粤北棉花坑铀矿床热液蚀变与物质迁移研究
|
摘要
本文以粤北长江铀矿区棉花坑铀矿床的横向矿化蚀变剖面为研究对象,系统研究了代表性新鲜花岗岩、蚀变岩和矿石的主量、微量以及稀土元素地球化学特征,运用质量平衡计算方法探讨了各蚀变带组分的迁移规律,以期解决成矿物质来源、成矿流体来源及其性质等问题。结果表明,该矿化蚀变剖面具有明显的水平分带特征,可分为新鲜花岗岩带(Ⅴ带)、远矿碱交代蚀变带(Ⅳ带)、近矿绿泥石化蚀变带(Ⅲ带)、矿旁水云母化蚀变带(Ⅱ带)和矿化中心赤铁矿化蚀变带(Ⅰ带)。从侧缘碱交代带→矿化中心带,Si O2的带入率(0. 27%→0. 21%→0. 50%→0. 70%)整体上与U的带入率(4. 73%→8. 07%→39. 26%→98. 29%)呈正比,K+与Na+相互排斥呈现"钾钠不相容"现象,Mg O与Mn O呈现出"此消彼长"的迁移特征,是对流平衡迁移方式的表现。Th、Pb、Cs、Mo、As元素在矿化中心带的带入率最大,Ba、Sr、Co、V元素在矿化中心带迁出率最小,这对铀成矿(铀矿化)具有很好的指示作用。根据各蚀变带元素的含量、比值及迁移特征,结合前人的研究成果,认为矿床的成矿物质主要来源于赋矿围岩长江岩体,成矿流体在成分上富含挥发分和矿化剂(CO_2、F、H_2O等)、碱金属元素(K、Cs、Rb)和重稀土元素,性质上具相对高的氧逸度,其来源是地幔流体与经历了深循环大气降水的混合成因流体。挥发分和矿化剂(CO_2、F、H_2O等)的带入是矿床重要的矿质迁移机制,CO2的逸出伴随着氧化向还原过渡的环境是矿床重要的矿质沉淀机制。
In this paper,the major,trace and rare earth elements of representative fresh samples of granites,altered rocks and ores were studied from the mineralization-alteration cross section in Mianhuakeng uranium deposit,northern Guangdong Province. Using the method of mass balance calculation,the migration law of components in each alteration zone was discussed to solve the problems of the source of ore-forming materials,source of ore-forming fluids and their properties. The results show that the mineralization-alteration cross section has obvious horizontal zoning characteristics,which can be divided into the fresh granite zone( Ⅴ),the alkali metasomatic alteration zone( Ⅳ),the chloritization alteration zone( Ⅲ),the hydromicatization alteration zone( Ⅱ) and the hematitization alteration zone(Ⅰ). From the lateral alteration zone( the alkali metasomatic zone) to the central mineralization zone( the hematite alteration zone),the immigration rate of SiO_2( 0. 27% →0. 21% →0. 50% →0. 70%) was positive to the immigration rate of U element( 4. 73% →8. 07% →39. 26% →98. 29%). K+and Na+were mutually exclusive and incompatible,Mg O and Mn O exhibit a negative relationship,which might show a balanced convection migration. Th,Pb,Cs,Mo and As elements have the highest immigration rate in the central mineralization zone,while Ba,Sr,Co and V elements have the lowest migration rate in the central mineralization zone,which could be used as a good indication for uranium mineralization. According to the content,ratio and migration characteristics of the elements in each alteration zone and combine to the previously published data,it is considered that the ore-forming materials of the deposit are mainly contributed by the host rock,the Changjiang granite. The ore-forming fluids were rich in volatiles and mineralization agents( CO_2,F,H_2 O,etc.),alkali metals( K,Cs,Rb) and HREE with relatively high oxygen fugacity,and its sources were a mixture of mantle fluids and meteoric waters during the deep circulation. The introduction of volatiles and mineralization agents were the important mechanism for mineral migration of the deposit,and the environment from oxidation to reduction with CO_2 escape was an important mechanism for mineral precipitation of the deposit.
In this paper,the major,trace and rare earth elements of representative fresh samples of granites,altered rocks and ores were studied from the mineralization-alteration cross section in Mianhuakeng uranium deposit,northern Guangdong Province. Using the method of mass balance calculation,the migration law of components in each alteration zone was discussed to solve the problems of the source of ore-forming materials,source of ore-forming fluids and their properties. The results show that the mineralization-alteration cross section has obvious horizontal zoning characteristics,which can be divided into the fresh granite zone( Ⅴ),the alkali metasomatic alteration zone( Ⅳ),the chloritization alteration zone( Ⅲ),the hydromicatization alteration zone( Ⅱ) and the hematitization alteration zone(Ⅰ). From the lateral alteration zone( the alkali metasomatic zone) to the central mineralization zone( the hematite alteration zone),the immigration rate of SiO_2( 0. 27% →0. 21% →0. 50% →0. 70%) was positive to the immigration rate of U element( 4. 73% →8. 07% →39. 26% →98. 29%). K+and Na+were mutually exclusive and incompatible,Mg O and Mn O exhibit a negative relationship,which might show a balanced convection migration. Th,Pb,Cs,Mo and As elements have the highest immigration rate in the central mineralization zone,while Ba,Sr,Co and V elements have the lowest migration rate in the central mineralization zone,which could be used as a good indication for uranium mineralization. According to the content,ratio and migration characteristics of the elements in each alteration zone and combine to the previously published data,it is considered that the ore-forming materials of the deposit are mainly contributed by the host rock,the Changjiang granite. The ore-forming fluids were rich in volatiles and mineralization agents( CO_2,F,H_2 O,etc.),alkali metals( K,Cs,Rb) and HREE with relatively high oxygen fugacity,and its sources were a mixture of mantle fluids and meteoric waters during the deep circulation. The introduction of volatiles and mineralization agents were the important mechanism for mineral migration of the deposit,and the environment from oxidation to reduction with CO_2 escape was an important mechanism for mineral precipitation of the deposit.
引文
Ague JJ.1994.Mass transfer during Barrovian metamorphism of pelites,South-Central Connecticut:1.Evidence for changes in composition and volume.American Journal of Science,294(8):989-1057
Ague JJ and van Haren JLM.1996.Assessing metasomatic mass and volume changes using the bootstrap,with application to deep crustal hydrothermal alteration of marble.Economic Geology,91(7):1169-1182
Ague JJ.1997.Crustal mass transfer and index mineral growth in Barrow’s garnet zone,Northeast Scotland.Geology,25(1):73-76
Bonnetti C,Liu XD,Mercadier J,Cuney M,Deloule E,Villeneuve Jand Liu WQ.2018.The genesis of granite-related hydrothermal uranium deposits in the Xiazhuang and Zhuguang ore fields,North Guangdong Province,SE China:Insights from mineralogical,trace elements and U-Pb isotopes signatures of the U mineralisation.Ore Geology Reviews,92:588-612
Brugger J,Liu WH,Etschmann B,Mei Y,Sherman DM and Testemale D.2016.A review of the coordination chemistry of hydrothermal systems,or do coordination changes make ore deposits?Chemical Geology,447:219-253
Campbell IH,Lesher CM,Coad P,Franklin JM,Gorton MP and Thurston PC.1984.Rare-earth element mobility in alteration pipes below massive Cu-Zn-sulfide deposits.Chemical Geology,45(3-4):181-202
Chen YF,Wang YW,Wang JB,Wang LJ,Tang PZ,Shi Y and Zhao LT.2018.Greisenized alteration-mineralization geochemistry of the tin deposit related to A-type granite:Case study on the Kamusite and Ganliangzi deposits,Xinjiang.Earth Science,43(9):3154-3168(in Chinese with English abstract)
Chen ZY,Huang GL,Zhu B,Chen ZH,Huang F,Zhao Z and Tian ZJ.2014.The characteristics and metallogenic specialization of granitehosted uranium deposits in the Nanling region.Geotectonica et Metallogenia,38(2):264-275(in Chinese with English abstract)
Deng HL,Tu GZ,Li CY and Liu CQ.1999.Mass balance of open geochemical systems:1.Theory.Acta Mineralogica Sinica,19(2):121-131(in Chinese with English abstract)
Deng P,Shu LS and Tan ZZ.2003.The geological setting for the formation of rich uranium ores in Zhuguang-Guidong large-scale uranium metallogenetic area.Geological Review,49(5):486-494(in Chinese with English abstract)
Fletcher RC and Merino E.2001.Mineral growth in rocks:Kineticrheological models of replacement,vein formation,and syntectonic crystallization.Geochimica et Cosmochimica Acta,65(21):3733-3748
Fourcade S and Allegre CJ.1981.Trace elements behavior in granite genesis:A case study the calc-alkaline plutonic association from the Querigut complex(Pyrénées,France).Contributions to Mineralogy and Petrology,76(2):177-195
Fu LW.2015.Study on wall rock alteration zoning,the source of oreforming fluid and ore-forming material of the 302 uranium deposit in northern Guangdong Province.Master Degree Thesis.Nanjing:Nanjing University,1-67(in Chinese with English summary)
Gao F,Lin JR,Zhong QL,Guo SY,Pang YQ,Rong JS and Hu ZH.2011.The wall rock alteration and its geochemical characteristics of uranium deposit No.302.Uranium Geology,27(5):274-281(in Chinese with English abstract)
Gao S,Luo TC,Zhang BR,Zhang HF,Han YW,Zhao ZD and Hu YK.1998.Chemical composition of the continental crust as revealed by studies in East China.Geochimica et Cosmochimica Acta,62(11):1959-1975
Gao S,Luo TC,Zhang BR,Zhang HF,Han YW,Zhao ZD and Kern H.1999.Chemical composition of the continental crust as revealed by studies in East China.Science in China(Series D),29(3):204-213(in Chinese)
Gao X,Shen WZ,Liu LL,Yao W,Zhu B,Huang GL and Li QY.2011.Geochemical characteristics and causes of wall rock alteration in the No.302 uranium deposit,northern Guangdong.Acta Petrologica et Mineralogica,30(1):71-82(in Chinese with English abstract)
Grant JA.1986.The isocon diagram:A simple solution to Gresens’equation for metasomatic alteration.Economic Geology,81(8):1976-1982
Gresens RL.1967.Composition-volume relationships of metasomatism.Chemical Geology,2:47-55
Guo J.2014.Study on uranium mineralization and alteration of the scientific deep drilling rocks in Xiangshan uranium orefield.Master Degree Thesis.Beijing:Beijing Research Institute of Uranium Geology,1-99(in Chinese with English summary)
Guo S,Ye K,Chen Y and Liu JB.2009.A normalization solution to mass transfer illustration of multiple progressively altered samples using the Isocon diagram.Economic Geology,104(6):881-886
Guo S,Ye K,Chen Y,Liu JB and Zhang LM.2013.Introduction of mass-balance calculation method for component transfer during the opening of a geological system.Acta Petrologica Sinica,29(5):1486-1498(in Chinese with English abstract)
Han YW and Ma ZD.2013.Geochemistry.Beijing:Geological Publishing House,71-80(in Chinese)
Hoefs J.1997.Stable Isotope Geochemistry.Berlin:Springer,1-201
Hu BQ,Lv GX,Sun ZX,Li MG,Shi WJ,Li XL,Wang Y and Bai LH.2011.Mineralization and fracture-water phase transition coupling in the Xiangshan uranium ore field,Jiangxi.Geotectonica et Metallogenia,35(4):502-512(in Chinese with English abstract)
Hu BQ,Wang Q,Qiu LF,Sun ZX,Wang Y,Lv GX and Hu RQ.2016.Geochemistry of alkali metasomatized rocks of Zoujiashan uranium ore-deposit in Xiangshan ore-field.Geotectonica et Metallogenia,40(2):377-385(in Chinese with English abstract)
Hu RZ and Jin JF.1988.Genesis and origin of the Guidong granitic batholith.Journal of Chengdu College of Geology,15(3):20-28(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 and Zhou MF.2012.Multiple mesozoic mineralization events in South China:An introduction to the thematic issue.Mineralium Deposita,47(6):579-588
Hu RZ,Mao JW,Hua RM and Fan WM.2015.Intra-Continental Mineralization of South China Craton.Beijing:Science Press,1-903(in Chinese)
Huang GL,Yin ZP,Ling HF,Deng P,Zhu B and Shen WZ.2010.Formation age,geochemical characteristics and genesis of pitchblende from No.302 uranium deposit in northern Guangdong.Mineral Deposits,29(2):352-360(in Chinese with English abstract)
Huang GL,Cao HJ,Ling HF,Shen WZ,Wang XD and Fu SC.2012.Zircon SHRIMP U-Pb age,geochemistry and genesis of the Youdong granite in northern Guangdong.Acta Geologica Sinica,86(4):577-586(in Chinese with English abstract)
Huang GL,Liu XY,Sun LQ,Li ZS and Zhang SJ.2014.Zircon U-Pb dating,geochemical characteristic and genesis of the Changjiang granite in northern Guangdong.Acta Geologica Sinica,88(5):836-849(in Chinese with English abstract)
Jiang YH,Jiang SY and Ling HF.2004.Mantle-derived fluids and uranium mineralization.Earth Science Frontiers,11(2):491-499(in Chinese with English abstract)
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 in Southeast China.Economic Geology,101(8):1613-1622
Jin JF and Hu RZ.1985.The genesis of uranium deposit No.302.Journal of Chengdu College of Geology,(4):1-11(in Chinese with English abstract)
Jin JF,Ni SJ and Hu RZ.1992.Vertical zoning of hydrothermal dikes in the No.302 uranium deposit and the cause of its formation.Mineral Deposits,11(3):252-258(in Chinese with English abstract)
Li HD,Pan JY,Xia F,Zhou JY,Liu Y and Zhong FJ.2016.Hydrothermal alteration and its geochemical characteristics of Lijialing deposit in Xiangshan uranium ore deposit.Geoscience,30(3):555-566(in Chinese with English abstract)
Li XH.1996.A discussion on the model and isochron ages of Sm-Nd isotopic systematics:Suitability and limitation.Scientia Geologica Sinica,31(1):97-103(in Chinese with English abstract)
Li XH,Hu RZ and Rao B.1997.Geochronology and geochemistry of Cretaceous mafic dikes from northern Guangdong,SE China.Geochimica,26(2):14-31(in Chinese with English abstract)
Ling HF.2011.Origin of hydrothermal fluids of granite-type uranium deposits:Constraints from redox conditions.Geological Review,57(2):193-206(in Chinese with English abstract)
Liu CQ,Huang ZL,Li HP and Su GL.2001.The geofluid in the mantle and its role in ore-forming processes.Earth Science Frontiers,8(4):231-243(in Chinese with English abstract)
Liu GQ,Zhao KD,Jiang SY and Wei C.2018.In-situ sulfur isotope and trace element analysis of pyrite from the Xiwang uranium ore deposit in South China:Implication for ore genesis.Journal of Geochemical Exploration,195:49-65
Liu JG,Li ZY,Huang ZZ,Li XZ and Nie JT.2017.The element mobility study of uranium mineralization alteration zones in Xiangshan,Jiangxi using the drill core CUSD3.Acta Geologica Sinica,91(4):896-912(in Chinese with English abstract)
Lu XL,Zhu MQ and Wu T.2015.Study on the stable isotope composition and hydrothermal fluids origin of uranium deposits in southern Zhuguangshan pluton.Uranium Geology,31(2):65-72(in Chinese with English abstract)
Luo Y,Wang MT,LI JH and Ma HF.2002.Geological characteristics and metallogenetic model of Zhuguang uranium ore concentrated area.China Nuclear Science and Technology Report,452-467(in Chinese with English abstract)
Mou BL.1999.Element Geochemistry.Beijing:Peking University Press,1-177(in Chinese)
Ni SJ and Jin JF.1992.The mixing and boiling of hydrothermal solution of uranium deposit No.302 and the geological interpretation.Journal of Chengdu College of Geology,(4):9-15(in Chinese with English abstract)
Ohmoto H.1986.Stable isotope geochemistry of ore deposits.Reviews in Mineralogy and Geochemistry,16(1):491-559
Qi JM,Huang GL,Zhu B,Fu SC,Xu Y and Ye SX.2014.Compositions study of auxiliary minerals in altered granitic rocks of the Mianhuakeng uranium deposit in northern Guangdong.Acta Geologica Sinica,88(9):1691-1704(in Chinese with English abstract)
Qi JM,Ye SX,Fang XQ,Cao HJ and Tang SY.2019.Study on hydrogeochemical and recharge sources characteristics of geothermal water in the Mianhuakeng uranium deposit,Renhua,northern Guangdong.Geological Review,65(1):199-210(in Chinese with English abstract)
Qu XM,Hou ZQ and Li YG.2004.Melt components derived from a subducted slab in late orogenic ore-bearing porphyries in the Gangdese copper belt,southern Tibetan Plateau.Lithos,74(3-4):131-148
Rosenbaum JM,Wilson M and Condliffe E.1997.Partial melts of subducted phosphatic sediments in the mantle.Geology,25(1):77-80
Shen WZ,Ling HF,Deng P,Zhu B,Huang GL and Tan ZZ.2010.Study on isotope geochemistry of uranium deposit 302 in northern Guangdong Province.Uranium Geology,26(2):80-87(in Chinese with English abstract)
Shu LS,Zhou XM,Deng P and Yu XQ.2006.Principal geological features of Nanling tectonic belt,South China.Geological Review,52(2):251-265(in Chinese with English abstract)
Sun LQ.2018.Petrogenesis of the Mesozoic granites in the Zhuguangshan area in the Nanling Region and their implications for the uranium mineralization.Ph.D.Dissertation.Nanjing:Nanjing University,1-192(in Chinese with English summary)
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publications,42(1):313-345
Wang CY,Li XF,Xiao R,Bai YP,Yang F,Mao W and Jiang SK.2012.Elements mobilization of mineralized porphyry rocks during hydrothermal alteration at Zhushahong porphyry copper deposit,Dexing district,South China.Acta Petrologica Sinica,28(12):3869-3886(in Chinese with English abstract)
Wang LK and Liu TG.1987.H,O,S,Pb isotopic studies of uranium ore deposits in granitoid rocks of South China.Geochimica,(1):67-78(in Chinese with English abstract)
Wang LX,Ma CQ,Lai ZX,Marks MAW,Zhang C and Zhong YF.2015.Early Jurassic mafic dykes from the Xiazhuang ore district(South China):Implications for tectonic evolution and uranium metallogenesis.Lithos,239:71-85
Wang MT,Luo Y,Sun ZF,Zhu JC and Li JH.1999.Discussion on genesis of uranium deposits in Zhuguang uranium metallogenic region.Uranium Geology,15(5):279-285(in Chinese with English abstract)
Wang ZQ and Li ZY.2007.Discussion on mantle-derived uranium mineralization.Geological Review,53(5):608-615(in Chinese with English abstract)
Wang ZQ,Fan HH,Chen DH,Zheng KZ,Luo QH,Liu JG,Wang FGand Wang YJ.2018.Geochemistry,element migration and mechanism of uranium mineralization in the periphery of the Shazijiang uranium ore deposit.Geological Journal of China Universities,24(2):185-199(in Chinese with English abstract)
Wei B.2011.Adsorption of rare earth elements La,Nd by clay minerals inorganic elements of soils.Master Degree Thesis.Hefei:Anhui Agricultural University,1-57(in Chinese with English summary)
Wei JH,Liu CQ and Ding ZJ.2000.Active laws of element migration in wall-rock alteration processes for hydrothermal gold deposits:As evidenced by Dongping,Hougou and Shuijingtun gold deposits.Acta Mineralogica Sinica,20(2):200-206(in Chinese with English abstract)
Wu DH,Pan JY,Xia F,Huang GW,Zhong FJ,Qi JY,Hong BY and Zhou TB.2018.Characteristics and formation conditions of chlorite in the Shangjiao uranium deposit in the southern Jiangxi Province,China.Acta Mineralogica Sinica,38(4):393-405(in Chinese with English abstract)
Wu DH,Pan JY,Xia F,Huang GW and Lai J.2019.The mineral chemistry of chlorites and its relationship with uranium mineralization from Huangsha uranium mining area in the middle Nanling range,SEChina.Minerals,9(3):199
Wu DH,Pan JY,Xia F,Huang GW,Zhong FJ,Lai J,Qi JM and Liu YL.2019.Characteristics and source significance of rare earth elements geochemistry of fluorite from Shangjiao uranium deposit in southern Jiangxi Province.Chinese Rare Earths,40(2):14-27(in Chinese with English abstract)
Yan DP,Zhou MF,Song HL,Wang XW and Malpas J.2003.Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block(South China).Tectonophysics,361(3-4):239-254
Yu DG.1979.Evolution of Yanshan granite and uranium mineralization enrichment:Discussion on diagenesis and mineralization relationship of some uranium-bearing rocks in South China.Uranium Geology,(4):13-25(in Chinese with English abstract)
Yu DG,Wu RG and Chen PR.2005.Uranium Geology.Harbin:Harbin Engineering University Press,1-450(in Chinese)
Zhang BL,Shan W,Li DP,Xiao BJ,Wang ZL and Zhang RZ.2017.Hydrothermal alteration in the Dayingezhuang gold deposit,Jiaodong,China.Acta Petrologica Sinica,33(7):2256-2272(in Chinese with English abstract)
Zhang BT,Dai YS,Wang NS and Liu JS.1988.Geochemical criteria for uranium metallogene-tic capacity of granitoids in South China.Chinese Journal of Nuclear Science&Engineering,8(2):153-164(in Chinese with English abstract)
Zhang GQ,Hu RZ,Bi XW,Feng HS,Shang PQ and Tian JJ.2007.REE geochemical characteristics of the No.302 uranium deposit in northern Guangdong,South China.Chinese Journal of Geochemistry,26(4):425-433
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 urnaium deposit.Acta mineralogica Sinica,28(4):413-420(in Chinese with English abstract)
Zhang GQ,Hu RZ,Jiang GH,Liu S,Zhu WG,Tian JJ,Shuang Y and Fan XR.2010.Mantle derived volatile components involved in uranium mineralization:Evidence from He isotopes of the No.302uranium deposit.Geochimica,39(4):386-395(in Chinese with English abstract)
Zhang KQ and Yang Y.2002.Introduction of the method for mass balance calculation in altered rocks.Geological Science and Technology Information,21(3):104-107(in Chinese with English abstract)
Zhang L,Chen ZY,Li SR,Santosh M,Huang GL and Tian ZJ.2017.Isotope geochronology,geochemistry,and mineral chemistry of the U-bearing and barren granites from the Zhuguangshan complex,South China:Implications for petrogenesis and uranium mineralization.Ore Geology Reviews,91:1040-1065
Zhang L,Chen ZY,Li SR and Huang GL.2018.Characteristics of uranium minerals in wall rock alteration zones of the Mianhuakeng(No.302)uranium deposit,northern Guangdong,South China.Acta Petrologica Sinica,34(9):2657-2670(in Chinese with English abstract)
Zhang M,Chen PR,Huang GL and Ling HF.2006.The research on the geochemical characteristics of Longyuanba composite pluton in Nanling region.Uranium Geology,22(6):336-344(in Chinese with English abstract)
Zhang YC.2002.Alkalic mantle fluids and uranium ore-formation in Zhuguang and Guidong granitic massifs.Uranium Geology,18(4):210-219(in Chinese with English abstract)
Zhang ZH and Zhang BT.1991.On the Uranium-Bearing Granites and Their Related Uranium Deposits in South China.Beijing:Atomic Energy Press,13-15(in Chinese)
Zhao ZF,Zheng YF,Wei CS and Gong B.2001.Carbon concentration and isotope composition of granites from Southeast China.Physics and Chemistry of the Earth,Part A:Solid Earth&Geodesy,26(9-10):821-833
Zhao ZH.1992.Geochemical characteristics of trace elements.Advances in Earth Science,7(5):65-66(in Chinese with English abstract)
Zhong FJ.2018.Petrogenesis and mineralization of granite type uranium deposits in South China:A case study of the Changjiang uranium ore field in northern Guangdong Province.Ph.D.Dissertation.Nanchang:East China University of Technology,1-226(in Chinese with English summary)
Zhong FJ,Pan JY,Qi JM,Yan J,Liu WQ and Li HD.2018.New insitu La-ICP-MS U-Pb ages of uraninite from the Mianhuakeng uranium deposit,northern Guangdong Province,China:Constraint on the metallogenic mechanism.Acta Geologica Sinica,92(2):852-854
Zhong J,Fan HH,Gu DZ,Wang SY,Chen JY,Shi CH and Li HQ.2016.Major and trace element migration and metallogenic processes of the Xinshuijing U-Th deposit in the Longshoushan metallogenic belt,Gansu Province.Geology in China,43(4):1393-1408(in Chinese with English abstract)
Zhong J,Chen YJ and Pirajno F.2017.Geology,geochemistry and tectonic settings of the molybdenum deposits in South China:Areview.Ore Geology Reviews,81:829-855
陈言飞，王玉往，王京彬，王莉娟，唐萍芝，石煜，赵路通．2018．与A型花岗岩有关锡矿的云英岩化蚀变矿化地球化学:以新疆卡姆斯特和干梁子矿床为例．地球科学，43(9):3154-3168
陈振宇，黄国龙，朱捌，陈郑辉，黄凡，赵正，田泽瑾．2014．南岭地区花岗岩型铀矿的特征及其成矿专属性．大地构造与成矿学，38(2):264-275
邓海琳，涂光炽，李朝阳，刘丛强．1999．地球化学开放系统的质量平衡:1．理论．矿物学报，19(2):121-131
邓平，舒良树，谭正中．2003．诸广-贵东大型铀矿聚集区富铀矿成矿地质条件．地质论评，49(5):486-494
傅丽雯．2015．粤北302铀矿床围岩蚀变分带、成矿流体与成矿物质来源研究．硕士学位论文．南京:南京大学，1-67
高飞，林锦荣，钟启龙，郭树英，庞雅庆，戎家树，胡志华．2011.302铀矿床围岩蚀变分带性及地球化学特征．铀矿地质，27(5):274-281
高山，骆庭川，张本仁，张宏飞，韩吟文，赵志丹，Kern H.1999．中国东部地壳的结构和组成．中国科学(D辑)，29(3):204-213
高翔，沈渭洲，刘莉莉，姚薇，朱捌，黄国龙，李秋英．2011．粤北302铀矿床围岩蚀变的地球化学特征和成因研究．岩石矿物学杂志，30(1):71-82
郭建．2014．相山铀矿田科学深钻岩石铀矿化蚀变作用研究．硕士学位论文．北京:核工业北京地质研究院，1-99
郭顺，叶凯，陈意，刘景波，张灵敏．2013．开放地质体系中物质迁移质量平衡计算方法介绍．岩石学报，29(5):1486-1498
韩吟文，马振东．2003．地球化学．北京:地质出版社，71-80
胡宝群，吕古贤，孙占学，李满根，史维浚，李学礼，王运，白丽红．2011．江西相山铀矿田中断裂与水相变耦合成矿---以邹家山矿床铀成矿作用分析为例．大地构造与成矿学，35(4):502-512
胡宝群，王倩，邱林飞，孙占学，王运，吕古贤，胡荣泉．2016．相山矿田邹家山铀矿床碱交代矿化蚀变岩地球化学．大地构造与成矿学，40(2):377-385
胡瑞忠，金景福．1988．论贵东花岗岩体的成因及其起源．成都地质学院学报，15(3):20-28
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
黄国龙，尹征平，凌洪飞，邓平，朱捌，沈渭洲．2010．粤北地区302矿床沥青铀矿的形成时代、地球化学特征及其成因研究．矿床地质，29(2):352-360
黄国龙，曹豪杰，凌洪飞，沈渭洲，王小冬，伏顺成．2012．粤北油洞岩体SHRIMP锆石U-Pb年龄、地球化学特征及其成因研究．地质学报，86(4):577-586
黄国龙，刘鑫扬，孙立强，李钟枢，张世佳．2014．粤北长江岩体的锆石U-Pb定年、地球化学特征及其成因研究．地质学报，88(5):836-849
姜耀辉，蒋少涌，凌洪飞．2004．地幔流体与铀成矿作用．地学前缘，11(2):491-499
金景福，胡瑞忠．1985.302矿床成因探讨．成都地质学院学报，(4):1-11
金景福，倪师军，胡瑞忠．1992.302铀矿床热液脉体的垂直分带及其成因探讨．矿床地质，11(3):252-258
李海东，潘家永，夏菲，周加云，刘颖，钟福军．2016．相山李家岭铀矿床热液蚀变作用地球化学特征．现代地质，30(3):555-566
李献华．1996.Sm-Nd模式年龄和等时线年龄的适用性与局限性．地质科学，31(1):97-103
李献华，胡瑞忠，饶冰．1997．粤北白垩纪基性岩脉的年代学和地球化学．地球化学，26(2):14-31
凌洪飞．2011．论花岗岩型铀矿床热液来源---来自氧逸度条件的制约．地质论评，57(2):193-206
刘丛强，黄智龙，李和平，苏根利．2001．地幔流体及其成矿作用．地学前缘，8(4):231-243
刘军港，李子颖，黄志章，李秀珍，聂江涛．2017．江西相山CUSD3钻孔铀矿化蚀变带元素活动性探讨．地质学报，91(4):896-912
卢小亮，祝民强，邬铁．2015．诸广岩体南部铀矿区稳定同位素组成及矿床成因分析．铀矿地质，31(2):65-72
罗毅，王明太，李建红，马汉峰．2002．诸广铀矿集区成矿地质特征及成矿模式．中国核科技报告，452-467
牟保磊．1999．元素地球化学．北京大学出版社，1-177
倪师军，金景福．1992.302铀矿床热液的混合和沸腾及其地质意义．成都地质学院学报，(4):9-15
祁家明，黄国龙，朱捌，伏顺成，许幼，叶松鑫．2014．粤北棉花坑铀矿床蚀变花岗岩副矿物特征研究．地质学报，88(9):1691-1704
祁家明，叶松鑫，方晓骐，曹豪杰，唐仕尧．2019．粤北仁化棉花坑铀矿床地下热水地球化学特征及补给来源研究．地质论评，65(1):199-210
沈渭洲，凌洪飞，邓平，朱捌，黄国龙，谭正中．2010．粤北302铀矿床同位素地球化学研究．铀矿地质，26(2):80-87
舒良树，周新民，邓平，余心起．2006．南岭构造带的基本地质特征．地质论评，52(2):251-265
孙立强．2018．南岭诸广山地区中生代花岗岩成因及其对铀成矿作用的启示．博士学位论文．南京:南京大学，1-192
王翠云，李晓峰，肖荣，白艳萍，杨锋，毛伟，蒋松坤．2012．德兴朱砂红斑岩铜矿热液蚀变作用及元素地球化学迁移规律．岩石学报，28(12):3869-3886
王联魁，刘铁庚．1987．华南花岗岩铀矿H、O、S、Pb同位素研究．地球化学，(1):67-78
王明太，罗毅，孙志富，朱杰辰，李建红．1999．诸广铀成矿区矿床成因探讨．铀矿地质，15(5):279-285
王正其，李子颖．2007．幔源铀成矿作用探讨．地质论评，53(5):608-615
王正庆，范洪海，陈东欢，郑可志，罗桥花，刘军港，王凤岗，王勇剑．2018．沙子江铀矿外围地化特征、元素迁移及铀成矿机理．高校地质学报，24(2):185-199
魏斌．2011．粘土矿物及土壤无机相对稀土元素La、Nd的吸附性研究．硕士学位论文．合肥:安徽农业大学，1-57
魏俊浩，刘丛强，丁振举．2000．热液型金矿床围岩蚀变过程中元素迁移规律---以张家口地区东坪、后沟、水晶屯金矿为例．矿物学报，20(2):200-206
吴德海，潘家永，夏菲，黄广文，钟福军，祁家明，洪斌跃，周堂波．2018．赣南上窖铀矿床绿泥石特征与形成环境．矿物学报，38(4):393-405
吴德海，潘家永，夏菲，黄广文，钟福军，赖静，祁家明，刘院龙．2019．赣南上窖铀矿床萤石稀土元素地球化学特征及其源区意义．稀土，40(2):14-27
余达淦．1979．燕山花岗岩演化与铀矿化富集---对华南一些含铀岩体成岩成矿关系探讨．铀矿地质，(4):13-25
余达淦，吴仁贵，陈培荣．2005．铀资源地质学．哈尔滨:哈尔滨工程大学出版社，1-450
张炳林，单伟，李大鹏，肖丙建，王中亮，张瑞忠．2017．胶东大尹格庄金矿床热液蚀变作用．岩石学报，33(7):2256-2272
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
张国全，胡瑞忠，蒋国豪，刘燊，朱维光，田建吉，双燕，范效仁．2010．幔源挥发性组分参与302铀矿床成矿作用的氦同位素证据．地球化学，39(4):386-395
张可清，杨勇．2002．蚀变岩质量平衡计算方法介绍．地质科技情报，21(3):104-107
张龙，陈振宇，李胜荣，黄国龙．2018．粤北棉花坑(302)铀矿床围岩蚀变分带的铀矿物研究．岩石学报，34(9):2657-2670
张敏，陈培荣，黄国龙，凌洪飞．2006．南岭龙源坝复式岩体的地球化学特征研究．铀矿地质，22(6):336-344
张彦春．2002．诸广、贵东花岗岩中碱性地幔流体与铀成矿．铀矿地质，18(4):210-219
张祖还，章邦桐．1991．华南产铀花岗岩及有关铀矿床研究．北京:原子能出版社，13-15
章邦桐，戴永善，王年生，刘继顺．1988．华南花岗岩铀成矿能力的地球化学判别标志．核科学与工程，8(2):153-164
赵振华．1992．微量元素地球化学．地球科学进展，7(5):65-66
钟福军．2018．华南花岗岩型铀矿成岩成矿作用研究---以粤北长江铀矿田为例．博士学位论文．南昌:东华理工大学，1-226
钟军，范洪海，顾大钊，王生云，陈金勇，史长昊，李恒强．2016．甘肃龙首山成矿带新水井铀(钍)矿床元素迁移规律及成矿作用过程研究．中国地质，43(4):1393-1408
(1)中国核工业地质局《华南铀矿地质志》编写组．2005．华南铀矿地质志．中国核工业地质局内部资料
Ague JJ and van Haren JLM.1996.Assessing metasomatic mass and volume changes using the bootstrap,with application to deep crustal hydrothermal alteration of marble.Economic Geology,91(7):1169-1182
Ague JJ.1997.Crustal mass transfer and index mineral growth in Barrow’s garnet zone,Northeast Scotland.Geology,25(1):73-76
Bonnetti C,Liu XD,Mercadier J,Cuney M,Deloule E,Villeneuve Jand Liu WQ.2018.The genesis of granite-related hydrothermal uranium deposits in the Xiazhuang and Zhuguang ore fields,North Guangdong Province,SE China:Insights from mineralogical,trace elements and U-Pb isotopes signatures of the U mineralisation.Ore Geology Reviews,92:588-612
Brugger J,Liu WH,Etschmann B,Mei Y,Sherman DM and Testemale D.2016.A review of the coordination chemistry of hydrothermal systems,or do coordination changes make ore deposits?Chemical Geology,447:219-253
Campbell IH,Lesher CM,Coad P,Franklin JM,Gorton MP and Thurston PC.1984.Rare-earth element mobility in alteration pipes below massive Cu-Zn-sulfide deposits.Chemical Geology,45(3-4):181-202
Chen YF,Wang YW,Wang JB,Wang LJ,Tang PZ,Shi Y and Zhao LT.2018.Greisenized alteration-mineralization geochemistry of the tin deposit related to A-type granite:Case study on the Kamusite and Ganliangzi deposits,Xinjiang.Earth Science,43(9):3154-3168(in Chinese with English abstract)
Chen ZY,Huang GL,Zhu B,Chen ZH,Huang F,Zhao Z and Tian ZJ.2014.The characteristics and metallogenic specialization of granitehosted uranium deposits in the Nanling region.Geotectonica et Metallogenia,38(2):264-275(in Chinese with English abstract)
Deng HL,Tu GZ,Li CY and Liu CQ.1999.Mass balance of open geochemical systems:1.Theory.Acta Mineralogica Sinica,19(2):121-131(in Chinese with English abstract)
Deng P,Shu LS and Tan ZZ.2003.The geological setting for the formation of rich uranium ores in Zhuguang-Guidong large-scale uranium metallogenetic area.Geological Review,49(5):486-494(in Chinese with English abstract)
Fletcher RC and Merino E.2001.Mineral growth in rocks:Kineticrheological models of replacement,vein formation,and syntectonic crystallization.Geochimica et Cosmochimica Acta,65(21):3733-3748
Fourcade S and Allegre CJ.1981.Trace elements behavior in granite genesis:A case study the calc-alkaline plutonic association from the Querigut complex(Pyrénées,France).Contributions to Mineralogy and Petrology,76(2):177-195
Fu LW.2015.Study on wall rock alteration zoning,the source of oreforming fluid and ore-forming material of the 302 uranium deposit in northern Guangdong Province.Master Degree Thesis.Nanjing:Nanjing University,1-67(in Chinese with English summary)
Gao F,Lin JR,Zhong QL,Guo SY,Pang YQ,Rong JS and Hu ZH.2011.The wall rock alteration and its geochemical characteristics of uranium deposit No.302.Uranium Geology,27(5):274-281(in Chinese with English abstract)
Gao S,Luo TC,Zhang BR,Zhang HF,Han YW,Zhao ZD and Hu YK.1998.Chemical composition of the continental crust as revealed by studies in East China.Geochimica et Cosmochimica Acta,62(11):1959-1975
Gao S,Luo TC,Zhang BR,Zhang HF,Han YW,Zhao ZD and Kern H.1999.Chemical composition of the continental crust as revealed by studies in East China.Science in China(Series D),29(3):204-213(in Chinese)
Gao X,Shen WZ,Liu LL,Yao W,Zhu B,Huang GL and Li QY.2011.Geochemical characteristics and causes of wall rock alteration in the No.302 uranium deposit,northern Guangdong.Acta Petrologica et Mineralogica,30(1):71-82(in Chinese with English abstract)
Grant JA.1986.The isocon diagram:A simple solution to Gresens’equation for metasomatic alteration.Economic Geology,81(8):1976-1982
Gresens RL.1967.Composition-volume relationships of metasomatism.Chemical Geology,2:47-55
Guo J.2014.Study on uranium mineralization and alteration of the scientific deep drilling rocks in Xiangshan uranium orefield.Master Degree Thesis.Beijing:Beijing Research Institute of Uranium Geology,1-99(in Chinese with English summary)
Guo S,Ye K,Chen Y and Liu JB.2009.A normalization solution to mass transfer illustration of multiple progressively altered samples using the Isocon diagram.Economic Geology,104(6):881-886
Guo S,Ye K,Chen Y,Liu JB and Zhang LM.2013.Introduction of mass-balance calculation method for component transfer during the opening of a geological system.Acta Petrologica Sinica,29(5):1486-1498(in Chinese with English abstract)
Han YW and Ma ZD.2013.Geochemistry.Beijing:Geological Publishing House,71-80(in Chinese)
Hoefs J.1997.Stable Isotope Geochemistry.Berlin:Springer,1-201
Hu BQ,Lv GX,Sun ZX,Li MG,Shi WJ,Li XL,Wang Y and Bai LH.2011.Mineralization and fracture-water phase transition coupling in the Xiangshan uranium ore field,Jiangxi.Geotectonica et Metallogenia,35(4):502-512(in Chinese with English abstract)
Hu BQ,Wang Q,Qiu LF,Sun ZX,Wang Y,Lv GX and Hu RQ.2016.Geochemistry of alkali metasomatized rocks of Zoujiashan uranium ore-deposit in Xiangshan ore-field.Geotectonica et Metallogenia,40(2):377-385(in Chinese with English abstract)
Hu RZ and Jin JF.1988.Genesis and origin of the Guidong granitic batholith.Journal of Chengdu College of Geology,15(3):20-28(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 and Zhou MF.2012.Multiple mesozoic mineralization events in South China:An introduction to the thematic issue.Mineralium Deposita,47(6):579-588
Hu RZ,Mao JW,Hua RM and Fan WM.2015.Intra-Continental Mineralization of South China Craton.Beijing:Science Press,1-903(in Chinese)
Huang GL,Yin ZP,Ling HF,Deng P,Zhu B and Shen WZ.2010.Formation age,geochemical characteristics and genesis of pitchblende from No.302 uranium deposit in northern Guangdong.Mineral Deposits,29(2):352-360(in Chinese with English abstract)
Huang GL,Cao HJ,Ling HF,Shen WZ,Wang XD and Fu SC.2012.Zircon SHRIMP U-Pb age,geochemistry and genesis of the Youdong granite in northern Guangdong.Acta Geologica Sinica,86(4):577-586(in Chinese with English abstract)
Huang GL,Liu XY,Sun LQ,Li ZS and Zhang SJ.2014.Zircon U-Pb dating,geochemical characteristic and genesis of the Changjiang granite in northern Guangdong.Acta Geologica Sinica,88(5):836-849(in Chinese with English abstract)
Jiang YH,Jiang SY and Ling HF.2004.Mantle-derived fluids and uranium mineralization.Earth Science Frontiers,11(2):491-499(in Chinese with English abstract)
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 in Southeast China.Economic Geology,101(8):1613-1622
Jin JF and Hu RZ.1985.The genesis of uranium deposit No.302.Journal of Chengdu College of Geology,(4):1-11(in Chinese with English abstract)
Jin JF,Ni SJ and Hu RZ.1992.Vertical zoning of hydrothermal dikes in the No.302 uranium deposit and the cause of its formation.Mineral Deposits,11(3):252-258(in Chinese with English abstract)
Li HD,Pan JY,Xia F,Zhou JY,Liu Y and Zhong FJ.2016.Hydrothermal alteration and its geochemical characteristics of Lijialing deposit in Xiangshan uranium ore deposit.Geoscience,30(3):555-566(in Chinese with English abstract)
Li XH.1996.A discussion on the model and isochron ages of Sm-Nd isotopic systematics:Suitability and limitation.Scientia Geologica Sinica,31(1):97-103(in Chinese with English abstract)
Li XH,Hu RZ and Rao B.1997.Geochronology and geochemistry of Cretaceous mafic dikes from northern Guangdong,SE China.Geochimica,26(2):14-31(in Chinese with English abstract)
Ling HF.2011.Origin of hydrothermal fluids of granite-type uranium deposits:Constraints from redox conditions.Geological Review,57(2):193-206(in Chinese with English abstract)
Liu CQ,Huang ZL,Li HP and Su GL.2001.The geofluid in the mantle and its role in ore-forming processes.Earth Science Frontiers,8(4):231-243(in Chinese with English abstract)
Liu GQ,Zhao KD,Jiang SY and Wei C.2018.In-situ sulfur isotope and trace element analysis of pyrite from the Xiwang uranium ore deposit in South China:Implication for ore genesis.Journal of Geochemical Exploration,195:49-65
Liu JG,Li ZY,Huang ZZ,Li XZ and Nie JT.2017.The element mobility study of uranium mineralization alteration zones in Xiangshan,Jiangxi using the drill core CUSD3.Acta Geologica Sinica,91(4):896-912(in Chinese with English abstract)
Lu XL,Zhu MQ and Wu T.2015.Study on the stable isotope composition and hydrothermal fluids origin of uranium deposits in southern Zhuguangshan pluton.Uranium Geology,31(2):65-72(in Chinese with English abstract)
Luo Y,Wang MT,LI JH and Ma HF.2002.Geological characteristics and metallogenetic model of Zhuguang uranium ore concentrated area.China Nuclear Science and Technology Report,452-467(in Chinese with English abstract)
Mou BL.1999.Element Geochemistry.Beijing:Peking University Press,1-177(in Chinese)
Ni SJ and Jin JF.1992.The mixing and boiling of hydrothermal solution of uranium deposit No.302 and the geological interpretation.Journal of Chengdu College of Geology,(4):9-15(in Chinese with English abstract)
Ohmoto H.1986.Stable isotope geochemistry of ore deposits.Reviews in Mineralogy and Geochemistry,16(1):491-559
Qi JM,Huang GL,Zhu B,Fu SC,Xu Y and Ye SX.2014.Compositions study of auxiliary minerals in altered granitic rocks of the Mianhuakeng uranium deposit in northern Guangdong.Acta Geologica Sinica,88(9):1691-1704(in Chinese with English abstract)
Qi JM,Ye SX,Fang XQ,Cao HJ and Tang SY.2019.Study on hydrogeochemical and recharge sources characteristics of geothermal water in the Mianhuakeng uranium deposit,Renhua,northern Guangdong.Geological Review,65(1):199-210(in Chinese with English abstract)
Qu XM,Hou ZQ and Li YG.2004.Melt components derived from a subducted slab in late orogenic ore-bearing porphyries in the Gangdese copper belt,southern Tibetan Plateau.Lithos,74(3-4):131-148
Rosenbaum JM,Wilson M and Condliffe E.1997.Partial melts of subducted phosphatic sediments in the mantle.Geology,25(1):77-80
Shen WZ,Ling HF,Deng P,Zhu B,Huang GL and Tan ZZ.2010.Study on isotope geochemistry of uranium deposit 302 in northern Guangdong Province.Uranium Geology,26(2):80-87(in Chinese with English abstract)
Shu LS,Zhou XM,Deng P and Yu XQ.2006.Principal geological features of Nanling tectonic belt,South China.Geological Review,52(2):251-265(in Chinese with English abstract)
Sun LQ.2018.Petrogenesis of the Mesozoic granites in the Zhuguangshan area in the Nanling Region and their implications for the uranium mineralization.Ph.D.Dissertation.Nanjing:Nanjing University,1-192(in Chinese with English summary)
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publications,42(1):313-345
Wang CY,Li XF,Xiao R,Bai YP,Yang F,Mao W and Jiang SK.2012.Elements mobilization of mineralized porphyry rocks during hydrothermal alteration at Zhushahong porphyry copper deposit,Dexing district,South China.Acta Petrologica Sinica,28(12):3869-3886(in Chinese with English abstract)
Wang LK and Liu TG.1987.H,O,S,Pb isotopic studies of uranium ore deposits in granitoid rocks of South China.Geochimica,(1):67-78(in Chinese with English abstract)
Wang LX,Ma CQ,Lai ZX,Marks MAW,Zhang C and Zhong YF.2015.Early Jurassic mafic dykes from the Xiazhuang ore district(South China):Implications for tectonic evolution and uranium metallogenesis.Lithos,239:71-85
Wang MT,Luo Y,Sun ZF,Zhu JC and Li JH.1999.Discussion on genesis of uranium deposits in Zhuguang uranium metallogenic region.Uranium Geology,15(5):279-285(in Chinese with English abstract)
Wang ZQ and Li ZY.2007.Discussion on mantle-derived uranium mineralization.Geological Review,53(5):608-615(in Chinese with English abstract)
Wang ZQ,Fan HH,Chen DH,Zheng KZ,Luo QH,Liu JG,Wang FGand Wang YJ.2018.Geochemistry,element migration and mechanism of uranium mineralization in the periphery of the Shazijiang uranium ore deposit.Geological Journal of China Universities,24(2):185-199(in Chinese with English abstract)
Wei B.2011.Adsorption of rare earth elements La,Nd by clay minerals inorganic elements of soils.Master Degree Thesis.Hefei:Anhui Agricultural University,1-57(in Chinese with English summary)
Wei JH,Liu CQ and Ding ZJ.2000.Active laws of element migration in wall-rock alteration processes for hydrothermal gold deposits:As evidenced by Dongping,Hougou and Shuijingtun gold deposits.Acta Mineralogica Sinica,20(2):200-206(in Chinese with English abstract)
Wu DH,Pan JY,Xia F,Huang GW,Zhong FJ,Qi JY,Hong BY and Zhou TB.2018.Characteristics and formation conditions of chlorite in the Shangjiao uranium deposit in the southern Jiangxi Province,China.Acta Mineralogica Sinica,38(4):393-405(in Chinese with English abstract)
Wu DH,Pan JY,Xia F,Huang GW and Lai J.2019.The mineral chemistry of chlorites and its relationship with uranium mineralization from Huangsha uranium mining area in the middle Nanling range,SEChina.Minerals,9(3):199
Wu DH,Pan JY,Xia F,Huang GW,Zhong FJ,Lai J,Qi JM and Liu YL.2019.Characteristics and source significance of rare earth elements geochemistry of fluorite from Shangjiao uranium deposit in southern Jiangxi Province.Chinese Rare Earths,40(2):14-27(in Chinese with English abstract)
Yan DP,Zhou MF,Song HL,Wang XW and Malpas J.2003.Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block(South China).Tectonophysics,361(3-4):239-254
Yu DG.1979.Evolution of Yanshan granite and uranium mineralization enrichment:Discussion on diagenesis and mineralization relationship of some uranium-bearing rocks in South China.Uranium Geology,(4):13-25(in Chinese with English abstract)
Yu DG,Wu RG and Chen PR.2005.Uranium Geology.Harbin:Harbin Engineering University Press,1-450(in Chinese)
Zhang BL,Shan W,Li DP,Xiao BJ,Wang ZL and Zhang RZ.2017.Hydrothermal alteration in the Dayingezhuang gold deposit,Jiaodong,China.Acta Petrologica Sinica,33(7):2256-2272(in Chinese with English abstract)
Zhang BT,Dai YS,Wang NS and Liu JS.1988.Geochemical criteria for uranium metallogene-tic capacity of granitoids in South China.Chinese Journal of Nuclear Science&Engineering,8(2):153-164(in Chinese with English abstract)
Zhang GQ,Hu RZ,Bi XW,Feng HS,Shang PQ and Tian JJ.2007.REE geochemical characteristics of the No.302 uranium deposit in northern Guangdong,South China.Chinese Journal of Geochemistry,26(4):425-433
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 urnaium deposit.Acta mineralogica Sinica,28(4):413-420(in Chinese with English abstract)
Zhang GQ,Hu RZ,Jiang GH,Liu S,Zhu WG,Tian JJ,Shuang Y and Fan XR.2010.Mantle derived volatile components involved in uranium mineralization:Evidence from He isotopes of the No.302uranium deposit.Geochimica,39(4):386-395(in Chinese with English abstract)
Zhang KQ and Yang Y.2002.Introduction of the method for mass balance calculation in altered rocks.Geological Science and Technology Information,21(3):104-107(in Chinese with English abstract)
Zhang L,Chen ZY,Li SR,Santosh M,Huang GL and Tian ZJ.2017.Isotope geochronology,geochemistry,and mineral chemistry of the U-bearing and barren granites from the Zhuguangshan complex,South China:Implications for petrogenesis and uranium mineralization.Ore Geology Reviews,91:1040-1065
Zhang L,Chen ZY,Li SR and Huang GL.2018.Characteristics of uranium minerals in wall rock alteration zones of the Mianhuakeng(No.302)uranium deposit,northern Guangdong,South China.Acta Petrologica Sinica,34(9):2657-2670(in Chinese with English abstract)
Zhang M,Chen PR,Huang GL and Ling HF.2006.The research on the geochemical characteristics of Longyuanba composite pluton in Nanling region.Uranium Geology,22(6):336-344(in Chinese with English abstract)
Zhang YC.2002.Alkalic mantle fluids and uranium ore-formation in Zhuguang and Guidong granitic massifs.Uranium Geology,18(4):210-219(in Chinese with English abstract)
Zhang ZH and Zhang BT.1991.On the Uranium-Bearing Granites and Their Related Uranium Deposits in South China.Beijing:Atomic Energy Press,13-15(in Chinese)
Zhao ZF,Zheng YF,Wei CS and Gong B.2001.Carbon concentration and isotope composition of granites from Southeast China.Physics and Chemistry of the Earth,Part A:Solid Earth&Geodesy,26(9-10):821-833
Zhao ZH.1992.Geochemical characteristics of trace elements.Advances in Earth Science,7(5):65-66(in Chinese with English abstract)
Zhong FJ.2018.Petrogenesis and mineralization of granite type uranium deposits in South China:A case study of the Changjiang uranium ore field in northern Guangdong Province.Ph.D.Dissertation.Nanchang:East China University of Technology,1-226(in Chinese with English summary)
Zhong FJ,Pan JY,Qi JM,Yan J,Liu WQ and Li HD.2018.New insitu La-ICP-MS U-Pb ages of uraninite from the Mianhuakeng uranium deposit,northern Guangdong Province,China:Constraint on the metallogenic mechanism.Acta Geologica Sinica,92(2):852-854
Zhong J,Fan HH,Gu DZ,Wang SY,Chen JY,Shi CH and Li HQ.2016.Major and trace element migration and metallogenic processes of the Xinshuijing U-Th deposit in the Longshoushan metallogenic belt,Gansu Province.Geology in China,43(4):1393-1408(in Chinese with English abstract)
Zhong J,Chen YJ and Pirajno F.2017.Geology,geochemistry and tectonic settings of the molybdenum deposits in South China:Areview.Ore Geology Reviews,81:829-855
陈言飞，王玉往，王京彬，王莉娟，唐萍芝，石煜，赵路通．2018．与A型花岗岩有关锡矿的云英岩化蚀变矿化地球化学:以新疆卡姆斯特和干梁子矿床为例．地球科学，43(9):3154-3168
陈振宇，黄国龙，朱捌，陈郑辉，黄凡，赵正，田泽瑾．2014．南岭地区花岗岩型铀矿的特征及其成矿专属性．大地构造与成矿学，38(2):264-275
邓海琳，涂光炽，李朝阳，刘丛强．1999．地球化学开放系统的质量平衡:1．理论．矿物学报，19(2):121-131
邓平，舒良树，谭正中．2003．诸广-贵东大型铀矿聚集区富铀矿成矿地质条件．地质论评，49(5):486-494
傅丽雯．2015．粤北302铀矿床围岩蚀变分带、成矿流体与成矿物质来源研究．硕士学位论文．南京:南京大学，1-67
高飞，林锦荣，钟启龙，郭树英，庞雅庆，戎家树，胡志华．2011.302铀矿床围岩蚀变分带性及地球化学特征．铀矿地质，27(5):274-281
高山，骆庭川，张本仁，张宏飞，韩吟文，赵志丹，Kern H.1999．中国东部地壳的结构和组成．中国科学(D辑)，29(3):204-213
高翔，沈渭洲，刘莉莉，姚薇，朱捌，黄国龙，李秋英．2011．粤北302铀矿床围岩蚀变的地球化学特征和成因研究．岩石矿物学杂志，30(1):71-82
郭建．2014．相山铀矿田科学深钻岩石铀矿化蚀变作用研究．硕士学位论文．北京:核工业北京地质研究院，1-99
郭顺，叶凯，陈意，刘景波，张灵敏．2013．开放地质体系中物质迁移质量平衡计算方法介绍．岩石学报，29(5):1486-1498
韩吟文，马振东．2003．地球化学．北京:地质出版社，71-80
胡宝群，吕古贤，孙占学，李满根，史维浚，李学礼，王运，白丽红．2011．江西相山铀矿田中断裂与水相变耦合成矿---以邹家山矿床铀成矿作用分析为例．大地构造与成矿学，35(4):502-512
胡宝群，王倩，邱林飞，孙占学，王运，吕古贤，胡荣泉．2016．相山矿田邹家山铀矿床碱交代矿化蚀变岩地球化学．大地构造与成矿学，40(2):377-385
胡瑞忠，金景福．1988．论贵东花岗岩体的成因及其起源．成都地质学院学报，15(3):20-28
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
黄国龙，尹征平，凌洪飞，邓平，朱捌，沈渭洲．2010．粤北地区302矿床沥青铀矿的形成时代、地球化学特征及其成因研究．矿床地质，29(2):352-360
黄国龙，曹豪杰，凌洪飞，沈渭洲，王小冬，伏顺成．2012．粤北油洞岩体SHRIMP锆石U-Pb年龄、地球化学特征及其成因研究．地质学报，86(4):577-586
黄国龙，刘鑫扬，孙立强，李钟枢，张世佳．2014．粤北长江岩体的锆石U-Pb定年、地球化学特征及其成因研究．地质学报，88(5):836-849
姜耀辉，蒋少涌，凌洪飞．2004．地幔流体与铀成矿作用．地学前缘，11(2):491-499
金景福，胡瑞忠．1985.302矿床成因探讨．成都地质学院学报，(4):1-11
金景福，倪师军，胡瑞忠．1992.302铀矿床热液脉体的垂直分带及其成因探讨．矿床地质，11(3):252-258
李海东，潘家永，夏菲，周加云，刘颖，钟福军．2016．相山李家岭铀矿床热液蚀变作用地球化学特征．现代地质，30(3):555-566
李献华．1996.Sm-Nd模式年龄和等时线年龄的适用性与局限性．地质科学，31(1):97-103
李献华，胡瑞忠，饶冰．1997．粤北白垩纪基性岩脉的年代学和地球化学．地球化学，26(2):14-31
凌洪飞．2011．论花岗岩型铀矿床热液来源---来自氧逸度条件的制约．地质论评，57(2):193-206
刘丛强，黄智龙，李和平，苏根利．2001．地幔流体及其成矿作用．地学前缘，8(4):231-243
刘军港，李子颖，黄志章，李秀珍，聂江涛．2017．江西相山CUSD3钻孔铀矿化蚀变带元素活动性探讨．地质学报，91(4):896-912
卢小亮，祝民强，邬铁．2015．诸广岩体南部铀矿区稳定同位素组成及矿床成因分析．铀矿地质，31(2):65-72
罗毅，王明太，李建红，马汉峰．2002．诸广铀矿集区成矿地质特征及成矿模式．中国核科技报告，452-467
牟保磊．1999．元素地球化学．北京大学出版社，1-177
倪师军，金景福．1992.302铀矿床热液的混合和沸腾及其地质意义．成都地质学院学报，(4):9-15
祁家明，黄国龙，朱捌，伏顺成，许幼，叶松鑫．2014．粤北棉花坑铀矿床蚀变花岗岩副矿物特征研究．地质学报，88(9):1691-1704
祁家明，叶松鑫，方晓骐，曹豪杰，唐仕尧．2019．粤北仁化棉花坑铀矿床地下热水地球化学特征及补给来源研究．地质论评，65(1):199-210
沈渭洲，凌洪飞，邓平，朱捌，黄国龙，谭正中．2010．粤北302铀矿床同位素地球化学研究．铀矿地质，26(2):80-87
舒良树，周新民，邓平，余心起．2006．南岭构造带的基本地质特征．地质论评，52(2):251-265
孙立强．2018．南岭诸广山地区中生代花岗岩成因及其对铀成矿作用的启示．博士学位论文．南京:南京大学，1-192
王翠云，李晓峰，肖荣，白艳萍，杨锋，毛伟，蒋松坤．2012．德兴朱砂红斑岩铜矿热液蚀变作用及元素地球化学迁移规律．岩石学报，28(12):3869-3886
王联魁，刘铁庚．1987．华南花岗岩铀矿H、O、S、Pb同位素研究．地球化学，(1):67-78
王明太，罗毅，孙志富，朱杰辰，李建红．1999．诸广铀成矿区矿床成因探讨．铀矿地质，15(5):279-285
王正其，李子颖．2007．幔源铀成矿作用探讨．地质论评，53(5):608-615
王正庆，范洪海，陈东欢，郑可志，罗桥花，刘军港，王凤岗，王勇剑．2018．沙子江铀矿外围地化特征、元素迁移及铀成矿机理．高校地质学报，24(2):185-199
魏斌．2011．粘土矿物及土壤无机相对稀土元素La、Nd的吸附性研究．硕士学位论文．合肥:安徽农业大学，1-57
魏俊浩，刘丛强，丁振举．2000．热液型金矿床围岩蚀变过程中元素迁移规律---以张家口地区东坪、后沟、水晶屯金矿为例．矿物学报，20(2):200-206
吴德海，潘家永，夏菲，黄广文，钟福军，祁家明，洪斌跃，周堂波．2018．赣南上窖铀矿床绿泥石特征与形成环境．矿物学报，38(4):393-405
吴德海，潘家永，夏菲，黄广文，钟福军，赖静，祁家明，刘院龙．2019．赣南上窖铀矿床萤石稀土元素地球化学特征及其源区意义．稀土，40(2):14-27
余达淦．1979．燕山花岗岩演化与铀矿化富集---对华南一些含铀岩体成岩成矿关系探讨．铀矿地质，(4):13-25
余达淦，吴仁贵，陈培荣．2005．铀资源地质学．哈尔滨:哈尔滨工程大学出版社，1-450
张炳林，单伟，李大鹏，肖丙建，王中亮，张瑞忠．2017．胶东大尹格庄金矿床热液蚀变作用．岩石学报，33(7):2256-2272
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
张国全，胡瑞忠，蒋国豪，刘燊，朱维光，田建吉，双燕，范效仁．2010．幔源挥发性组分参与302铀矿床成矿作用的氦同位素证据．地球化学，39(4):386-395
张可清，杨勇．2002．蚀变岩质量平衡计算方法介绍．地质科技情报，21(3):104-107
张龙，陈振宇，李胜荣，黄国龙．2018．粤北棉花坑(302)铀矿床围岩蚀变分带的铀矿物研究．岩石学报，34(9):2657-2670
张敏，陈培荣，黄国龙，凌洪飞．2006．南岭龙源坝复式岩体的地球化学特征研究．铀矿地质，22(6):336-344
张彦春．2002．诸广、贵东花岗岩中碱性地幔流体与铀成矿．铀矿地质，18(4):210-219
张祖还，章邦桐．1991．华南产铀花岗岩及有关铀矿床研究．北京:原子能出版社，13-15
章邦桐，戴永善，王年生，刘继顺．1988．华南花岗岩铀成矿能力的地球化学判别标志．核科学与工程，8(2):153-164
赵振华．1992．微量元素地球化学．地球科学进展，7(5):65-66
钟福军．2018．华南花岗岩型铀矿成岩成矿作用研究---以粤北长江铀矿田为例．博士学位论文．南昌:东华理工大学，1-226
钟军，范洪海，顾大钊，王生云，陈金勇，史长昊，李恒强．2016．甘肃龙首山成矿带新水井铀(钍)矿床元素迁移规律及成矿作用过程研究．中国地质，43(4):1393-1408
(1)中国核工业地质局《华南铀矿地质志》编写组．2005．华南铀矿地质志．中国核工业地质局内部资料
© 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 |