必须声明标量变量 "@Script_ID"。 江西相山矿田邹家山铀矿床特富矿石流体包裹体特征:来自共生磷灰石-紫黑色细晶萤石等矿物制约-《地球科学与环境学报》
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[1]郭晶晶,邱林飞,胡宝群*,等.江西相山矿田邹家山铀矿床特富矿石流体包裹体特征:来自共生磷灰石-紫黑色细晶萤石等矿物制约[J].地球科学与环境学报,2020,42(04):526-539.[doi:10.19814/j.jese.2020.04023]
 GUO Jing-jing,QIU Lin-fei,HU Bao-qun*,et al.Characteristics of Fluid Inclusions of the Ultra-rich Ore from Zoujiashan Uranium Deposit in Xiangshan Orefield of Jiangxi, China: Insights from Paragenesis Apatite-purple Black Fine Crystal Fluorite and Other Minerals[J].Journal of Earth Sciences and Environment,2020,42(04):526-539.[doi:10.19814/j.jese.2020.04023]
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江西相山矿田邹家山铀矿床特富矿石流体包裹体特征:来自共生磷灰石-紫黑色细晶萤石等矿物制约(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第42卷
期数:
2020年第04期
页码:
526-539
栏目:
基础地质与矿产地质
出版日期:
2020-07-15

文章信息/Info

Title:
Characteristics of Fluid Inclusions of the Ultra-rich Ore from Zoujiashan Uranium Deposit in Xiangshan Orefield of Jiangxi, China: Insights from Paragenesis Apatite-purple Black Fine Crystal Fluorite and Other Minerals
文章编号:
1672-6561(2020)04-0526-14
作者:
郭晶晶1邱林飞2胡宝群1*高海东1王运1薛栋1
(1. 东华理工大学 地球科学学院,江西 南昌 330013; 2. 核工业北京地质研究院,北京 100029)
Author(s):
GUO Jing-jing1 QIU Lin-fei2 HU Bao-qun1* GAO Hai-dong1 WANG Yun1 XUE Dong1
(1. School of Earth Sciences, East China University of Technology, Nanchang 330013, Jiangxi, China; 2. Beijing Research Institute of Uranium Geology, Beijing 100029, China)
关键词:
铀矿床 流体包裹体 磷灰石 紫黑色细晶萤石 均一温度 盐度 激光拉曼光谱 江西
Keywords:
uranium deposit fluid inclusion apatite purple black fine crystal fluorite homogenization temperature salinity laser Raman spectrum Jiangxi
分类号:
P619.14
DOI:
10.19814/j.jese.2020.04023
文献标志码:
A
摘要:
在相山矿田成矿流体研究中,前人一般选择成矿晚期结晶良好、透明度高的脉石矿物中的流体包裹体进行研究,其结果难以准确反映成矿流体的信息。基于此,选择江西相山矿田邹家山铀矿床特富矿石中与铀矿物紧密共生的磷灰石及其伴生微细晶透明矿物作为研究对象,通过岩相学观察、扫描电镜能谱分析及流体包裹体研究,讨论该矿床的成矿流体性质,以期为成矿流体来源的判断与成矿过程的研究提供新资料。结果表明:特富铀矿石中与铀矿物密切共生的磷灰石可分为两类。一类为含黑色矿物包裹体的微晶磷灰石(Ap1型),晶形较差,形状不规则,透明度较差,粒度小,推测为主成矿阶段产物,与之共生的主要有微晶石英和紫黑色细晶萤石,同属主成矿阶段产物; 另一类为中粗晶磷灰石(Ap2型),自形程度高,形状规则,部分呈六方柱形,粒度大,推测为成矿晚阶段产物。主成矿阶段,紫黑色细晶萤石中流体包裹体气体成分主要为H2,微晶石英中流体包裹体气体成分主要为O2和CO2,指示了成矿流体中的气体组分以H2、O2为主,可能含有少量的CO2,说明成矿流体具有富H2的深源流体加入。主成矿阶段流体包裹体均一温度为270 ℃~330 ℃,盐度为5%~9% NaCleq,成矿晚阶段流体包裹体均一温度为180 ℃~220 ℃,盐度为4%~10% NaCleq,成矿温度最低为180 ℃。特富铀矿石中成矿期磷灰石及其共生脉石矿物中流体包裹体组合特征较好地指示了铀主成矿阶段的流体性质。
Abstract:
Xiangshan uranium orefield in Jiangxi is always the focus of scholars. Most of them chose fluid inclusions in gangue minerals with good crystallization and high transparency for research. These gangue minerals are generally the products of crystallization in the late or post mineralization period, and the results are difficult to accurately reflect the information of ore-forming fluids. In view of this, the apatite and its associated fine crystal transparent mineral, which are closely associated with uranium minerals of the ultra-rich ore in Zoujiashan uranium deposit, were studied by petrographic observation, SEM-EDS analysis and fluid inclusions determining. Ore-forming fluid properties of the deposit were discussed in order to provide new information for the determination of ore-forming fluid source and the study of ore-forming process. The results show that there are two types of apatites closely associated with uranium minerals in ultra-rich uranium ore. One is microcrystalline apatite(Ap1)with inclusions of black minerals, which has poor crystal shape, irregular shape, poor transparency and small particle size, and it should be formed in main ore-forming stage. Microcrystalline quartz and purple black fine crystal fluorite are associated with microcrystalline apatite, and both are formed in main ore-forming stage. The another one is medium coarse crystalline apatite(Ap2), which has high degree of automorphism, regular shape, hexagonal column shape and large particle size, and it should be formed in late ore-forming stage. In main ore-forming stage, the gas composition of fluid inclusions in the purple black fine crystal fluorite is mainly H2, and that of fluid inclusions in microcrystalline quartz is mainly O2 and CO2. It shows that the gas composition of the ore-forming fluids is mainly H2 and O2, and a small amount of CO2, indicating that the ore-forming fluids have the addition of deep source fluid rich in H2. The homogenization temperature of fluid inclusions is concentrated in 270 ℃-330 ℃, and the salinity is 5%-9% NaCleq in main ore-forming stage. The homogenization temperature of fluid inclusions is concentrated in 180 ℃-220 ℃, the salinity is 4%-10% NaCleq in late ore-forming stage, and the lowest mineralization temperature is above 180 ℃. The characteristics of fluid inclusion assemblage in apatite and its associated gangue minerals in the metallogenic stage of ultra-rich uranium ore indicate the fluid properties in the main ore-forming stage of uranium.

参考文献/References:

[1] 刘 斌,陈卫锋,方启春,等.相山铀矿田成矿流体特征:来自微量、稀土元素地球化学证据[J].岩石学报,2019,35(9):2774-2786.
LIU Bin,CHEN Wei-feng,FANG Qi-chun,et al.Characteristics of Ore-forming Fluids in the Xiangshan Uranium Ore-field:Constraints from Trace Elements and Rare Earth Elements[J].Acta Petrologica Sinica,2019,35(9):2774-2786.
[2] 王 健,聂江涛,郭 建.江西相山矿田铜矿化特征及成矿流体演化[J].矿物岩石,2015,35(4):74-84.
WANG Jian,NIE Jiang-tao,GUO Jian.Charateristic of Copper Mineralization and Ore-forming Fluid Evolution in Xiangshan Ore Field,Jiangxi Province[J].Journal of Mineralogy and Petrology,2015,35(4):74-84.
[3] 邵 飞,徐恒力,邹茂卿.相山铀矿田火山岩浆期后成矿热液系统[J].铀矿地质,2009,25(3):137-143,183.
SHAO Fei,XU Heng-li,ZOU Mao-qing.Metallogenic Hydrothermal Solution System of Post Volcanic Magma in Xiangshan Ore Field[J].Uranium Geology,2009,25(3):137-143,183.
[4] 刘军港,李子颖,聂江涛,等.江西相山铀矿田深部多金属矿化成矿流体来源:流体包裹体He-Ar同位素证据[J].大地构造与成矿学,2019,43(2):271-282.
LIU Jun-gang,LI Zi-ying,NIE Jiang-tao,et al.Origin of Ore-forming Fluids in the Deep Polymetallic Mine-ralization in Western Xiangshan Uranium Ore Field,Jiangxi Province,China:Constraints from He-Ar Isotopes[J].Geotectonica et Metallogenia,2019,43(2):271-282.
[5] 刘军港,李子颖,聂江涛,等.相山铀矿田西部地区深部多金属矿化成矿年代与成矿流体演化:Rb-Sr同位素体系的制约[J].岩石学报,2019,35(9):2787-2800.
LIU Jun-gang,LI Zi-ying,NIE Jiang-tao,et al.The Timing and Ore-forming Fluid Evolution of Deep Polymetalic Mineralization in Western Xiangshan Uranium Ore Field,South China:Constraints from Rb-Sr Isotope Systematics[J].Acta Petrologica Sinica,2019,35(9):2787-2800.
[6] 聂江涛,李子颖,王 健,等.相山铀矿田铅锌矿化同位素特征及成矿物质来源探讨[J].铀矿地质,2018,34(6):353-359.
NIE Jiang-tao,LI Zi-ying,WANG Jian,et al.Isotopic Feature and Provenance of Lead-zinc Mineralization Ores of the Scientific Drilling in Xiangshan Ore Field[J].Uranium Geology,2018,34(6):353-359.
[7] 张万良,李子颖.江西邹家山铀矿床成矿特征及物质来源[J].现代地质,2005,19(3):369-374.
ZHANG Wan-liang,LI Zi-ying.Metallogenic Characteristics and Material Source of Zoujiashan Uranium Deposit,Jiangxi Province[J].Geoscience,2005,19(3):369-374.
[8] 范洪海,凌洪飞,王德滋,等.江西相山铀矿田成矿物质来源的Nd、Sr、Pb同位素证据[J].高校地质学报,2001,7(2):139-145.
FAN Hong-hai,LING Hong-fei,WANG De-zi,et al.Ore-forming Material Sources for Xiangshan Uranium Ore-field in Jiangxi Province:Evidence from Nd-Sr-Pb Isotopes[J].Geological Journal of China Universities,2001,7(2):139-145.
[9] 邵 飞,陈晓明,徐恒力,等.相山铀矿田成矿物质来源探讨[J].东华理工大学学报(自然科学版),2008,31(1):39-44,80.
SHAO Fei,CHEN Xiao-ming,XU Heng-li,et al.Discussion of Metallogenic Substance Source of Xiangshan Uranium Orefield[J].Journal of East China Institute of Technology(Natural Science),2008,31(1):39-44,80.
[10] 孙占学.相山铀矿田铀源的地球化学证据[J].矿物学报,2004,24(1):19-24.
SUN Zhan-xue.Uranium Sources of the Xiangshan Uranium Ore-field:Geochemical Evidence[J].Acta Mine-ralogica Sinica,2004,24(1):19-24.
[11] 张万良,余西垂.相山铀矿田成矿综合模式研究[J].大地构造与成矿学,2011,35(2):249-258.
ZHANG Wan-liang,YU Xi-chui.A Study of Integrated Metallogenic Model for the Xiangshan Uranium Field[J].Geotectonica et Metallogenia,2011,35(2):249-258.
[12] 邵 飞,陈晓明,徐恒力,等.江西省相山铀矿田成矿模式探讨[J].地质力学学报,2008,14(1):65-73.
SHAO Fei,CHEN Xiao-ming,XU Heng-li,et al.Metallogenic Model of the Xiangshan Uranium Ore Field,Jiangxi Province[J].Journal of Geomechanics,2008,14(1):65-73.
[13] BONNETTI C,LIU X D,CUNEY M,et al.Evolution of the Uranium Mineralisation in the Zoujiashan Deposit,Xiangshan Ore Field:Implications for the Genesis of Volcanic-related Hydrothermal U Deposits in South China[J].Ore Geology Reviews,2020,122:103514.
[14] 陈正乐,王平安,王 永,等.江西相山铀矿田山南矿区控矿构造解析与找矿预测[J].地球科学与环境学报,2013,35(2):8-18.
CHEN Zheng-le,WANG Ping-an,WANG Yong,et al.Ore-controlling Tectonic Analysis and Ore-prospecting in Shannan Mining Area of Xiangshan Uranium Ore-field,Jiangxi[J].Journal of Earth Sciences and Environment,2013,35(2):8-18.
[15] 杨庆坤,郭福生,周万蓬,等.江西相山矿田铀铅锌多金属年代学特征及成矿模式[J].地学前缘,2017,24(5):283-298.
YANG Qing-kun,GUO Fu-sheng,ZHOU Wan-peng,et al.Geochronology and Metallogenic Model of the Xiangshan U-Pb-Zn Deposits,Southern Jiangxi,China[J].Earth Science Frontiers,2017,24(5):283-298.
[16] 邱林飞,欧光习,罗一鹏,等.相山铀矿田成矿流体研究现状及存在问题[J].铀矿地质,2017,33(3):150-155.
QIU Lin-fei,OU Guang-xi,LUO Yi-peng,et al.Ana-lysis on the Situation and Problems of Uranium Ore-forming Fluid Research in Xiangshan Ore Field[J].Uranium Geology,2017,33(3):150-155.
[17] 王 蕾,张树明,蒋振频,等.相山铀矿田沙洲矿床流体包裹体研究[J].大地构造与成矿学,2008,32(4):500-508.
WANG Lei,ZHANG Shu-ming,JIANG Zhen-pin,et al.The Study of Fluid Inclusion of Shazhou Deposit in Xiangshan Uranium Ore-field[J].Geotectonica et Metallogenia,2008,32(4):500-508.
[18] 黄锡强,陈正乐,王平安,等.江西相山铀矿田沙洲矿床流体包裹体研究[J].地质力学学报,2008,14(2):176-185.
HUANG Xi-qiang,CHEN Zheng-le,WANG Ping-an,et al.Fluid Inclusion Study of the Shazhou Uranium Orefield in the Xiangshan Deposit,Jiangxi[J].Journal of Geomechanics,2008,14(2):176-185.
[19] 张树明,王 蕾,蒋振频,等.邹家山铀矿床流体包裹体研究[J].铀矿地质,2009,25(5):263-269.
ZHANG Shu-ming,WANG Lei,JIANG Zhen-pin,et al.Fluid Inclusion Study of Zoujiashan Deposit in Xiangshan Uranium Ore-field[J].Uranium Geology,2009,25(5):263-269.
[20] 白丹丹,胡宝群,孙占学,等.相山铀矿田邹家山矿床流体包裹体研究[J].铀矿地质,2012,28(5):290-296.
BAI Dan-dan,HU Bao-qun,SUN Zhan-xue,et al.Discussion on the Physicochemical Conditions of Uranium Mineralization of Zoujiashan Deposit in Xiangshan Orefield[J].Uranium Geology,2012,28(5):290-296.
[21] 邱林飞,吴 迪,吴 玉,等.相山牛头山地区铀矿床深部多金属成矿流体特征与成矿物质来源探讨[J].矿床地质,2019,38(2):291-302.
QIU Lin-fei,WU Di,WU Yu,et al.Characteristics of Ore-forming Fluids and Sources of Polymetallic Ore-forming Materials in Deep Segment of Uranium Deposits in Niutoushan Area,Xiangshan[J].Mineral Deposits,2019,38(2):291-302.
[22] 郭 建,李子颖,李秀珍,等.相山铀矿田邹家山矿床成矿流体特征[J].铀矿地质,2014,30(5):263-270.
GUO Jian,LI Zi-ying,LI Xiu-zhen,et al.Mineralization Fluid Features of Zoujiashan Uranium Deposit in Xiangshan Ore-field,Jiangxi[J].Uranium Geology,2014,30(5):263-270.
[23] KETTERER M E,WETZEL W C,LAYMAN R R,et al.Isotopic Studies of Sources of Uranium in Sediments of the Ashtabula River,Ohio,USA[J].Environmental Science and Technology,2000,34(6):966-972.
[24] KUMAR T B P,TIWARY A,FAHMI S.Nature of Uranium Mineralization in the Kerpura-Tiwari-Ka-Bas Area,Sikar District,Rajasthan[J].Journal of the Geological Society of India,2009,73(2):220-228.
[25] 胡宝群,邱林飞,李满根,等.江西相山铀矿田构造-岩浆演化及其成矿规律[J].地学前缘,2015,22(4):29-36.
HU Bao-qun,QIU Lin-fei,LI Man-gen,et al.The Tectono-magmatic Evolution and Metallogenic Regularity of Xiangshan Uranium Ore-field in Jiangxi Province[J].Earth Science Frontiers,2015,22(4):29-36.
[26] 王 倩,胡宝群,宋金如,等.磷灰石吸附铀试验及其铀成矿意义:以江西相山矿田为例[J].地球科学与环境学报,2016,38(6):813-821.
WANG Qian,HU Bao-qun,SONG Jin-ru,et al.Experiment on Apatite Adsorbing Uranium and Its Implication on Uranium Mineralization:Taking Xiangshan Orefield in Jiangxi as an Example[J].Journal of Earth Sciences and Environment,2016,38(6):813-821.
[27] 王 运.江西邹家山铀矿床重稀土赋存特征及富集机制研究[D].成都:成都理工大学,2018.
WANG Yun.Study of Occurrence Characteristics and Enrichment Mechanism of HREE in Zoujiashan Uranium Deposit,Jiangxi Province[D].Chengdu:Chengdu University of Technology,2018.
[28] YU Z Q,LING H F,MAVROGENES J,et al.Metallogeny of the Zoujiashan Uranium Deposit in the Meso-zoic Xiangshan Volcanic-intrusive Complex,Southeast China:Insights from Chemical Compositions of Hydrothermal Apatite and Metal Elements of Individual Fluid Inclusions[J].Ore Geology Reviews,2019,113:103085.
[29] PAL D C,BHOWMICK T.Petrography and Microthermometry of Fluid Inclusions in Apatite in the Turamdih Uranium Deposit,Singhbhum Shear Zone,Eastern India:An Insight into Ore Forming Fluid[J].Journal of the Geological Society of India,2015,86(3):253-262.
[30] PATINO DOUCE A E,RODEN M F,CHAUMBA J,et al.Compositional Variability of Terrestrial Mantle Apatites,Thermodynamic Modeling of Apatite Volatile Contents,and the Halogen and Water Budgets of Planetary Mantles[J].Chemical Geology,2011,288(1/2):14-31.
[31] 温志坚,杜乐天,刘正义.相山铀矿田磷灰石与富矿形成的关系[J].铀矿地质,1999,15(4):217.
WEN Zhi-jian,DU Le-tian,LIU Zheng-yi.Relation Between Francolite and Metallogenesis of High-grade Uranium Ores in Xiangshan Uranium Orefield[J].Uranium Geology,1999,15(4):217.
[32] 胡宝群,王 倩,邱林飞,等.相山矿田邹家山铀矿床碱交代矿化蚀变岩地球化学[J].大地构造与成矿学,2016,40(2):377-385.
HU Bao-qun,WANG Qian,QIU Lin-fei,et al.Geochemistry of Alkali Metasomatized Rocks of Zoujia-shan Uranium Ore-deposit in Xiangshan Ore-field[J].Geotectonica et Metallogenia,2016,40(2):377-385.
[33] 姚宏鑫,吕古贤,聂江涛,等.江西相山铀矿田邹家山铀矿床蚀变特征及热液来源[J].现代地质,2013,27(2):332-338.
YAO Hong-xin,LV Gu-xian,NIE Jiang-tao,et al.Characteristics of Mineralizing Alteration and Hydrothermal Sources in Zoujiashan Uranium Deposits in Xiangshan Uranium Ore Field in Jiangxi Province[J].Geoscience,2013,27(2):332-338.
[34] 杨水源,蒋少涌,赵葵东,等.江西相山铀矿田邹家山矿床中流纹斑岩的锆石U-Pb年代学、岩石地球化学与Sr-Nd-Hf同位素组成[J].岩石学报,2012,28(12):3915-3928.
YANG Shui-yuan,JIANG Shao-yong,ZHAO Kui-dong,et al.Zircon U-Pb Geochronology,Geochemistry and Sr-Nd-Hf Isotopic Compositions of the Rhyolite Porphyry from the Zhoujiaoshan Deposit in Xiangshan Uranium Ore Field,Jiangxi Province,SE China[J].Acta Petrologica Sinica,2012,28(12):3915-3928.
[35] 王 运,胡宝群,孙占学,等.相山铀矿田邹家山矿床碱交代型矿石地球化学特征及其成矿意义[J].铀矿地质,2012,28(5):281-289.
WANG Yun,HU Bao-qun,SUN Zhan-xue,et al.The Geochemical Characteristics of Alkali Metasomatic Ore and Its Ore-forming Significance at Zoujiashan Deposit,Xiangshan Uranium Field[J].Uranium Geology,2012,28(5):281-289.
[36] 黄 振,胡宝群,王 运,等.相山矿田邹家山铀矿床围岩蚀变地球化学特征[J].东华理工大学学报(自然科学版),2014(37):129-135.
HUANG Zhen,HU Bao-qun,WANG Yun,et al.Wall Rock Alteration and Its Geochemical Characteristics of Zoujiashan Deposit in Xiangshan Uranium Ore-field[J].Journal of East China Institute of Technology(Natural Science Edition),2014(37):129-135.
[37] 汤国平,庞文静,张运涛,等.相山火山盆地邹家山铀矿床温热水分布特征及其找矿意义[J].铀矿地质,2020,36(2):123-130.
TANG Guo-ping,PANG Wen-jing,ZHANG Yun-tao,et al.Distribution Pattern and Prospecting Significance of Thermal Water of Zoujiashan Deposit in Xiangshan Volcanic Basin[J].Uranium Geology,2020,36(2):123-130.
[38] 林锦荣,胡志华,陶 意,等.相山矿田邹家山铀矿床成矿热事件的锆石裂变径迹年龄响应[J].铀矿地质,2019,35(4):193-198.
LIN Jin-rong,HU Zhi-hua,TAO Yi,et al.The Response of Zircon Fission Track Age on the Metallogenic Thermal Events of Zoujiashan Uranium Deposit in Xiangshan Orefield[J].Uranium Geology,2019,35(4):193-198.
[39] 胡宝群,吕古贤,孙占学,等.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[J].大地构造与成矿学,2011,35(4):502-512.
HU Bao-qun,LV Gu-xian,SUN Zhan-xue,et al.Mine-ralization and Fracture-water Phase Transition Coupling in the Xiangshan Uranium Ore Field,Jiangxi:A Case Study of Uranium Mineralization in Zoujiashan Deposit[J].Geotectonica et Metallogenia,2011,35(4):502-512.
[40] 张树明,曹寿孙,曾文乐,等.江西相山矿田典型铀矿床流体包裹体特征及意义[J].矿床地质,2012,31(1):65-82.
ZHANG Shu-ming,CAO Shou-sun,ZENG Wen-le,et al.Fluid Inclusion Characteristics of Typical Uranium Deposits in Xiangshan Orefield,Jiangxi Province[J].Mineral Deposits,2012,31(1):65-82.
[41] 邱林飞,欧光习,张 敏,等.相山居隆庵矿床铀成矿流体特征及其来源探讨[J].矿床地质,2012,31(2):271-281.
QIU Lin-fei,OU Guang-xi,ZHANG Min,et al.Cha-racteristics and Origin of Ore-forming Fluid of Julong'an Uranium Deposit in Xiangshan Uranium Orefield[J].Mineral Deposits,2012,31(2):271-281.
[42] BODNAR R J.Revised Equation and Table for Determining the Freezing Point Depression of H2O-NaCl Solutions[J].Geochimica et Cosmochimica Acta,1993,57(3):683-684.
[43] 范洪海.江西相山壳源型火山-侵入杂岩及其深部成矿作用[D].南京:南京大学,2001.
FAN Hong-hai.Volcanic-intrusive Complex of Crust Type and Deep Mineralization in Xiangshan,Jiangxi Province[D].Nanjing:Nanjing University,2001.
[44] 王 运,胡宝群,孙占学,等.相山铀矿田邹家山矿床钛铀矿赋存特征及成因[J].铀矿地质,2010,26(6):344-349.
WANG Yun,HU Bao-qun,SUN Zhan-xue,et al.Occurring Characteristic and Genesis of Brannerite at Zou-jiashan Uranium Deposits,Xiangshan Ore Field[J].Uranium Geology,2010,26(6):344-349.
[45] 胡志华,林锦荣,王勇剑,等.相山矿田邹家山铀矿床钛铀矿地球化学特征及其成矿意义探讨[J].世界核地质科学,2018,35(2):63-70.
HU Zhi-hua,LIN Jin-rong,WANG Yong-jian,et al.Discussion on Geochemical Characteristics of the Brannerite and Its Metallogenic Significance in Zoujiashan Uranium Deposit,Xiangshan Ore Field[J].World Nuclear Geoscience,2018,35(2):63-70.
[46] 郭 建,李子颖,黄志章,等.相山铀矿田邹家山矿床成矿流体氢氧同位素地球化学特征[J].地质学报,2015,89(增1):99-100.
GUO Jian,LI Zi-ying,HUANG Zhi-zhang,et al.Hydrogen and Oxygen Isotopic Geochemical Characteristics of Ore-forming Fluid in Zoujiashan Deposit in Xiangshan Uranium Ore-field[J].Acta Geologica Sinica,2015,89(S1):99-100.
[47] 孙占学,李学礼,史维浚,等.华东南相山铀矿田的氢氧同位素地球化学研究[J].地质与勘探,2001,37(3):20-23.
SUN Zhan-xue,LI Xue-li,SHI Wei-jun,et al.Isotope Geochemistry of Oxygen and Hydrogen of the Xiangshan Uranium Ore-field,SE China[J].Geology and Prospecting,2001,37(3):20-23.
[48] 严 冰,严 寒,周 莉,等.江西相山火山岩型铀矿C、O、H、S同位素特征及意义[J].矿物岩石,2013,33(3):47-53.
YAN Bing,YAN Han,ZHOU Li,et al.Isotopic Chara-cteristics of C,O,H and S in Xiangshan Uranium Orefield,Jiangxi Province[J].Journal of Mineralogy and Petrology,2013,33(3):47-53.
[49] 黄锡强.江西相山铀矿田热液蚀变特征及成矿物理化学条件分析[D].北京:中国地质科学院,2008.
HUANG Xi-qiang.The Hydrothermal Alteration Cha-racteristics and Physics and Chemistry Conditions of Mineralization of Xiangshan Uranium Ore-field in Jiangxi[D].Beijing:Chinese Academy of Geological Sciences,2008.
[50] 李子颖,黄志章,李秀珍,等.相山火成岩与铀成矿作用[M].北京:地质出版社,2014.
LI Zi-ying,HUANG Zhi-zhang,LI Xiu-zhen,et al.Pyrogenesis and Uranium Metallogeny in Xiangshan Volcanic Basin,South China[M].Beijing:Geological Publishing House,2014.
[51] 杨水源,蒋少涌,赵葵东,等.江西相山铀矿田如意亭剖面火山岩的年代学格架及其地质意义[J].岩石学报,2013,29(12):4362-4372.
YANG Shui-yuan,JIANG Shao-yong,ZHAO Kui-dong,et al.Timing and Geological Implications of Volcanic Rocks from the Ruyiting Section,Xiangshan Uranium Ore Field,Jiangxi Province,SE China[J].Acta Petrologica Sinica,2013,29(12):4362-4372.
[52] 杨庆坤,黄强太,罗 勇,等.江西相山铀矿田深部铅锌矿成矿流体演化特征[J].科学技术与工程,2017,17(5):132-141.
YANG Qing-kun,HUANG Qiang-tai,LUO Yong,et al.The Characteristics of Metallogenic Fluid Evolution of Lead-zinc Polymetallic in Xiangshan Ore Field,Jiangxi Province[J].Science Technology and Engineering,2017,17(5):132-141.

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备注/Memo

备注/Memo:
收稿日期:2020-04-11; 修回日期:2020-06-01; 网络首发日期:2020-07-24投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41472069); 江西省自然科学基金重大项目(20152ACB20015)
作者简介:郭晶晶(1995-),女,江西赣州人,理学硕士研究生,E-mail:2053730463@qq.com。
*通讯作者:胡宝群(1965-),男,江西南昌人,教授,博士研究生导师,理学博士,E-mail:bqhu@ecut.edu.cn。
更新日期/Last Update: 2020-07-27