin of Triassic S-type granites in South China.Lithos,300-301:261-277
GouziniéS,Laurent O,Moyen JF,Zeh A,Bouilhol P and Villaros A.2016.Post-collisional magmatism:Crustal growth not identified by zircon Hf-O isotopes.Earth and Planetary Science Letters,456:182-195
Griffin WL,Pearson NJ,Belousova E,Jackson SE,van Achterbergh E,O’Reilly SY and Shee SR.2000.The Hf isotope composition of cratonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Grimes CB,Ushikubo T,Kozdon R and Valley JW.2013.Perspectives on the origin of plagiogranite in ophiolites from oxygen isotopes in zircon.Lithos,179:48-66
Hawkesworth CJ and Kemp AIS.2006.Using hafnium and oxygen isotopes in zircons to unravel the record of crustal evolution.Chemical Geology,226(3-4):144-162
Hua RM,Zhu JC,Zhao YJ,Zhou JP,Wu YY and Chen XD.1997.Preliminary study on metallogenetic series of nonferrous metal deposits in Youjiang fold belt.Geological Journal of China Universities,3(2):183-191(in Chinese with English abstract)
Hua RM,Chen PR,Zhang WL,Liu XD,Lu JJ,Lin JF,Yao JM,Qi HW,Zhang ZS and Gu MY.2003.Metallogenic systems related to Mesozoic and Cenozoic granitoids in South China.Science in China(Series D),46(8):816-829
Huang WL,Xu JF,Chen JL,Huang F,Zeng YC,Pi QH,Cai YF and Jiang XZ.2016.Geochronology and geochemistry of the Gejiu complex in the Yunnan Province,SW China:Petrogenesis and contributions of mantle-derived melts to tin mineralization.Acta Petrologica Sinica,32(8):2330-2346(in Chinese with English abstract)
Ickert RB,Hiess J,Williams IS,Holden P,Ireland TR,Lanc P,Schram N,Foster JJ and Clement SW.2008.Determining high precision,in situ,oxygen isotope ratios with a SHRIMPⅡ:Analyses of MPI-DING silicate-glass reference materials and zircon from contrasting granites.Chemical Geology,257(1-2):114-128
Kemp AIS,Hawkesworth CJ,Foster GL,Paterson BA,Woodhead JD,Hergt JM,Gray CM and Whitehouse MJ.2007.Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon.Science,315(5814):980-983
King EM,Valley JW,Davis DW and Edwards GR.1998.Oxygen isotope ratios of Archean plutonic zircons from granite-greenstone belts of the Superior Province:Indicator of magmatic source.Precambrian Research,92(4):365-387
Lackey JS,Valley JW and Saleeby JB.2005.Supracrustal input to magmas in the deep crust of Sierra Nevada batholith:Evidence from high-δ18O zircon.Earth and Planetary Science Letters,235(1-2):315-330
Lapierre H,Jahn BM,Charvet J and Yu YW.1997.Mesozoic felsic arc magmatism and continental olivine tholeiites in Zhejiang Province and their relationship with the tectonic activity in southeastern china.Tectonophysics,274(4):321-338
Li JW,Pei RF,Wang YL,She HQ,Feng CY,Guo ZJ,Wang HL and Xu K.2013.Isotopic chronological studies of Dulong tin-zinc deposit in Yunnan Province.Mineral Deposits,32(4):767-782(in Chinese with English abstract)
Li XH,Li WX,Wang XC,Li QL,Liu Y and Tang GQ.2009.Role of mantle-derived magma in genesis of early Yanshanian granites in the Nanling Range,South China:In situ zircon Hf-O isotopic constraints.Science in China(Series D),52(9):1262-1278
Liang T,Wang DH,Hou KJ,Li HQ,Huang HM,Cai MH and Wang DM.2011.LA-MC-ICP-MS zircon U-Pb dating of Longxianggai pluton in Dachang of Guangxi and its geological significance.Acta Petrologica Sinica,27(6):1624-1636(in Chinese with English abstract)
Liu XF,Wang QF,Zhang QZ,Yang SJ,Zhang Y,Liang YY and Qing C.2017.Transformation from Permian to Quaternary bauxite in southwestern South China Block driven by superimposed orogeny:Acase study from Sanhe ore deposit.Ore Geology Reviews,90:998-1017
Liu YB,Mo XX,Zhang D,Que CY,Di YJ,Pu XM,Cheng GS and Ma HH.2014.Petrogenesis of the Late Cretaceous granite discovered in the Laojunshan region,southeastern Yunnan Province.Acta Petrologica Sinica,30(11):3271-3286(in Chinese with English abstract)
Lu JH.2015.Geological characteristics,metallogenic regularity and metallogenic model of Xidamingshan Ag-Pb-Zn-Au-W-Bi deposit.Mineral Resources and Geology,29(5):560-567(in Chinese with English abstract)
Mao JW,Xie GQ,Li XF,Zhang CQ and Mei YX.2004.Mesozoic large scale mineralization and multiple lithospheric extension in South China.Earth Science Frontiers,11(1):45-55(in Chinese with English abstract)
Mao JW,Chen MH,Yuan SD and Guo CL.2011.Geological characteristics of the Qinhang(or Shihang)metallogenic belt in South China and spatial-temporal distribution regularity of mineral deposits.Acta Geologica Sinica,85(5):636-658(in Chinese with English abstract)
Monani S and Valley JW.2001.Oxygen isotope ratios of zircon:Magma genesis of lowδ18O granites from the British Tertiary igneous province,western Scotland.Earth and Planetary Science Letters,184(2):377-392
Page FZ,Ushikubo T,Kita NY,Riciputi LR and Valley JW.2007.High-precision oxygen isotope analysis of picogram samples reveals2μm gradients and slow diffusion in zircon.American Mineralogist,92(10):1772-1775
Peck WH,Valley JW,Wilde SA and Graham CM.2001.Oxygen Isotope ratios and rare earth elements in 3.3 to 4.4 Ga zircons:Ion microprobe evidence for highδ18O continental crust and oceans in the Early Archean.Geochimica et Cosmochimica Acta,65(22):4215-4229
Qiao L.2016.Tectonic evolution and bauxite metallogenesis in the Youjiang basin and adjacent area.Ph.D.Dissertation.Beijing:China University of Geosciences(Beijing),1-165(in Chinese with English summary)
Romer RL and Kroner U.2016.Phanerozoic tin and tungsten mineralization-tectonic controls on the distribution of enriched protoliths and heat sources for crustal melting.Gondwana Research,31:60-95
Rumble D and Yui TF.1998.The Qinglongshan oxygen and hydrogen isotope anomaly near Donghai in Jiangsu Province,China.Geochimica et Cosmochimica Acta,62(19-20):3307-3321
Scherer EE,Camerson KL and Blichert-Toft J.2000.Lu-Hf garnet geochronology:Closure temperature relative to the Sm-Nd system and the effects of trace mineral inclusions.Geochimica et Cosmochimica Acta,64(19):3413-3432
Tan J,Wei JH,Li SR,Wang ZM,Fu LB and Zhang KQ.2008.Geochemical characteristics and tectonic significance of Kunlunguan A-type granite,Guangxi.Earth Science(Journal of China University of Geosciences),33(6):743-754(in Chinese with English abstract)
Taylor Jr HP.1968.The oxygen isotope geochemistry of igneous rocks.Contributions to Mineralogy and Petrology,19(1):1-71
Valley JW,Chiarenzelli JR and Mc Lelland JM.1994.Oxygen isotope geochemistry of zircon.Earth and Planetary Science Letters,126(4):187-206
Valley JW,Kinny PD,Schulze DJ and Spicuzza MJ.1998.Zircon megacrysts from kimberlite:Oxygen Isotope variability among mantle melts.Contributions to Mineralogy and Petrology,133(1-2):1-11
Valley JW.2003.Oxygen isotopes in zircon.Reviews in Mineralogy and Geochemistry,53(1):343-385
Valley JW,Lackey JS,Cavosie AJ,Clechenko CC,Spicuzza MJ,Basei MAS,Bindeman IN,Ferreira VP,Sial AN,King EM,Peck WH,Sinha AK and Wei CS.2005.4.4 billion years of crustal maturation:Oxygen isotope ratios of magmatic zircon.Contributions to Mineralogy and Petrology,150(6):561-580
Wang DS,Liu JL,Tran M,Ngyuen Q,Guo Q,Wu WB,Zhang ZC and Zhao ZD.2011.Geochronology,geochemistry and tectonic significance of granites in the T nh Túc W-Sn ore deposits,Northeast Vietnam.Acta Petrologica Sinica,27(9):2795-2808(in Chinese with English abstract)
Wang QF,Deng J,Liu XF,Zhang QZ,Sun SL,Jiang CZ and Zhou F.2010.Discovery of the REE minerals and its geological significance in the Quyang bauxite deposit,West Guangxi,China.Journal of Asian Earth Sciences,39(6):701-712
Wang QF,Deng J,Li CS,Li GJ,Yu L and Qiao L.2014.The boundary between the Simao and Yangtze blocks and their locations in Gondwana and Rodinia:Constraints from detrital and inherited zircons.Gondwana Research,26(2):438-448
Watson EB and Cherniak DJ.1997.Oxygen diffusion in zircon.Earth and Planetary Science Letters,148(3-4):527-544
Wei CS,Zhao ZF and Spicuzza MJ.2008.Zircon oxygen isotopic constraint on the sources of Late Mesozoic A-type granites in eastern China.Chemical Geology,250(1-4):1-15
Xiao CH,Shen YK,Wei CS,Su XK,Le XW and Zhang L.2018.LA-ICP-MS zircon U-Pb dating,Hf isotopic composition and Ce4+/Ce3+characteristics of the Yanshanian acid magma in the Xidamingshan cluster,southeastern margin of the Youjiang fold belt,Guangxi.Geoscience,32(2):289-304(in Chinese)
Xu B,Jiang SY,Wang R,Ma L,Zhao KD and Yan X.2015.Late Cretaceous granites from the giant Dulong Sn-polymetallic ore district in Yunnan Province,South China:Geochronology,geochemistry,mineral chemistry and Nd-Hf isotopic compositions.Lithos,218-219:54-72
Yan DP,Zhou MF,Wang CY and Xia B.2006.Structural and geochronological constraints on the tectonic evolution of the DulongSong Chay tectonic dome in Yunnan Province,SW China.Journal of Asian Earth Sciences,28(4-6):332-353
Zhang Y,Yang JH,Chen JY,Wang H and Xiang YX.2017.Petrogenesis of Jurassic tungsten-bearing granites in the Nanling Range,South China:Evidence from whole-rock geochemistry and zircon U-Pb and Hf-O isotopes.Lithos,278-281:166-180
Zhao PL,Yuan SD,Mao JW,Santosh M and Zhang DL.2017.Zircon U-Pb and Hf-O isotopes trace the architecture of polymetallic deposits:A case study of the Jurassic ore-forming porphyries in the Qin-Hang metallogenic belt,China.Lithos,292-293:132-145
Zhao XL,Liu K,Mao JR,Ye HM and Yu SY.2013.The differences of geochemical characteristics and relative with ore-forming processes of two types Early-Cretaceous granites in southwestern Fujian Province.Bulletin of Mineralogy,Petrology and Geochemistry,32(1):87-96(in Chinese with English abstract)
Zheng YF and Fu B.1998.Estimation of oxygen diffusivity from anion porosity in minerals.Geochemical Journal,32(2):71-89
Zheng YF,Fu B,Xiao YL,Li YL and Gong B.1999.Hydrogen and oxygen isotope evidence for fluid-rock interactions in the stages of pre-and post-UHP metamorphism in the Dabie Mountains.Lithos,46(4):677-693
Zheng YF,Fu B,Gong B and Li L.2003.Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China:Implications for geodynamics and fluid regime.Earth-Science Reviews,62(1-2):105-161
蔡明海,何龙清,刘国庆,吴德成,黄惠明.2006.广西大厂锡矿田侵入岩SHRIMP锆石U-Pb年龄及其意义.地质论评,52(3):409-414
陈懋弘,陆刚,李新华.2012.桂西北地区石英斑岩脉白云母40Ar/39Ar年龄及其地质意义.高校地质学报,18(1):106-116
广西壮族自治区地质矿产局.1985.广西壮族自治区区域地质志.北京:地质出版社,1-853
华仁民,朱金初,赵一英,周建平,吴燕玉,陈晓东.1997.右江褶皱带有色金属矿床成矿系列初步研究.高校地质学报,3(2):183-191
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.中国科学(D辑),33(4):335-343
黄文龙,许继峰,陈建林,黄丰,曾云川,皮桥辉,蔡永丰,蒋兴洲.2016.云南个旧杂岩体年代学与地球化学:岩石成因和幔源岩浆对锡成矿贡献.岩石学报,32(8):2330-2346
李进文,裴荣富,王永磊,佘宏全,丰成友,郭志军,王浩琳,徐可.2013.云南都龙锡锌矿区同位素年代学研究.矿床地质,32(4):767-782
梁婷,王登红,侯可军,李华芹,黄惠明,蔡明海,王东明.2011.广西大厂笼箱盖复式岩体的LA-MC-ICP-MS锆石U-Pb年龄及其地质意义.岩石学报,27(6):1624-1636
刘艳宾,莫宣学,张达,阙朝阳,狄永军,蒲兴明,程国顺,马慧慧.2014.滇东南老君山地区晚白垩世花岗岩的成因.岩石学报,30(11):3271-3286
陆建辉.2015.西大明山银铅锌金钨铋矿地质特征、成矿规律及成矿模式.矿产与地质,29(5):560-567
毛景文,谢桂青,李晓峰,张长青,梅燕雄.2004.华南地区中生代大规模成矿作用与岩石圈多阶段伸展.地学前缘,11(1):45-55
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.地质学报,85(5):636-658
乔龙.2016.右江盆地及其周缘地区构造演化及铝土矿成矿作用.博士学位论文.北京:中国地质大学(北京),1-165
谭俊,魏俊浩,李水如,王忠铭,付乐兵,张可清.2008.广西昆仑关A型花岗岩地球化学特征及构造意义.地球科学-中国地质大学学报,33(6):743-754
王东升,刘俊来,Tran M,Ngyuen Q,郭强,吴文彬,张招崇,赵志丹.2011.越南东北部静足(T nh Túc)钨锡矿区花岗岩年代学、地球化学与区域构造意义.岩石学报,27(9):2795-2808
肖昌浩,申玉科,韦昌山,苏晓凯,乐兴文,张亮.2018.广西右江褶皱带东南缘西大明山矿集区燕山期酸性岩浆锆石U-Pb年龄、Hf同位素和Ce(Ⅳ)/Ce(Ⅲ)特征.现代地质,32(2):289-304
赵希林,刘凯,毛建仁,叶海敏,于胜尧.2013.闽西南地区早白垩世两类花岗质岩体地球化学异同及其与成矿作用关系.矿物岩石地球化学通报,32(1):87-96
Belousova EA,Griffin WL and O'Reilly SY.2006.Zircon crystal morphology,trace element signatures and Hf isotope composition as a tool for petrogenetic modelling:Examples from eastern Australian granitoids.Journal of Petrology,47(2):329-353
Bindeman IN and Valley JW.2000.Formation of low-δ18O rhyolites after caldera collapse at Yellowstone,Wyoming,USA.Geology,28(8):719-722
Bindeman IN and Valley JW.2001.Low-δ18O rhyolites from Yellowstone:Magmatic evolution based on analyses of zircons and individual phenocrysts.Journal of Petrology,42(8):1491-1517
Bindeman IN,Ponomareva VV,Bailey JC and Valley JW.2004.Volcanic arc of Kamchatka:A province with high-δ18O magma sources and large-scale18O/16O depletion of the upper crust.Geochimica et Cosmochimica Acta,68(4):841-865
Bindeman IN.2008.Oxygen isotopes in mantle and crustal magmas as revealed by single crystal analysis.Reviews in Mineralogy and Geochemistry,69(1):445-478
Bindeman IN,Gurenko A,Carley T,Miller C,Martin E and Sigmarsson O.2012.Silicic magma petrogenesis in Iceland by remelting of hydrothermally altered crust based on oxygen isotope diversity and disequilibria between zircon and magma with implications for MORB.Terra Nova,24(3):227-232
Black LP,Kamo SL,Allen CM,Davis DW,Aleinikoff JN,Valley JW,Mundil R,Campbell IH,Korsch RJ,Williams IS and Foudoulis C.2004.Improved206Pb/238U microprobe geochronology by the monitoring of a trace-element-related matrix effect:SHRIMP,ID-TIMS,ELA-ICP-MS and oxygen isotope documentation for a series of zircon standards.Chemical Geology,205(1-2):115-140
Booth AL,Kolodny Y,Chamberlain CP,Mc Williams M,Schmitt AK and Wooden J.2005.Oxygen isotopic composition and U-Pb discordance in zircon.Geochimica et Cosmochimica Acta,69(20):4895-4905
Bureau of Geology and Mineral Resources of Guangxi Zhuang Autonomous Region.1985.Regional Geology of the Guangxi Zhuang Autonomous Region.Beijing:Geological Publishing House,1-853(in Chinese)
Cai JX and Zhang KJ.2009.A new model for the Indochina and South China collision during the Late Permian to the Middle Triassic.Tectonophysics,467(1-4):35-43
Cai MH,He LQ,Liu GQ,Wu DC and Huang HM.2006.SHRIMPzircon U-Pb dating of the intrusive rocks in the Dachang tinpolymetallic ore field,Guangxi and their geological significance.Geological Review,52(3):409-414(in Chinese with English abstract)
Charoy B and Barbey P.2008.Ferromagnesian silicate association in S-type granites:The Darongshan granitic complex(Guangxi,South China).Bulletin de la SociétéGéologique de France,179(1):13-27
Chen CH,Hsieh PS,Lee CY and Zhou HW.2011.Two episodes of the Indosinian thermal event on the South China Block:Constraints from LA-ICPMS U-Pb zircon and electron microprobe monazite ages of the Darongshan S-type granitic suite.Gondwana Research,19(4):1008-1023
Chen MH,Lu G and Li XH.2012.Muscovite40Ar/39Ar dating of the quartz porphyry veins from Northwest Guangxi,China,and its geological significance.Geological Journal of China Universities,18(1):106-116(in Chinese with English abstract)
Chen XC,Hu RZ,Bi XW,Zhong H,Lan JB,Zhao CH and Zhu JJ.2015.Zircon U-Pb ages and Hf-O isotopes,and whole-rock Sr-Nd isotopes of the Bozhushan granite,Yunnan province,SW China:Constraints on petrogenesis and tectonic setting.Journal of Asian Earth Sciences,99:57-71
Chen ZC,Lin W,Faure M,Lepvier C,van Vuong N and van Tich V.2014.Geochronology and isotope analysis of the Late Paleozoic to Mesozoic granitoids from northeastern Vietnam and implications for the evolution of the South China block.Journal of Asian Earth Sciences,86:131-150
Cheng YB and Mao JW.2010.Age and geochemistry of granites in Gejiu area,Yunnan Province,SW China:Constraints on their petrogenesis and tectonic setting.Lithos,120(3-4):258-276
Cheng YB,Mao JW and Spandler C.2013.Petrogenesis and geodynamic implications of the Gejiu igneous complex in the western Cathaysia block,South China.Lithos,175-176:213-229
Cheng YB,Mao JW and Liu P.2016.Geodynamic setting of Late Cretaceous Sn-W mineralization in southeastern Yunnan and northeastern Vietnam.Solid Earth Sciences,1(3):79-88
Dang Y,Chen MH,Fu B,Mao JW,Fanning CM and Li ZY.2018.Petrogenesis of the Yupo W-bearing and Dali Mo-bearing granitoids in the Dayaoshan area,South China:Constraints of geochronology and geochemistry.Ore Geology Reviews,92:643-655
Davies JHFL,Stern RA,Heaman LM,Rojas X and Walton EL.2015.Resolving oxygen isotopic disturbance in zircon:A case study from the lowδ18O Scourie dikes,NW Scotland.American Mineralogist,100(8-9):1952-1966
Deng J,Wang QF,Yang SJ,Liu XF,Zhang QZ,Yang LQ and Yang YH.2010.Genetic relationship between the Emeishan plume and the bauxite deposits in western Guangxi,China:Constraints from U-Pb and Lu-Hf isotopes of the detrital zircons in bauxite ores.Journal of Asian Earth Sciences,37(5-6):412-424
Deng J,Wang QF,Li GJ and Santosh M.2014a.Cenozoic tectonomagmatic and metallogenic processes in the Sanjiang region,southwestern China.Earth-Science Reviews,138:168-299
Deng J,Wang QF,Li GJ,Li CS and Wang CM.2014b.Tethys tectonic evolution and its bearing on the distribution of important mineral deposits in the Sanjiang region,SW China.Gondwana Research,26(2):419-437
Deng J,Wang QF and Li GJ.2017.Tectonic evolution,superimposed orogeny,and composite metallogenic system in China.Gondwana Research,50:216-266
Fu B,Zheng YF,Wang ZR,Xiao YL,Gong B and Li SG.1999.Oxygen and hydrogen isotope geochemistry of gneisses associated with ultrahigh pressure eclogites at Shuanghe in the Dabie Mountains.Contributions to Mineralogy and Petrology,134(1):52-66
Fu B,Br9cker M,Ireland T,Holden P and Kinsley LPJ.2015.Zircon U-Pb,O,and Hf isotopic constraints on Mesozoic magmatism in the Cyclades,Aegean Sea,Greece.International Journal of Earth Sciences,104(1):75-87
Gao P,Zheng YF,Chen YX,Zhao ZF and Xia XP.2018.Relict zircon U-Pb age and O isotope evidence for reworking of Neoproterozoic crustal rocks in the origin of Triassic S-type granites in South China.Lithos,300-301:261-277
GouziniéS,Laurent O,Moyen JF,Zeh A,Bouilhol P and Villaros A.2016.Post-collisional magmatism:Crustal growth not identified by zircon Hf-O isotopes.Earth and Planetary Science Letters,456:182-195
Griffin WL,Pearson NJ,Belousova E,Jackson SE,van Achterbergh E,O’Reilly SY and Shee SR.2000.The Hf isotope composition of cratonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Grimes CB,Ushikubo T,Kozdon R and Valley JW.2013.Perspectives on the origin of plagiogranite in ophiolites from oxygen isotopes in zircon.Lithos,179:48-66
Hawkesworth CJ and Kemp AIS.2006.Using hafnium and oxygen isotopes in zircons to unravel the record of crustal evolution.Chemical Geology,226(3-4):144-162
Hua RM,Zhu JC,Zhao YJ,Zhou JP,Wu YY and Chen XD.1997.Preliminary study on metallogenetic series of nonferrous metal deposits in Youjiang fold belt.Geological Journal of China Universities,3(2):183-191(in Chinese with English abstract)
Hua RM,Chen PR,Zhang WL,Liu XD,Lu JJ,Lin JF,Yao JM,Qi HW,Zhang ZS and Gu MY.2003.Metallogenic systems related to Mesozoic and Cenozoic granitoids in South China.Science in China(Series D),46(8):816-829
Huang WL,Xu JF,Chen JL,Huang F,Zeng YC,Pi QH,Cai YF and Jiang XZ.2016.Geochronology and geochemistry of the Gejiu complex in the Yunnan Province,SW China:Petrogenesis and contributions of mantle-derived melts to tin mineralization.Acta Petrologica Sinica,32(8):2330-2346(in Chinese with English abstract)
Ickert RB,Hiess J,Williams IS,Holden P,Ireland TR,Lanc P,Schram N,Foster JJ and Clement SW.2008.Determining high precision,in situ,oxygen isotope ratios with a SHRIMPⅡ:Analyses of MPI-DING silicate-glass reference materials and zircon from contrasting granites.Chemical Geology,257(1-2):114-128
Kemp AIS,Hawkesworth CJ,Foster GL,Paterson BA,Woodhead JD,Hergt JM,Gray CM and Whitehouse MJ.2007.Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon.Science,315(5814):980-983
King EM,Valley JW,Davis DW and Edwards GR.1998.Oxygen isotope ratios of Archean plutonic zircons from granite-greenstone belts of the Superior Province:Indicator of magmatic source.Precambrian Research,92(4):365-387
Lackey JS,Valley JW and Saleeby JB.2005.Supracrustal input to magmas in the deep crust of Sierra Nevada batholith:Evidence from high-δ18O zircon.Earth and Planetary Science Letters,235(1-2):315-330
Lapierre H,Jahn BM,Charvet J and Yu YW.1997.Mesozoic felsic arc magmatism and continental olivine tholeiites in Zhejiang Province and their relationship with the tectonic activity in southeastern china.Tectonophysics,274(4):321-338
Li JW,Pei RF,Wang YL,She HQ,Feng CY,Guo ZJ,Wang HL and Xu K.2013.Isotopic chronological studies of Dulong tin-zinc deposit in Yunnan Province.Mineral Deposits,32(4):767-782(in Chinese with English abstract)
Li XH,Li WX,Wang XC,Li QL,Liu Y and Tang GQ.2009.Role of mantle-derived magma in genesis of early Yanshanian granites in the Nanling Range,South China:In situ zircon Hf-O isotopic constraints.Science in China(Series D),52(9):1262-1278
Liang T,Wang DH,Hou KJ,Li HQ,Huang HM,Cai MH and Wang DM.2011.LA-MC-ICP-MS zircon U-Pb dating of Longxianggai pluton in Dachang of Guangxi and its geological significance.Acta Petrologica Sinica,27(6):1624-1636(in Chinese with English abstract)
Liu XF,Wang QF,Zhang QZ,Yang SJ,Zhang Y,Liang YY and Qing C.2017.Transformation from Permian to Quaternary bauxite in southwestern South China Block driven by superimposed orogeny:Acase study from Sanhe ore deposit.Ore Geology Reviews,90:998-1017
Liu YB,Mo XX,Zhang D,Que CY,Di YJ,Pu XM,Cheng GS and Ma HH.2014.Petrogenesis of the Late Cretaceous granite discovered in the Laojunshan region,southeastern Yunnan Province.Acta Petrologica Sinica,30(11):3271-3286(in Chinese with English abstract)
Lu JH.2015.Geological characteristics,metallogenic regularity and metallogenic model of Xidamingshan Ag-Pb-Zn-Au-W-Bi deposit.Mineral Resources and Geology,29(5):560-567(in Chinese with English abstract)
Mao JW,Xie GQ,Li XF,Zhang CQ and Mei YX.2004.Mesozoic large scale mineralization and multiple lithospheric extension in South China.Earth Science Frontiers,11(1):45-55(in Chinese with English abstract)
Mao JW,Chen MH,Yuan SD and Guo CL.2011.Geological characteristics of the Qinhang(or Shihang)metallogenic belt in South China and spatial-temporal distribution regularity of mineral deposits.Acta Geologica Sinica,85(5):636-658(in Chinese with English abstract)
Monani S and Valley JW.2001.Oxygen isotope ratios of zircon:Magma genesis of lowδ18O granites from the British Tertiary igneous province,western Scotland.Earth and Planetary Science Letters,184(2):377-392
Page FZ,Ushikubo T,Kita NY,Riciputi LR and Valley JW.2007.High-precision oxygen isotope analysis of picogram samples reveals2μm gradients and slow diffusion in zircon.American Mineralogist,92(10):1772-1775
Peck WH,Valley JW,Wilde SA and Graham CM.2001.Oxygen Isotope ratios and rare earth elements in 3.3 to 4.4 Ga zircons:Ion microprobe evidence for highδ18O continental crust and oceans in the Early Archean.Geochimica et Cosmochimica Acta,65(22):4215-4229
Qiao L.2016.Tectonic evolution and bauxite metallogenesis in the Youjiang basin and adjacent area.Ph.D.Dissertation.Beijing:China University of Geosciences(Beijing),1-165(in Chinese with English summary)
Romer RL and Kroner U.2016.Phanerozoic tin and tungsten mineralization-tectonic controls on the distribution of enriched protoliths and heat sources for crustal melting.Gondwana Research,31:60-95
Rumble D and Yui TF.1998.The Qinglongshan oxygen and hydrogen isotope anomaly near Donghai in Jiangsu Province,China.Geochimica et Cosmochimica Acta,62(19-20):3307-3321
Scherer EE,Camerson KL and Blichert-Toft J.2000.Lu-Hf garnet geochronology:Closure temperature relative to the Sm-Nd system and the effects of trace mineral inclusions.Geochimica et Cosmochimica Acta,64(19):3413-3432
Tan J,Wei JH,Li SR,Wang ZM,Fu LB and Zhang KQ.2008.Geochemical characteristics and tectonic significance of Kunlunguan A-type granite,Guangxi.Earth Science(Journal of China University of Geosciences),33(6):743-754(in Chinese with English abstract)
Taylor Jr HP.1968.The oxygen isotope geochemistry of igneous rocks.Contributions to Mineralogy and Petrology,19(1):1-71
Valley JW,Chiarenzelli JR and Mc Lelland JM.1994.Oxygen isotope geochemistry of zircon.Earth and Planetary Science Letters,126(4):187-206
Valley JW,Kinny PD,Schulze DJ and Spicuzza MJ.1998.Zircon megacrysts from kimberlite:Oxygen Isotope variability among mantle melts.Contributions to Mineralogy and Petrology,133(1-2):1-11
Valley JW.2003.Oxygen isotopes in zircon.Reviews in Mineralogy and Geochemistry,53(1):343-385
Valley JW,Lackey JS,Cavosie AJ,Clechenko CC,Spicuzza MJ,Basei MAS,Bindeman IN,Ferreira VP,Sial AN,King EM,Peck WH,Sinha AK and Wei CS.2005.4.4 billion years of crustal maturation:Oxygen isotope ratios of magmatic zircon.Contributions to Mineralogy and Petrology,150(6):561-580
Wang DS,Liu JL,Tran M,Ngyuen Q,Guo Q,Wu WB,Zhang ZC and Zhao ZD.2011.Geochronology,geochemistry and tectonic significance of granites in the T nh Túc W-Sn ore deposits,Northeast Vietnam.Acta Petrologica Sinica,27(9):2795-2808(in Chinese with English abstract)
Wang QF,Deng J,Liu XF,Zhang QZ,Sun SL,Jiang CZ and Zhou F.2010.Discovery of the REE minerals and its geological significance in the Quyang bauxite deposit,West Guangxi,China.Journal of Asian Earth Sciences,39(6):701-712
Wang QF,Deng J,Li CS,Li GJ,Yu L and Qiao L.2014.The boundary between the Simao and Yangtze blocks and their locations in Gondwana and Rodinia:Constraints from detrital and inherited zircons.Gondwana Research,26(2):438-448
Watson EB and Cherniak DJ.1997.Oxygen diffusion in zircon.Earth and Planetary Science Letters,148(3-4):527-544
Wei CS,Zhao ZF and Spicuzza MJ.2008.Zircon oxygen isotopic constraint on the sources of Late Mesozoic A-type granites in eastern China.Chemical Geology,250(1-4):1-15
Xiao CH,Shen YK,Wei CS,Su XK,Le XW and Zhang L.2018.LA-ICP-MS zircon U-Pb dating,Hf isotopic composition and Ce4+/Ce3+characteristics of the Yanshanian acid magma in the Xidamingshan cluster,southeastern margin of the Youjiang fold belt,Guangxi.Geoscience,32(2):289-304(in Chinese)
Xu B,Jiang SY,Wang R,Ma L,Zhao KD and Yan X.2015.Late Cretaceous granites from the giant Dulong Sn-polymetallic ore district in Yunnan Province,South China:Geochronology,geochemistry,mineral chemistry and Nd-Hf isotopic compositions.Lithos,218-219:54-72
Yan DP,Zhou MF,Wang CY and Xia B.2006.Structural and geochronological constraints on the tectonic evolution of the DulongSong Chay tectonic dome in Yunnan Province,SW China.Journal of Asian Earth Sciences,28(4-6):332-353
Zhang Y,Yang JH,Chen JY,Wang H and Xiang YX.2017.Petrogenesis of Jurassic tungsten-bearing granites in the Nanling Range,South China:Evidence from whole-rock geochemistry and zircon U-Pb and Hf-O isotopes.Lithos,278-281:166-180
Zhao PL,Yuan SD,Mao JW,Santosh M and Zhang DL.2017.Zircon U-Pb and Hf-O isotopes trace the architecture of polymetallic deposits:A case study of the Jurassic ore-forming porphyries in the Qin-Hang metallogenic belt,China.Lithos,292-293:132-145
Zhao XL,Liu K,Mao JR,Ye HM and Yu SY.2013.The differences of geochemical characteristics and relative with ore-forming processes of two types Early-Cretaceous granites in southwestern Fujian Province.Bulletin of Mineralogy,Petrology and Geochemistry,32(1):87-96(in Chinese with English abstract)
Zheng YF and Fu B.1998.Estimation of oxygen diffusivity from anion porosity in minerals.Geochemical Journal,32(2):71-89
Zheng YF,Fu B,Xiao YL,Li YL and Gong B.1999.Hydrogen and oxygen isotope evidence for fluid-rock interactions in the stages of pre-and post-UHP metamorphism in the Dabie Mountains.Lithos,46(4):677-693
Zheng YF,Fu B,Gong B and Li L.2003.Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China:Implications for geodynamics and fluid regime.Earth-Science Reviews,62(1-2):105-161
蔡明海,何龙清,刘国庆,吴德成,黄惠明.2006.广西大厂锡矿田侵入岩SHRIMP锆石U-Pb年龄及其意义.地质论评,52(3):409-414
陈懋弘,陆刚,李新华.2012.桂西北地区石英斑岩脉白云母40Ar/39Ar年龄及其地质意义.高校地质学报,18(1):106-116
广西壮族自治区地质矿产局.1985.广西壮族自治区区域地质志.北京:地质出版社,1-853
华仁民,朱金初,赵一英,周建平,吴燕玉,陈晓东.1997.右江褶皱带有色金属矿床成矿系列初步研究.高校地质学报,3(2):183-191
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.中国科学(D辑),33(4):335-343
黄文龙,许继峰,陈建林,黄丰,曾云川,皮桥辉,蔡永丰,蒋兴洲.2016.云南个旧杂岩体年代学与地球化学:岩石成因和幔源岩浆对锡成矿贡献.岩石学报,32(8):2330-2346
李进文,裴荣富,王永磊,佘宏全,丰成友,郭志军,王浩琳,徐可.2013.云南都龙锡锌矿区同位素年代学研究.矿床地质,32(4):767-782
梁婷,王登红,侯可军,李华芹,黄惠明,蔡明海,王东明.2011.广西大厂笼箱盖复式岩体的LA-MC-ICP-MS锆石U-Pb年龄及其地质意义.岩石学报,27(6):1624-1636
刘艳宾,莫宣学,张达,阙朝阳,狄永军,蒲兴明,程国顺,马慧慧.2014.滇东南老君山地区晚白垩世花岗岩的成因.岩石学报,30(11):3271-3286
陆建辉.2015.西大明山银铅锌金钨铋矿地质特征、成矿规律及成矿模式.矿产与地质,29(5):560-567
毛景文,谢桂青,李晓峰,张长青,梅燕雄.2004.华南地区中生代大规模成矿作用与岩石圈多阶段伸展.地学前缘,11(1):45-55
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.地质学报,85(5):636-658
乔龙.2016.右江盆地及其周缘地区构造演化及铝土矿成矿作用.博士学位论文.北京:中国地质大学(北京),1-165
谭俊,魏俊浩,李水如,王忠铭,付乐兵,张可清.2008.广西昆仑关A型花岗岩地球化学特征及构造意义.地球科学-中国地质大学学报,33(6):743-754
王东升,刘俊来,Tran M,Ngyuen Q,郭强,吴文彬,张招崇,赵志丹.2011.越南东北部静足(T nh Túc)钨锡矿区花岗岩年代学、地球化学与区域构造意义.岩石学报,27(9):2795-2808
肖昌浩,申玉科,韦昌山,苏晓凯,乐兴文,张亮.2018.广西右江褶皱带东南缘西大明山矿集区燕山期酸性岩浆锆石U-Pb年龄、Hf同位素和Ce(Ⅳ)/Ce(Ⅲ)特征.现代地质,32(2):289-304
赵希林,刘凯,毛建仁,叶海敏,于胜尧.2013.闽西南地区早白垩世两类花岗质岩体地球化学异同及其与成矿作用关系.矿物岩石地球化学通报,32(1):87-96
© 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 |