大茶园铀矿床成矿物质来源:C-O和Sr-Nd同位素证据
|
摘要
赣杭铀成矿带是我国最大的火山岩型铀成矿带,大茶园(661)铀矿床是该成矿带东段最重要的火山岩型铀矿床,矿体赋存于晚中生代磨石山群九里坪组流纹岩中。为探讨该铀矿床成矿物质来源,对采自大茶园铀矿床中的脉石矿物开展了系统的C-O和Sr-Nd同位素研究。结果表明,成矿流体中矿化剂∑CO_2主要来源于地幔,部分来自于基底大理岩或沉积碳酸盐岩碳;成矿期后方解石碳同位素组成靠近基底大理岩或沉积碳酸盐岩组成,可能主要为壳源碳酸盐岩的贡献;成矿期流体中∑CO_2以HCO_3~-为主,CO_2去气作用为方解石沉淀形成的主要机制。成矿期不同阶段方解石与萤石的Sr、Nd同位素组成没有明显差别且变化较小,显示矿床中脉石矿物的同源性。通过与基底陈蔡群变质岩和盖层火山岩的Sr、Nd同位素组成对比发现,成矿期萤石与盖层火山岩具有类似的Sr同位素组成,表明大茶园铀矿床成矿物质以壳源为主,主要来自于赋矿火山岩,而Nd同位素进一步表明成矿物质可能来源于赋矿的流纹岩。岩石圈伸展控制着富CO_2热液的形成,富CO_2热液在上升过程中萃取壳源(尤其是富铀火山岩)中成矿物质,并在有利的成矿部位通过CO_2去气作用导致铀沉淀成矿。
Gan-Hang uranium metallogenic belt is the largest volcanic-type uranium metallogenic belt in China. The Dachayuan( No. 661) uranium deposit,one of the most important uranium deposits in the Dazhou uranium orefield,is located in the eastern part of Gan-Hang uranium metallogenic belt,with the orebodies existent in the Late Mesozoic rhyolite of Jiuliping Formation,Moshishan Group. In order to define the source of metallogenic matter at the Dachayuan uranium deposit,C,O,Sr and Nd isotopic compositions of hydrothermal minerals( including fluorite,calcite) associated with uranium mineralization were systematically analyzed in this paper. The results show that the mineralizer ∑CO2 in the ore-forming fluid was mainly derived from the mantle,and partly from the marble of Chencai Group or the sedimentary carbonate; the post-mineralization calcites have the similar carbon isotopic compositions with the marble of Chencai Group or the sedimentary carbonate,indicating the main contribution of crust-derived carbonate rock. A quantitative mode simulated for the formation of calcites shows that the mineralizer ∑CO_2 in metallogenic fluid mainly occurs in the form of HCO_3~-,and the degasification of CO_2 is the main precipitation mechanism of calcite. The Sr and Nd isotopic compositions of gangue minerals in different stages are similar and fall in a narrow range,indicating a uniform and homogenous origin of Sr and Nd isotopes. In comparison with that of metamorphite from Chencai Group and volcanic rocks from Moshishan Group,the compositions of Sr and Nd isotopes indicate that the metallogenic matter of the Dachayuan uranium deposit may be mainly derived from crust,and the Nd isotopic composition further shows that the ore material might come from the rhyolite of the Jiuliping Formation. The CO_2-rich fluid that formed by the lithospheric extension,can leach the ore-forming matters from crust-derived rocks( especially the uranium-rich volcanics) during the rising process,and finally uranium precipitated in the favorable position through the degasification of CO_2.
Gan-Hang uranium metallogenic belt is the largest volcanic-type uranium metallogenic belt in China. The Dachayuan( No. 661) uranium deposit,one of the most important uranium deposits in the Dazhou uranium orefield,is located in the eastern part of Gan-Hang uranium metallogenic belt,with the orebodies existent in the Late Mesozoic rhyolite of Jiuliping Formation,Moshishan Group. In order to define the source of metallogenic matter at the Dachayuan uranium deposit,C,O,Sr and Nd isotopic compositions of hydrothermal minerals( including fluorite,calcite) associated with uranium mineralization were systematically analyzed in this paper. The results show that the mineralizer ∑CO2 in the ore-forming fluid was mainly derived from the mantle,and partly from the marble of Chencai Group or the sedimentary carbonate; the post-mineralization calcites have the similar carbon isotopic compositions with the marble of Chencai Group or the sedimentary carbonate,indicating the main contribution of crust-derived carbonate rock. A quantitative mode simulated for the formation of calcites shows that the mineralizer ∑CO_2 in metallogenic fluid mainly occurs in the form of HCO_3~-,and the degasification of CO_2 is the main precipitation mechanism of calcite. The Sr and Nd isotopic compositions of gangue minerals in different stages are similar and fall in a narrow range,indicating a uniform and homogenous origin of Sr and Nd isotopes. In comparison with that of metamorphite from Chencai Group and volcanic rocks from Moshishan Group,the compositions of Sr and Nd isotopes indicate that the metallogenic matter of the Dachayuan uranium deposit may be mainly derived from crust,and the Nd isotopic composition further shows that the ore material might come from the rhyolite of the Jiuliping Formation. The CO_2-rich fluid that formed by the lithospheric extension,can leach the ore-forming matters from crust-derived rocks( especially the uranium-rich volcanics) during the rising process,and finally uranium precipitated in the favorable position through the degasification of CO_2.
引文
Brannon JC,Podosek FA,Viets JG,Leach DL,Goldhabe M and Rowan EL.1991.Strontium isotopic constraints on the origin of ore-forming fluids of the Viburnum Trend,Southeast Missouri.Geochimica et Cosmochimica Acta,55(5):1407-1419
Cai YQ,Zhang JD,Li ZY,Guo QY,Song JY,Fan HH,Liu WS,Qi FCand Zhang ML.2015.Outline of uranium resources characteristics and metallogenetic regularity in China.Acta Geologica Sinica,89(6):1051-1069(in Chinese with English abstract)
Chen JF,Zhou TX,Li XM et al.1992.Sr and Nd isotopic compositions of Mesozoic magmatic rocks from the southeastern China and its tectonic significance.In:Li JL(ed.).Studies of Structure and Evolution of the Continental and Oceanic Lithosphere of SE China.Beijing:China Science and Technology Press,119-130(in Chinese)
Chen ZB.1981．“Double mixing”genetic model of uranium deposits in volcanic rocks and relationship between China’s Mesozoic vein-type uranium deposits and Pacific plate tectonics metallogenesis of uranium.In:Proceedings of the 26thIGC.Beogard:Geoinstitute,65-97
Choi SG,Kim ST and Lee JG.2003.Stable isotope systematics of Ulsan Fe-W skarn deposit,Korea.Journal of Geochemical Exploration,78-79:601-606
Cuney M.1978.Geologic environment,mineralogy,and fluid inclusions of the Bois Noirs-Limouzat uranium vein,Forez,France.Economic Geology,73(8):1567-1610
Deer WA,Howie RA and Zussman J.1966.An Introduction to the Rockforming Minerals.New York:Longman Press,511-515
Deines P and Gold DP.1973.The isotopic composition of carbonatite and kimberlite carbonates and their bearing on the isotopic composition of deep-seated carbon.Geochimica et Cosmochimica Acta,37(7):1709-1733
Deng P,Shen WZ,Ling HF,Ye HM,Wang XC,Pu W and Tan ZZ.2003.Uranium mineralization related to mantle fluid:A case study of the Xianshi deposit in the Xiazhuang uranium orefield.Geochimica,32(6):520-528(in Chinese with English abstract)
Fan HH,Ling HF,Wang DZ,Shen WZ,Liu CS and Jiang YH.2001.Ore-forming material sources for Xiangshan uranium ore-field in Jiangxi Province:Evidence from Nd-Sr-Pb isotopes.Geological Journal of China Universities,7(2):139-145(in Chinese with English abstract)
Fang XH.2009.Principal geological characteristics of the volcanic-type uranium deposits in China.Uranium Geology,25(2):98-104(in Chinese with English abstract)
Faure G.1986.Principles of Isotope Geology.2ndEdition.New York,US:Wiley
Gao BE and Wang XW.1991.Mesurement of uranium content in melt inclusions using fission-track method and its significance.GeologyGeochemistry,(4):67-68(in Chinese)
Gao X and Meng JY.2017.The source of ore-forming fluids and materials in the Tongchanggou Mo-Cu deposit,northwestern Yunnan,China:Constrains from skarn mineralogy and stable isotopes.Acta Petrologica Sinica,33(7):2161-2174(in Chinese with English abstract)
Gu MG.2003.Geochemical study on volcanic rocks of the Moshishan Group in Yantou region of Southeast Zhejiang.Geology and Mineral Resources of South China,(4):24-30(in Chinese with English abstract)
Hu RZ,Li CY,Ni SJ,Liu L and Yu JS.1993.Research on∑CO2source in ore-forming hydrothermal solution of granite-type uranium deposit,South China.Science in China(Series B),36(10):1252-1262
Hu RZ,Bi XW,Su WC,Peng JT and Li CY.2004.The relationship between uranium metallogenesis and crustal extension during the Cretaceous-Tertiary in South China.Earth Science Frontiers,11(1):153-160(in Chinese with English abstract)
Hu RZ,Bi XW,Zhou MF,Peng JT,Su WC,Liu S and Qi HW.2008.Uranium metallogenesis in South China and its relationship to crustal extension during the Cretaceous to Tertiary.Economic Geology,103(3):583-598
Hu RZ,Burnard PG,Bi XW,Zhou MF,Peng JT,Su WC and Zhao JH.2009.Mantle-derived gaseous components in ore-forming fluids of the Xiangshan uranium deposit,Jiangxi Province,China:Evidence from He,Ar and C isotopes.Chemical Geology,266(1-2):86-95
Hu RZ,Mao JW,Hua RM and Fan WM.2015.Intra-Continental Mineralization of South China Craton.Beijing:Science Press,1-903(in Chinese)
Hu RZ,Fu SL,Huang Y,Zhou MF,Fu SH,Zhao CH,Wang YJ,Bi XW and Xiao JF.2017.The giant South China Mesozoic lowtemperature metallogenic domain:Reviews and a new geodynamic model.Journal of Asian Earth Sciences,137:9-34
Hui XC,Han XZ,Lin JP,Wang MT,Zhang B,Tang JW,Du JH,Jin MZ and Lei YM.2012.Tectonic stress field’s characteristic and its relationship of uranium mineralization at Dazhou volcanic faulted basin in Quzhou,Zhejiang Province.Acta Geologica Sinica,86(2):228-240(in Chinese with English abstract)
Javoy M,Pineau F and Delorme H.1986.Carbon and nitrogen isotopes in the mantle.Chemical Geology,57(1-2):41-62
Jiang YH,Ling HF,Jiang SY,Shen WZ,Fan HH and Ni P.2006.Trace element and Sr-Nd isotope geochemistry of fluorite from the Xiangshan uranium deposit,Southeast China.Economic Geology,101(8):1613-1622
Jin JF and Hu RZ.1987.Transportation and deposition of uranium in hydrothermal ore-forming fluids as exemplified by uranium deposit No.302.Geochimica,(4):320-329(in Chinese with English abstract)
Keith ML and Weber JN.1964.Carbon and oxygen isotopic composition of selected limestones and fossils.Geochimica et Cosmochimica Acta,28(10-11):1787-1816
Kerrich R.1990.Carbon-isotope systematics of Archean Au-Ag vein deposits in the Superior Province.Canadian Journal of Earth Sciences,27(1):40-56
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
Leroy J.1978.The Margnac and Fanay uranium deposits of the La Crouzille District(western Massif Central,France):Geologic and fluid inclusion studies.Economic Geology,73(8):1611-1634
Li CJ and Jiang XL.1989.Strontium isotope geochemistry of fluorite deposits in Wuyi-Dongyang area,Zhejiang Province.Mineral Deposits,8(3):65-74(in Chinese with English abstract)
Liu HS.1986.The characteristics and distribution law of uranium mineralization of Mesozoic land facies volcanic rock-type in Zhejiang Province.Geology of Zhejiang,2(1):7-31(in Chinese with English abstract)
Liu JJ,He MQ,Li ZM,Liu YP,Li CY,Zhang Q,Yang WG and Yang AP.2004.Oxygen and carbon isotopic geochemistry of Baiyangping silver-copper polymetallic ore concentration area in Lanping Basin of Yunnan Province and its significance.Mineral Deposits,23(1):1-10(in Chinese with English abstract)
Liu RR,Li ZY,Tang JW and Xu XQ.2018.The source of uranium metallogenic fluid and its migration and enrichment mechanism in Quzhou area,Zhejiang.Journal of East China University of Technology,41(2):101-110(in Chinese with English abstract)
Mao MC.2004.Ore-forming feature and the prospect for volcanics-hosted uranium ore deposits in Zhejiang Province.Contributions to Geology and Mineral Resources Research,19(1):8-12,29(in Chinese with English abstract)
Ohmoto H.1972.Systematics of sulfur and carbon isotopes in hydrothermal ore deposits.Economic Geology,67(5):551-578
Peng JT,Hu RZ and Burnard PG.2003.Samarium-neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit(Hunan,China):The potential of calcite as a geochronometer.Chemical Geology,200(1-2):129-136
Qi HW and Hu RZ.2000.Comparison between uranium ore-forming fluids and magmatic fluids of granites,Southern China:Apreliminary study.Acta Mineralogica Sinica,20(4):401-405(in Chinese with English abstract)
Relvas JMRS,Barriga FJAS and Longstaffe FJ.2006.Hydrothermal alteration and mineralization in the Neves-Corvo volcanic-hosted massive sulfide deposit,Portugal．Ⅱ．Oxygen,hydrogen,and carbon isotopes.Economic Geology,101(4):791-804
Ruzicka V.1993.Vein uranium deposits.Ore Geology Reviews,8(3-4):247-276
Rye RO and Ohmoto H.1974.Sulfur and carbon isotopes and ore genesis:A review.Economic Geology,69(6):826-842
Shang PQ,Hu RZ,Bi XW,Liu L and Zhang GQ.2006.Study on carbon and oxygen isotopes in granite-type hydrothermal uranium deposits:A case of the Xiazhuang uranium ore field in northern Guangdong.Journal of Mineralogy and Petrology,26(3):71-76(in Chinese with English abstract)
Shang PQ,Hu RZ,Bi XW,Zhang GQ and Tian JJ.2012.Sr,Nd and Pb isotopic geochemistry of gangue minerals in the Xiazhuang uranium orefield,northern Guangdong Province.Geology in China,39(6):1847-1856(in Chinese with English abstract)
Shen WZ.1987.Stable Isotopic Geology.Beijing:Atomic Energy Press(in Chinese)
Shen WZ,Ling HF,Wang DZ,Xu BT and Yu YW.1999.Study on NdSr isotopes of Mesozoic igneous rocks in Zhejiang,China.Scientia Geolocia Sinica,34(2):223-232(in Chinese with English abstract)
Sheppard SMF and Dawson JB.1975.Hydrogen,carbon and oxygen isotope studies of megacryst and matrix minerals from Lesothan and South African kimberlites.In:Ahrens LH,Dawson JB,Duncan ARand Erlank AJ(eds.).Physics and Chemistry of the Earth.Oxford:Pergamon Press,747-763
Simonetti A and Bell K.1995.Nd,Pb,and Sr isotope systematics of fluorite at the Amba Dongar carbonatite complex,India:Evidence for hydrothermal and crustal fluid mixing.Economic Geology,90(7):2018-2027
Spangenberg J,FontbotéL,Sharp ZD and Hunziker J.1996.Carbon and oxygen isotope study of hydrothermal carbonates in the zinc-lead deposits of the San Vicente district,central Peru:A quantitative modeling on mixing processes and CO2degassing.Chemical Geology,133(1-4):289-315
Sun ZX.2004.Uranium sources of the Xiangshan uranium ore-field:Geochemical evidence.Acta Mineralogica Sinica,24(1):19-24(in Chinese with English abstract)
Taylor Jr HP,Frechen J and Degens ET.1967.Oxygen and carbon isotope studies of carbonatites from the Laacher See District,West Germany and the Aln9 District,Sweden.Geochimica et Cosmochimica Acta,31(3):407-430
Tian JJ,Hu RZ,Su WC,Zhang GQ and Shang PQ.2010a.Ore U-Pb isochron ages and metallogenic tectonic setting of No.661 uranium deposit.Mineral Deposits,29(3):452-460(in Chinese with English abstract)
Tian JJ,Hu RZ,Su WC,Zhang GQ,Shang PQ and Qi YQ.2010b.Characteristics of fluid inclusions and discussion on the origin of oreforming fluid in the No.661 uranium deposit,Zhejiang Province.Bulletin of Mineralogy,Petrology and Geochemistry,29(1):17-23,30(in Chinese with English abstract)
Tian JJ,Hu RZ,Su WC,Zhang GQ,Shang PQ and Qi YQ.2010c.Lead isotope compositions and its significance for ore-forming material of No.661 uranium deposit,Zhejiang Province,China.Acta Mineralogica Sinica,30(3):304-310(in Chinese with English abstract)
Tu GC.1996.The discussion on some CO2problems.Earth Science Frontiers,3(3-4):53-62(in Chinese with English abstract)
Wang CW.1983.A model of the genesis of granite-type and volcanitetype uranium mineralization.Mineral Deposits,2(2):59-67(in Chinese with English abstract)
Wang DZ,Zhou JC,Qiu JS and Fan HH.2000.Characteristics and petrogenesis of Late Mesozoic granitic volcanic-intrusive complexes in southeastern China.Geological Journal of China Universities,6(4):487-498(in Chinese with English abstract)
Xing GF and Tao KY.1998.The impact of Sr content on Sr isotope of magmatic rocks during crust-mantle interaction:An application to prtrogenesis of Cretaceous bimodal rocks in the coastal region of southeastern China.Volcanology and Mineral Resources,19(1):24-33(in Chinese with English abstract)
Xing GF,Yang ZL,Xue HM,Shen JL,Zhao Y,Mao JR and Tao KY.1999.The study progress and orientation of Mesozoic volcanic rock belts in southeastern continent,China.Jiangsu Geology,23(4):221-224(in Chinese with English abstract)
Xu BT.1988.Studies of H,O,C and Sr isotopes in metamorphic rocks of the Chencai Group,Zhejiang Province.Geochimica,(2):174-182(in Chinese with English abstract)
Xu XS and Xie X.2005.Late Mesozoic-Cenozoic basaltic rocks and crust-mantle interaction,SE China.Geological Journal of China Universities,11(3):318-334(in Chinese with English abstract)
Xue HM,Tao KY and Shen JL.1996.Sr and Nd isotopic characteristics and magma genesis of Mesozoic volcanic rocks along the coastal region of southeastern China.Acta Geologica Sinica,70(1):35-47(in Chinese with English abstract)
Yang LS.1987.A discussion of the genesis of green alteration band at a uranic ore-field and its significance.Geology of Zhejiang,3(2):46-52(in Chinese with English abstract)
Yang SY,Jiang SY,Zhao KD and Jiang YH.2013.Petrogenesis and tectonic significance of Early Cretaceous high-Zr rhyolite in the Dazhou uranium district,Gan-Hang Belt,Southeast China.Journal of Asian Earth Sciences,74:303-315
Yu YW,Xu BT,Chen JF and Dong CW.2001.Nd isotopic systematics of the late Mesozoic volcanic rocks from southeastern Zhejiang Province,China:Implications for stratigraphic study.Geological Journal of China Universities,7(1):62-69(in Chinese with English abstract)
Yu YW,Jiang Y and Lu CZ.2008.Stratigraphic subdivision and neodymium isotope characteristics of the Cretaceous volcanic rocks in Zhejiang Province.Journal of Stratigraphy,32(1):69-78(in Chinese with English abstract)
Zhang BT,Wu JQ,Qiu ZL and Li Y.1990.On the relationship between hydrothermal alteration and uranium enrichment.Geological Review,36(3):238-244(in Chinese with English abstract)
Zhang BT,Qin SC,Ni QS and Wu JQ.1992.On genesis and ore-control of stratiform green tectonic altered rock on No.661 uranium deposit in western Zhejiang Province.Journal of Nanjing University(Natural Sciences Edition),28(3):439-451(in Chinese with English abstract)
Zhang BT and Zhang ZH.1993.The Evolution of Continental Crust and Uranium Metallization in Southeastern China.Beijing:Atomic Energy Press(in Chinese)
Zhang GQ,Hu RZ,Shang PQ,Tian JJ and Shuang Y.2008.Study on the C-O isotopic composition of calcites and metallogenic dynamics background in the No.302 uranium deposit.Acta Mineralogica Sinica,28(4):413-420(in Chinese with English abstract)
Zhang XP.1999.Formation and evolution of Mesozoic volcanic basins in Gan-Hang tectonic belt.Uranium Geology,15(1):18-23(in Chinese with English abstract)
Zhang ZH.1984.Uranium Geochemistry.Beijing:Atomic Energy Press(in Chinese)
Zhao ZF,Zheng YF,Gong B and Zhao YB.2000.Carbon content and isotope composition of granites from southeastern China.Acta Geologica Sinica,74(1):51-62(in Chinese with English abstract)
Zheng YF.1990.Carbon-oxygen isotopic covariation in hydrothermal calcite during degassing of CO2.A quantitative evaluation and application to the Kushikino gold mining area in Japan.Mineralium Deposita,25(4):246-250
Zheng YF and Hoefs J.1993.Carbon and oxygen isotopic covariations in hydrothermal calcites.Theoretical modeling on mixing processes and application to Pb-Zn deposits in the Harz Mountains,Germany.Mineralium Deposita,28(2):79-89
Zheng YF.2001.Theoretical modeling of stable isotope systems and its applications to geochemistry of hydrothermal ore deposits.Mineral Deposits,20(1):57-70,85(in Chinese with English abstract)
Zhou JX,Huang ZL,Zhou GF and Zeng QS.2012.C,O isotope and REE geochemistry of the hydrothermal calcites from the Tianqiao PbZn ore deposit in NW Guizhou Province,China.Geotectonica et Metallogenia,36(1):93-101(in Chinese with English abstract)
Zhou JX,Wang XC,Wilde SA,Luo K,Huang ZL,Wu T and Jin ZG.2018.New insights into the metallogeny of MVT Zn-Pb deposits:Acase study from the Nayongzhi in South China,using field data,fluid compositions,and in situ S-Pb isotopes.American Mineralogist,103(1):91-108
Zhou JZ.1989.Metallogenic geological conditions of the No.661 uranium deposit.Uranium Geology of East China,(1):6-17(in Chinese)
Zhou XM.2007.Petrogenisis of Late Mesozoic Granite and Dynamic Evolution of Lithosphere in Nanling Region.Beijing:Science Press(in Chinese)
蔡煜琦，张金带，李子颖，郭庆银，宋继叶，范洪海，刘武生，漆富成，张明林．2015．中国铀矿资源特征及成矿规律概要．地质学报，89(6):1051-1069
陈江峰，周泰禧，李学明等．1992．中国东南地区中生代岩浆岩的Sr、Nd同位素组成及其大地构造意义．见:李继亮主编．中国东南海陆岩石圈结构与演化研究．北京:中国科学技术出版社，119-130
邓平，沈渭洲，凌洪飞，叶海敏，王学成，濮巍，谭正中．2003．地幔流体与铀成矿作用:以下庄矿田仙石铀矿床为例．地球化学，32(6):520-528
范洪海，凌洪飞，王德滋，沈渭洲，刘昌实，姜耀辉．2001．江西相山铀矿田成矿物质来源的Nd、Sr、Pb同位素证据．高校地质学报，7(2):139-145
方锡珩．2009．中国火山岩型铀矿的主要地质特征．铀矿地质，25(2):98-104
高必娥，王兴无．1991．裂变径迹法测量熔融包裹体中的铀含量及其意义．地质地球化学，(4):67-68
高雪，孟健寅．2017．滇西北铜厂沟Mo-Cu矿床成矿流体和成矿物质来源:矽卡岩矿物学与稳定同位素证据．岩石学报，33(7):2161-2174
顾明光．2003．浙东南岩头地区磨石山群火山岩岩石地球化学研究．华南地质与矿产，(4):24-30
胡瑞忠，毕献武，苏文超，彭建堂，李朝阳．2004．华南白垩-第三纪地壳拉张与铀成矿的关系．地学前缘，11(1):153-160
胡瑞忠，毛景文，华仁民，范蔚茗．2015．华南陆块陆内成矿作用．北京:科学出版社，1-903
惠小朝，韩效忠，林建平，王明太，张斌，汤江伟，杜江浩，金淼张，雷遥明．2012．浙江衢州大洲火山断陷盆地构造应力场特征及其与铀成矿关系．地质学报，86(2):228-240
金景福，胡瑞忠．1987.302矿床成矿热液中铀的迁移和沉淀．地球化学，(4):320-329
李长江，蒋叙良．1989．浙江武义-东阳地区萤石矿床的锶同位素地球化学研究．矿床地质，8(3):65-74
刘惠三．1986．浙江中生代陆相火山岩型铀矿化特征及其分布规律．浙江地质，2(1):7-31
刘家军，何明勤，李志明，刘玉平，李朝阳，张乾，杨伟光，杨爱平．2004．云南白秧坪银铜多金属矿集区碳氧同位素组成及其意义．矿床地质，23(1):1-10
刘蓉蓉，李子颖，汤江伟，徐小奇．2018．浙江衢州地区铀成矿流体来源及其迁移富集机理．东华理工大学学报(自然科学版)，41(2):101-110
毛孟才．2004．浙江火山岩型铀成矿特征及找矿前景．地质找矿论丛，19(1):8-12,29
戚华文，胡瑞忠．2000．华南花岗岩岩浆期后热液与铀成矿热液的初步对比．矿物学报，20(4):401-405
商朋强，胡瑞忠，毕献武，刘雷，张国全．2006．花岗岩型热液铀矿床C,O同位素研究---以粤北下庄铀矿田为例．矿物岩石，26(3):71-76
商朋强，胡瑞忠，毕献武，张国全，田建吉．2012．粤北下庄铀矿田脉石矿物Sr、Nd、Pb同位素地球化学研究．中国地质，39(6):1847-1856
沈渭洲．1987．稳定同位素地质．北京:原子能出版社
沈渭洲，凌洪飞，王德滋，徐步台，俞云文．1999．浙江省中生代火成岩的Nd-Sr同位素研究．地质科学，34(2):223-232
孙占学．2004．相山铀矿田铀源的地球化学证据．矿物学报，24(1):19-24
田建吉，胡瑞忠，苏文超，张国全，商朋强．2010a.661铀矿床矿石U-Pb等时线年龄及其成矿构造背景．矿床地质，29(3):452-460
田建吉，胡瑞忠，苏文超，张国全，商朋强，齐有强．2010b.661铀矿床流体包裹体特征及成矿流体来源探讨．矿物岩石地球化学通报，29(1):17-23,30
田建吉，胡瑞忠，苏文超，张国全，商朋强，齐有强．2010c.661铀矿床铅同位素组成与成矿物质来源探讨．矿物学报，30(3):304-310
涂光炽．1996．关于CO2若干问题的讨论．地学前缘，3(3-4):53-62
王传文．1983．花岗岩型和火山岩型铀矿化的成因．矿床地质，2(2):59-67
王德滋，周金城，邱检生，范洪海．2000．中国东南部晚中生代花岗质火山-侵入杂岩特征与成因．高校地质学报，6(4):487-498
邢光福，陶奎元．1998．在壳幔作用过程中Sr含量对岩浆岩Sr同位素组成的影响---兼论东南沿海白垩纪双峰式火山岩成因．火山地质与矿产，19(1):24-33
邢光福，杨祝良，薛怀民，沈加林，赵宇，毛建仁，陶奎元．1999．中国东南大陆中生代火山岩带研究进展和方向．江苏地质，23(4):221-224
徐步台．1988．浙江陈蔡群变质岩系的氢、氧、碳及锶稳定同位素研究．地球化学，(2):174-182
徐夕生，谢昕．2005．中国东南部晚中生代-新生代玄武岩与壳幔作用．高校地质学报，11(3):318-334
薛怀民，陶奎元，沈加林．1996．中国东南沿海中生代酸性火山岩的锶和钕同位素特征与岩浆成因．地质学报，70(1):35-47
杨流顺．1987．某铀矿田“绿色层”的成因及其意义．浙江地质，3(2):46-52
俞云文，徐步台，陈江峰，董传万．2001．浙东南中生代晚期火山岩Nd同位素组成及其地层学意义．高校地质学报，7(1):62-69
俞云文，姜禹，卢成忠．2008．浙江白垩纪火山岩的地层划分及钕同位素特征．地层学杂志，32(1):69-78
章邦桐，吴俊奇，丘志力，刘义．1990．论热液蚀变与铀成矿富集作用的关系．地质论评，36(3):238-244
章邦桐，秦社彩，倪琦生，吴俊奇．1992．浙江661铀矿床“绿色层”成因及控矿作用的研究．南京大学学报，28(3):439-451
章邦桐，张祖还．1993．华南东部陆壳演化与铀成矿作用．北京:原子能出版社
张国全，胡瑞忠，商朋强，田建吉，双燕．2008.302铀矿床方解石C-O同位素组成与成矿动力学背景研究．矿物学报，28(4):413-420
张星蒲．1999．赣杭构造带中生代火山盆地的形成和演化．铀矿地质，15(1):18-23
张祖还．1984．铀地球化学．北京:原子能出版社
赵子福，郑永飞，龚冰，赵彦冰．2000．中国东南部花岗岩的碳含量和同位素比值．地质学报，74(1):51-62
郑永飞．2001．稳定同位素体系理论模式及其矿床地球化学应用．矿床地质，20(1):57-70,85
周家喜，黄智龙，周国富，曾乔松．2012．黔西北天桥铅锌矿床热液方解石C、O同位素和REE地球化学．大地构造与成矿学，36(1):93-101
周家志．1989.661铀矿床成矿地质条件．华东铀矿地质，(1):6-17
周新民．2007．南岭地区晚中生代花岗岩成因与岩石圈动力学演化．北京:科学出版社
(1)华东地勘局269大队．1984．六六零矿田六六一、六六三矿床实例报告．内部资料
Cai YQ,Zhang JD,Li ZY,Guo QY,Song JY,Fan HH,Liu WS,Qi FCand Zhang ML.2015.Outline of uranium resources characteristics and metallogenetic regularity in China.Acta Geologica Sinica,89(6):1051-1069(in Chinese with English abstract)
Chen JF,Zhou TX,Li XM et al.1992.Sr and Nd isotopic compositions of Mesozoic magmatic rocks from the southeastern China and its tectonic significance.In:Li JL(ed.).Studies of Structure and Evolution of the Continental and Oceanic Lithosphere of SE China.Beijing:China Science and Technology Press,119-130(in Chinese)
Chen ZB.1981．“Double mixing”genetic model of uranium deposits in volcanic rocks and relationship between China’s Mesozoic vein-type uranium deposits and Pacific plate tectonics metallogenesis of uranium.In:Proceedings of the 26thIGC.Beogard:Geoinstitute,65-97
Choi SG,Kim ST and Lee JG.2003.Stable isotope systematics of Ulsan Fe-W skarn deposit,Korea.Journal of Geochemical Exploration,78-79:601-606
Cuney M.1978.Geologic environment,mineralogy,and fluid inclusions of the Bois Noirs-Limouzat uranium vein,Forez,France.Economic Geology,73(8):1567-1610
Deer WA,Howie RA and Zussman J.1966.An Introduction to the Rockforming Minerals.New York:Longman Press,511-515
Deines P and Gold DP.1973.The isotopic composition of carbonatite and kimberlite carbonates and their bearing on the isotopic composition of deep-seated carbon.Geochimica et Cosmochimica Acta,37(7):1709-1733
Deng P,Shen WZ,Ling HF,Ye HM,Wang XC,Pu W and Tan ZZ.2003.Uranium mineralization related to mantle fluid:A case study of the Xianshi deposit in the Xiazhuang uranium orefield.Geochimica,32(6):520-528(in Chinese with English abstract)
Fan HH,Ling HF,Wang DZ,Shen WZ,Liu CS and Jiang YH.2001.Ore-forming material sources for Xiangshan uranium ore-field in Jiangxi Province:Evidence from Nd-Sr-Pb isotopes.Geological Journal of China Universities,7(2):139-145(in Chinese with English abstract)
Fang XH.2009.Principal geological characteristics of the volcanic-type uranium deposits in China.Uranium Geology,25(2):98-104(in Chinese with English abstract)
Faure G.1986.Principles of Isotope Geology.2ndEdition.New York,US:Wiley
Gao BE and Wang XW.1991.Mesurement of uranium content in melt inclusions using fission-track method and its significance.GeologyGeochemistry,(4):67-68(in Chinese)
Gao X and Meng JY.2017.The source of ore-forming fluids and materials in the Tongchanggou Mo-Cu deposit,northwestern Yunnan,China:Constrains from skarn mineralogy and stable isotopes.Acta Petrologica Sinica,33(7):2161-2174(in Chinese with English abstract)
Gu MG.2003.Geochemical study on volcanic rocks of the Moshishan Group in Yantou region of Southeast Zhejiang.Geology and Mineral Resources of South China,(4):24-30(in Chinese with English abstract)
Hu RZ,Li CY,Ni SJ,Liu L and Yu JS.1993.Research on∑CO2source in ore-forming hydrothermal solution of granite-type uranium deposit,South China.Science in China(Series B),36(10):1252-1262
Hu RZ,Bi XW,Su WC,Peng JT and Li CY.2004.The relationship between uranium metallogenesis and crustal extension during the Cretaceous-Tertiary in South China.Earth Science Frontiers,11(1):153-160(in Chinese with English abstract)
Hu RZ,Bi XW,Zhou MF,Peng JT,Su WC,Liu S and Qi HW.2008.Uranium metallogenesis in South China and its relationship to crustal extension during the Cretaceous to Tertiary.Economic Geology,103(3):583-598
Hu RZ,Burnard PG,Bi XW,Zhou MF,Peng JT,Su WC and Zhao JH.2009.Mantle-derived gaseous components in ore-forming fluids of the Xiangshan uranium deposit,Jiangxi Province,China:Evidence from He,Ar and C isotopes.Chemical Geology,266(1-2):86-95
Hu RZ,Mao JW,Hua RM and Fan WM.2015.Intra-Continental Mineralization of South China Craton.Beijing:Science Press,1-903(in Chinese)
Hu RZ,Fu SL,Huang Y,Zhou MF,Fu SH,Zhao CH,Wang YJ,Bi XW and Xiao JF.2017.The giant South China Mesozoic lowtemperature metallogenic domain:Reviews and a new geodynamic model.Journal of Asian Earth Sciences,137:9-34
Hui XC,Han XZ,Lin JP,Wang MT,Zhang B,Tang JW,Du JH,Jin MZ and Lei YM.2012.Tectonic stress field’s characteristic and its relationship of uranium mineralization at Dazhou volcanic faulted basin in Quzhou,Zhejiang Province.Acta Geologica Sinica,86(2):228-240(in Chinese with English abstract)
Javoy M,Pineau F and Delorme H.1986.Carbon and nitrogen isotopes in the mantle.Chemical Geology,57(1-2):41-62
Jiang YH,Ling HF,Jiang SY,Shen WZ,Fan HH and Ni P.2006.Trace element and Sr-Nd isotope geochemistry of fluorite from the Xiangshan uranium deposit,Southeast China.Economic Geology,101(8):1613-1622
Jin JF and Hu RZ.1987.Transportation and deposition of uranium in hydrothermal ore-forming fluids as exemplified by uranium deposit No.302.Geochimica,(4):320-329(in Chinese with English abstract)
Keith ML and Weber JN.1964.Carbon and oxygen isotopic composition of selected limestones and fossils.Geochimica et Cosmochimica Acta,28(10-11):1787-1816
Kerrich R.1990.Carbon-isotope systematics of Archean Au-Ag vein deposits in the Superior Province.Canadian Journal of Earth Sciences,27(1):40-56
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
Leroy J.1978.The Margnac and Fanay uranium deposits of the La Crouzille District(western Massif Central,France):Geologic and fluid inclusion studies.Economic Geology,73(8):1611-1634
Li CJ and Jiang XL.1989.Strontium isotope geochemistry of fluorite deposits in Wuyi-Dongyang area,Zhejiang Province.Mineral Deposits,8(3):65-74(in Chinese with English abstract)
Liu HS.1986.The characteristics and distribution law of uranium mineralization of Mesozoic land facies volcanic rock-type in Zhejiang Province.Geology of Zhejiang,2(1):7-31(in Chinese with English abstract)
Liu JJ,He MQ,Li ZM,Liu YP,Li CY,Zhang Q,Yang WG and Yang AP.2004.Oxygen and carbon isotopic geochemistry of Baiyangping silver-copper polymetallic ore concentration area in Lanping Basin of Yunnan Province and its significance.Mineral Deposits,23(1):1-10(in Chinese with English abstract)
Liu RR,Li ZY,Tang JW and Xu XQ.2018.The source of uranium metallogenic fluid and its migration and enrichment mechanism in Quzhou area,Zhejiang.Journal of East China University of Technology,41(2):101-110(in Chinese with English abstract)
Mao MC.2004.Ore-forming feature and the prospect for volcanics-hosted uranium ore deposits in Zhejiang Province.Contributions to Geology and Mineral Resources Research,19(1):8-12,29(in Chinese with English abstract)
Ohmoto H.1972.Systematics of sulfur and carbon isotopes in hydrothermal ore deposits.Economic Geology,67(5):551-578
Peng JT,Hu RZ and Burnard PG.2003.Samarium-neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit(Hunan,China):The potential of calcite as a geochronometer.Chemical Geology,200(1-2):129-136
Qi HW and Hu RZ.2000.Comparison between uranium ore-forming fluids and magmatic fluids of granites,Southern China:Apreliminary study.Acta Mineralogica Sinica,20(4):401-405(in Chinese with English abstract)
Relvas JMRS,Barriga FJAS and Longstaffe FJ.2006.Hydrothermal alteration and mineralization in the Neves-Corvo volcanic-hosted massive sulfide deposit,Portugal．Ⅱ．Oxygen,hydrogen,and carbon isotopes.Economic Geology,101(4):791-804
Ruzicka V.1993.Vein uranium deposits.Ore Geology Reviews,8(3-4):247-276
Rye RO and Ohmoto H.1974.Sulfur and carbon isotopes and ore genesis:A review.Economic Geology,69(6):826-842
Shang PQ,Hu RZ,Bi XW,Liu L and Zhang GQ.2006.Study on carbon and oxygen isotopes in granite-type hydrothermal uranium deposits:A case of the Xiazhuang uranium ore field in northern Guangdong.Journal of Mineralogy and Petrology,26(3):71-76(in Chinese with English abstract)
Shang PQ,Hu RZ,Bi XW,Zhang GQ and Tian JJ.2012.Sr,Nd and Pb isotopic geochemistry of gangue minerals in the Xiazhuang uranium orefield,northern Guangdong Province.Geology in China,39(6):1847-1856(in Chinese with English abstract)
Shen WZ.1987.Stable Isotopic Geology.Beijing:Atomic Energy Press(in Chinese)
Shen WZ,Ling HF,Wang DZ,Xu BT and Yu YW.1999.Study on NdSr isotopes of Mesozoic igneous rocks in Zhejiang,China.Scientia Geolocia Sinica,34(2):223-232(in Chinese with English abstract)
Sheppard SMF and Dawson JB.1975.Hydrogen,carbon and oxygen isotope studies of megacryst and matrix minerals from Lesothan and South African kimberlites.In:Ahrens LH,Dawson JB,Duncan ARand Erlank AJ(eds.).Physics and Chemistry of the Earth.Oxford:Pergamon Press,747-763
Simonetti A and Bell K.1995.Nd,Pb,and Sr isotope systematics of fluorite at the Amba Dongar carbonatite complex,India:Evidence for hydrothermal and crustal fluid mixing.Economic Geology,90(7):2018-2027
Spangenberg J,FontbotéL,Sharp ZD and Hunziker J.1996.Carbon and oxygen isotope study of hydrothermal carbonates in the zinc-lead deposits of the San Vicente district,central Peru:A quantitative modeling on mixing processes and CO2degassing.Chemical Geology,133(1-4):289-315
Sun ZX.2004.Uranium sources of the Xiangshan uranium ore-field:Geochemical evidence.Acta Mineralogica Sinica,24(1):19-24(in Chinese with English abstract)
Taylor Jr HP,Frechen J and Degens ET.1967.Oxygen and carbon isotope studies of carbonatites from the Laacher See District,West Germany and the Aln9 District,Sweden.Geochimica et Cosmochimica Acta,31(3):407-430
Tian JJ,Hu RZ,Su WC,Zhang GQ and Shang PQ.2010a.Ore U-Pb isochron ages and metallogenic tectonic setting of No.661 uranium deposit.Mineral Deposits,29(3):452-460(in Chinese with English abstract)
Tian JJ,Hu RZ,Su WC,Zhang GQ,Shang PQ and Qi YQ.2010b.Characteristics of fluid inclusions and discussion on the origin of oreforming fluid in the No.661 uranium deposit,Zhejiang Province.Bulletin of Mineralogy,Petrology and Geochemistry,29(1):17-23,30(in Chinese with English abstract)
Tian JJ,Hu RZ,Su WC,Zhang GQ,Shang PQ and Qi YQ.2010c.Lead isotope compositions and its significance for ore-forming material of No.661 uranium deposit,Zhejiang Province,China.Acta Mineralogica Sinica,30(3):304-310(in Chinese with English abstract)
Tu GC.1996.The discussion on some CO2problems.Earth Science Frontiers,3(3-4):53-62(in Chinese with English abstract)
Wang CW.1983.A model of the genesis of granite-type and volcanitetype uranium mineralization.Mineral Deposits,2(2):59-67(in Chinese with English abstract)
Wang DZ,Zhou JC,Qiu JS and Fan HH.2000.Characteristics and petrogenesis of Late Mesozoic granitic volcanic-intrusive complexes in southeastern China.Geological Journal of China Universities,6(4):487-498(in Chinese with English abstract)
Xing GF and Tao KY.1998.The impact of Sr content on Sr isotope of magmatic rocks during crust-mantle interaction:An application to prtrogenesis of Cretaceous bimodal rocks in the coastal region of southeastern China.Volcanology and Mineral Resources,19(1):24-33(in Chinese with English abstract)
Xing GF,Yang ZL,Xue HM,Shen JL,Zhao Y,Mao JR and Tao KY.1999.The study progress and orientation of Mesozoic volcanic rock belts in southeastern continent,China.Jiangsu Geology,23(4):221-224(in Chinese with English abstract)
Xu BT.1988.Studies of H,O,C and Sr isotopes in metamorphic rocks of the Chencai Group,Zhejiang Province.Geochimica,(2):174-182(in Chinese with English abstract)
Xu XS and Xie X.2005.Late Mesozoic-Cenozoic basaltic rocks and crust-mantle interaction,SE China.Geological Journal of China Universities,11(3):318-334(in Chinese with English abstract)
Xue HM,Tao KY and Shen JL.1996.Sr and Nd isotopic characteristics and magma genesis of Mesozoic volcanic rocks along the coastal region of southeastern China.Acta Geologica Sinica,70(1):35-47(in Chinese with English abstract)
Yang LS.1987.A discussion of the genesis of green alteration band at a uranic ore-field and its significance.Geology of Zhejiang,3(2):46-52(in Chinese with English abstract)
Yang SY,Jiang SY,Zhao KD and Jiang YH.2013.Petrogenesis and tectonic significance of Early Cretaceous high-Zr rhyolite in the Dazhou uranium district,Gan-Hang Belt,Southeast China.Journal of Asian Earth Sciences,74:303-315
Yu YW,Xu BT,Chen JF and Dong CW.2001.Nd isotopic systematics of the late Mesozoic volcanic rocks from southeastern Zhejiang Province,China:Implications for stratigraphic study.Geological Journal of China Universities,7(1):62-69(in Chinese with English abstract)
Yu YW,Jiang Y and Lu CZ.2008.Stratigraphic subdivision and neodymium isotope characteristics of the Cretaceous volcanic rocks in Zhejiang Province.Journal of Stratigraphy,32(1):69-78(in Chinese with English abstract)
Zhang BT,Wu JQ,Qiu ZL and Li Y.1990.On the relationship between hydrothermal alteration and uranium enrichment.Geological Review,36(3):238-244(in Chinese with English abstract)
Zhang BT,Qin SC,Ni QS and Wu JQ.1992.On genesis and ore-control of stratiform green tectonic altered rock on No.661 uranium deposit in western Zhejiang Province.Journal of Nanjing University(Natural Sciences Edition),28(3):439-451(in Chinese with English abstract)
Zhang BT and Zhang ZH.1993.The Evolution of Continental Crust and Uranium Metallization in Southeastern China.Beijing:Atomic Energy Press(in Chinese)
Zhang GQ,Hu RZ,Shang PQ,Tian JJ and Shuang Y.2008.Study on the C-O isotopic composition of calcites and metallogenic dynamics background in the No.302 uranium deposit.Acta Mineralogica Sinica,28(4):413-420(in Chinese with English abstract)
Zhang XP.1999.Formation and evolution of Mesozoic volcanic basins in Gan-Hang tectonic belt.Uranium Geology,15(1):18-23(in Chinese with English abstract)
Zhang ZH.1984.Uranium Geochemistry.Beijing:Atomic Energy Press(in Chinese)
Zhao ZF,Zheng YF,Gong B and Zhao YB.2000.Carbon content and isotope composition of granites from southeastern China.Acta Geologica Sinica,74(1):51-62(in Chinese with English abstract)
Zheng YF.1990.Carbon-oxygen isotopic covariation in hydrothermal calcite during degassing of CO2.A quantitative evaluation and application to the Kushikino gold mining area in Japan.Mineralium Deposita,25(4):246-250
Zheng YF and Hoefs J.1993.Carbon and oxygen isotopic covariations in hydrothermal calcites.Theoretical modeling on mixing processes and application to Pb-Zn deposits in the Harz Mountains,Germany.Mineralium Deposita,28(2):79-89
Zheng YF.2001.Theoretical modeling of stable isotope systems and its applications to geochemistry of hydrothermal ore deposits.Mineral Deposits,20(1):57-70,85(in Chinese with English abstract)
Zhou JX,Huang ZL,Zhou GF and Zeng QS.2012.C,O isotope and REE geochemistry of the hydrothermal calcites from the Tianqiao PbZn ore deposit in NW Guizhou Province,China.Geotectonica et Metallogenia,36(1):93-101(in Chinese with English abstract)
Zhou JX,Wang XC,Wilde SA,Luo K,Huang ZL,Wu T and Jin ZG.2018.New insights into the metallogeny of MVT Zn-Pb deposits:Acase study from the Nayongzhi in South China,using field data,fluid compositions,and in situ S-Pb isotopes.American Mineralogist,103(1):91-108
Zhou JZ.1989.Metallogenic geological conditions of the No.661 uranium deposit.Uranium Geology of East China,(1):6-17(in Chinese)
Zhou XM.2007.Petrogenisis of Late Mesozoic Granite and Dynamic Evolution of Lithosphere in Nanling Region.Beijing:Science Press(in Chinese)
蔡煜琦，张金带，李子颖，郭庆银，宋继叶，范洪海，刘武生，漆富成，张明林．2015．中国铀矿资源特征及成矿规律概要．地质学报，89(6):1051-1069
陈江峰，周泰禧，李学明等．1992．中国东南地区中生代岩浆岩的Sr、Nd同位素组成及其大地构造意义．见:李继亮主编．中国东南海陆岩石圈结构与演化研究．北京:中国科学技术出版社，119-130
邓平，沈渭洲，凌洪飞，叶海敏，王学成，濮巍，谭正中．2003．地幔流体与铀成矿作用:以下庄矿田仙石铀矿床为例．地球化学，32(6):520-528
范洪海，凌洪飞，王德滋，沈渭洲，刘昌实，姜耀辉．2001．江西相山铀矿田成矿物质来源的Nd、Sr、Pb同位素证据．高校地质学报，7(2):139-145
方锡珩．2009．中国火山岩型铀矿的主要地质特征．铀矿地质，25(2):98-104
高必娥，王兴无．1991．裂变径迹法测量熔融包裹体中的铀含量及其意义．地质地球化学，(4):67-68
高雪，孟健寅．2017．滇西北铜厂沟Mo-Cu矿床成矿流体和成矿物质来源:矽卡岩矿物学与稳定同位素证据．岩石学报，33(7):2161-2174
顾明光．2003．浙东南岩头地区磨石山群火山岩岩石地球化学研究．华南地质与矿产，(4):24-30
胡瑞忠，毕献武，苏文超，彭建堂，李朝阳．2004．华南白垩-第三纪地壳拉张与铀成矿的关系．地学前缘，11(1):153-160
胡瑞忠，毛景文，华仁民，范蔚茗．2015．华南陆块陆内成矿作用．北京:科学出版社，1-903
惠小朝，韩效忠，林建平，王明太，张斌，汤江伟，杜江浩，金淼张，雷遥明．2012．浙江衢州大洲火山断陷盆地构造应力场特征及其与铀成矿关系．地质学报，86(2):228-240
金景福，胡瑞忠．1987.302矿床成矿热液中铀的迁移和沉淀．地球化学，(4):320-329
李长江，蒋叙良．1989．浙江武义-东阳地区萤石矿床的锶同位素地球化学研究．矿床地质，8(3):65-74
刘惠三．1986．浙江中生代陆相火山岩型铀矿化特征及其分布规律．浙江地质，2(1):7-31
刘家军，何明勤，李志明，刘玉平，李朝阳，张乾，杨伟光，杨爱平．2004．云南白秧坪银铜多金属矿集区碳氧同位素组成及其意义．矿床地质，23(1):1-10
刘蓉蓉，李子颖，汤江伟，徐小奇．2018．浙江衢州地区铀成矿流体来源及其迁移富集机理．东华理工大学学报(自然科学版)，41(2):101-110
毛孟才．2004．浙江火山岩型铀成矿特征及找矿前景．地质找矿论丛，19(1):8-12,29
戚华文，胡瑞忠．2000．华南花岗岩岩浆期后热液与铀成矿热液的初步对比．矿物学报，20(4):401-405
商朋强，胡瑞忠，毕献武，刘雷，张国全．2006．花岗岩型热液铀矿床C,O同位素研究---以粤北下庄铀矿田为例．矿物岩石，26(3):71-76
商朋强，胡瑞忠，毕献武，张国全，田建吉．2012．粤北下庄铀矿田脉石矿物Sr、Nd、Pb同位素地球化学研究．中国地质，39(6):1847-1856
沈渭洲．1987．稳定同位素地质．北京:原子能出版社
沈渭洲，凌洪飞，王德滋，徐步台，俞云文．1999．浙江省中生代火成岩的Nd-Sr同位素研究．地质科学，34(2):223-232
孙占学．2004．相山铀矿田铀源的地球化学证据．矿物学报，24(1):19-24
田建吉，胡瑞忠，苏文超，张国全，商朋强．2010a.661铀矿床矿石U-Pb等时线年龄及其成矿构造背景．矿床地质，29(3):452-460
田建吉，胡瑞忠，苏文超，张国全，商朋强，齐有强．2010b.661铀矿床流体包裹体特征及成矿流体来源探讨．矿物岩石地球化学通报，29(1):17-23,30
田建吉，胡瑞忠，苏文超，张国全，商朋强，齐有强．2010c.661铀矿床铅同位素组成与成矿物质来源探讨．矿物学报，30(3):304-310
涂光炽．1996．关于CO2若干问题的讨论．地学前缘，3(3-4):53-62
王传文．1983．花岗岩型和火山岩型铀矿化的成因．矿床地质，2(2):59-67
王德滋，周金城，邱检生，范洪海．2000．中国东南部晚中生代花岗质火山-侵入杂岩特征与成因．高校地质学报，6(4):487-498
邢光福，陶奎元．1998．在壳幔作用过程中Sr含量对岩浆岩Sr同位素组成的影响---兼论东南沿海白垩纪双峰式火山岩成因．火山地质与矿产，19(1):24-33
邢光福，杨祝良，薛怀民，沈加林，赵宇，毛建仁，陶奎元．1999．中国东南大陆中生代火山岩带研究进展和方向．江苏地质，23(4):221-224
徐步台．1988．浙江陈蔡群变质岩系的氢、氧、碳及锶稳定同位素研究．地球化学，(2):174-182
徐夕生，谢昕．2005．中国东南部晚中生代-新生代玄武岩与壳幔作用．高校地质学报，11(3):318-334
薛怀民，陶奎元，沈加林．1996．中国东南沿海中生代酸性火山岩的锶和钕同位素特征与岩浆成因．地质学报，70(1):35-47
杨流顺．1987．某铀矿田“绿色层”的成因及其意义．浙江地质，3(2):46-52
俞云文，徐步台，陈江峰，董传万．2001．浙东南中生代晚期火山岩Nd同位素组成及其地层学意义．高校地质学报，7(1):62-69
俞云文，姜禹，卢成忠．2008．浙江白垩纪火山岩的地层划分及钕同位素特征．地层学杂志，32(1):69-78
章邦桐，吴俊奇，丘志力，刘义．1990．论热液蚀变与铀成矿富集作用的关系．地质论评，36(3):238-244
章邦桐，秦社彩，倪琦生，吴俊奇．1992．浙江661铀矿床“绿色层”成因及控矿作用的研究．南京大学学报，28(3):439-451
章邦桐，张祖还．1993．华南东部陆壳演化与铀成矿作用．北京:原子能出版社
张国全，胡瑞忠，商朋强，田建吉，双燕．2008.302铀矿床方解石C-O同位素组成与成矿动力学背景研究．矿物学报，28(4):413-420
张星蒲．1999．赣杭构造带中生代火山盆地的形成和演化．铀矿地质，15(1):18-23
张祖还．1984．铀地球化学．北京:原子能出版社
赵子福，郑永飞，龚冰，赵彦冰．2000．中国东南部花岗岩的碳含量和同位素比值．地质学报，74(1):51-62
郑永飞．2001．稳定同位素体系理论模式及其矿床地球化学应用．矿床地质，20(1):57-70,85
周家喜，黄智龙，周国富，曾乔松．2012．黔西北天桥铅锌矿床热液方解石C、O同位素和REE地球化学．大地构造与成矿学，36(1):93-101
周家志．1989.661铀矿床成矿地质条件．华东铀矿地质，(1):6-17
周新民．2007．南岭地区晚中生代花岗岩成因与岩石圈动力学演化．北京:科学出版社
(1)华东地勘局269大队．1984．六六零矿田六六一、六六三矿床实例报告．内部资料
© 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 |