«上一篇/Previous Article|本期目录/Table of Contents|下一篇/Next Article»

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第32卷

期数:

2010年第01期

页码:

1-14

栏目:

基础地质与矿产地质

出版日期:

2010-03-15

文章信息/Info

Title:

Porphyry Cu,Epithermal Ag-Pb-Zn, Distal Hydrothermal Au Deposits:a New Model of Mineral Deposit——Taking the Dexing Area as an Example

文章编号:

1672-6561(2010)01-0001-14

作者:

毛景文; 张建东; 郭春丽

(中国地质科学院矿产资源研究所 成矿作用与资源评价国土资源部重点实验室,北京 100037)

Author(s):

MAO Jing-wen;  ZHANG Jian-dong;  GUO Chun-li

(Key Laboratory of Metallogeny and Mineral Assessment of Ministry of Land and Resources, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China)

关键词:

成矿流体; 铜矿; 银铅锌矿; 金矿; 德兴

Keywords:

ore-forming fluid;  Cu;  Ag-Pb-Zn;  Au;  Dexing

分类号:

P612

DOI:

-

文献标志码:

A

摘要:

在前人研究的基础上,通过系统的野外考察,论证了位于赣东北德兴地区德乐中生代火山盆地中的德兴铜矿、银山银铜铅锌矿和金山金矿及蛤蟆石金矿属于同一成矿系统。德兴铜矿是典型的斑岩铜矿,成矿流体和金属元素主要来自岩浆;银山银铜铅锌矿是一个下部为斑岩铜矿、上部为浅成低温热液型银铅锌矿,成矿流体早期以岩浆为主,晚期有较多的大气降水参与,成矿物质主要来自岩浆;金山和蛤蟆石金矿是远接触带热液矿床,成矿流体为岩浆热液与大气降水的混合产物,金主要来自围岩——双桥山群浅变质岩。这3套矿床以中酸性花岗斑岩或石英斑岩(高钾钙碱质花岗岩)为核心具有明显的分带性,自中心向外或深部向浅部为:斑岩铜金钼矿、浅成低温热液型银铅锌矿和远接触带热液型金矿。这种矿床组合关系不同于已知的经典斑岩铜矿模型和斑岩铜矿-浅成低温热液金银矿床模型,因而,有必要提出一个新的模型:斑岩铜矿-浅成低温热液银铅锌矿-远接触带热液金矿模型。这套矿床形成于中侏罗世,抑或是古太平洋俯冲板片局部重熔或撕裂重熔的产物,抑或是在活动大陆边缘岩浆弧后伸展带由地幔底侵的结果。

Abstract:

Based on the previous studies and detailed field investigations in the Dexing porphyry Cu deposit, the Yinshan Ag-Pb-Zn deposit and the Jinshan shear zone-hosted Au deposit in the Dele Jurassic volcanic basin in the northeastern Jiangxi Province, East China are proposed to be same metallogenic system in this paper. The Dexing is a typical porphyry Cu-Au-Mo deposit in which both ore-forming fluid and elements are derived from the granite porphyry. The Yinshan consists of porphyry Cu ore at the copular of quartz porphyry in the lower part and the vein type Ag-Pb-Zn ore in the upper part. The hydrothermal fluid was mainly derived from the magma in the early stage and was incorporated with more meteoric water in the late stage. Its ore-forming elements are mainly from the magma. The both Jinshan and the Hamashi, a quartz vein type gold deposit hosted by brittle fractures, are distal hydrothermal deposits, which were formed by mixed fluids of magmatic and meteoric water whereas the Au is mainly leached from the country rocks of Middle Proterozoic schists of the Shuangqiaoshan Group. These deposits spatially show a distinct zoning of porphyry Cu, epithermal Ag-Pb-Zn and distal Au from the granite porphyry of quartz porphyry outside. In this case we suggest a new model entitled in porphyry-epithermal-distal system model for the group of mineral deposits with genetic relationship.

参考文献/References:

[1] Emmons W H.Principle of Economic Geology[M].New York:McGraw-Hill,1918.
[2] Lowell J D,Guilbert J M.Lateral and Vertical Alteration-mineralization Zoning in Porphyry Ore Deposits[J].Econo-mic Geology,1970,65(4):373-408.
[3] White N C,Hedenquist J W.Epithermal Gold Deposits:Styles,Characteristics and Exploration[J].SEG Newsletter,1995,23:9-13.
[4] 芮宗瑶,黄崇轲,齐国明,等.中国斑岩铜(钼)矿床[M].北京:地质出版社,1984.
[5] 裴荣富.中国特大型矿床成矿偏在性与异常成矿构造聚敛场[M].北京:地质出版社,1998.
[6] Zhou X M,Zhu Y H.Late Proterozoic Collisional Orogen and Geosuture in Southeastern China:Petrological Evidence[J].Chinese Journal of Geochemistry,1993,12(3):239-251.
[7] Li X H,Zhao J X,McCulloch M T,et al.Geochemical and Sm-Nd Isotopic Study of Neoproterozoic Ophiolites from Southeastern China:Petrogenesis and Tectonic Implications[J].Precambrian Research,1997,81(1/2):129-144.
[8] Li Z X,Li X H,Zhou H W,et al.Grenvillian Continental Collision in South China:New SHRIMP U-Pb Zircon Results and Implications for the Configuration of Rodinia[J].Geology,2002,30(2):163-166.
[9] 刘英俊,孙承辕,马东升.江南金矿及其成矿地球化学背景[M].南京:南京大学出版社,1993.
[10] 毛景文,李红艳.江南古陆某些金矿床成因讨论[J].地球化学,1997,26(5):71-81.
[11] Gilder S A,Gill J,Coe R S,et al.Isotopic and Paleomagnetic Constraints on the Mesozoic Tectonic Evolution of South China[J].Journal of Geophysical Research,1996,101(B7):16137-16154.
[12] 李晓峰,易先奎,朱和平.德兴金山金矿床成矿流体来源:小尺度构造和同位素地球化学证据[J].矿床地质,2009,28(1):42-52.
[13] 刘英俊,沙 鹏,朱凯军.江西德兴地区中元古界双桥山群含金建造的地球化学研究[J].桂林冶金地质学院学报,1989,9(2):115-126.
[14] 江西省地质矿产局.江西省区域地质志[M].北京:地质出版社,1984.
[15] 徐 备,乔广生.赣东北晚元古代蛇绿岩套的Sm-Nd同位素年龄及原始构造环境[J].南京大学学报:自然科学版,1989,25(3):108-114.
[16] 周国庆,赵建新.华南扬子克拉通东南缘赣东北蛇绿岩的Sm-Nd同位素研究[J].科学通报,1991,36(2):129-132.
[17] 李献华,周国庆,赵建新,等.赣东北蛇绿岩的离子探针锆石U-Pb年龄及其构造意义[J].地球化学,1994,23(2):125-131.
[18] Li X H,Li Z X,Li W X,et al.U-Pb Zircon,Geochemical and Sr-Nd-Hf Isotopic Constraints on Age and Origin of Jurassic I- and A-type Granites from Central Guangdong,SE China:a Major Igneous Event in Response to Foundering of a Subducted Flat-slab?[J].Lithos,2007,96(1/2):186-204.
[19] 王 强,赵振华,简 平,等.德兴花岗闪长斑岩SHRIMP锆石U-Pb年代学和Nd-Sr同位素地球化学[J].岩石学报,2004,20(2):315-324.
[20] 朱 训,黄崇轲,芮宗瑶,等.德兴斑岩铜矿[M].北京:地质出版社,1983.
[21] Li X F,Sasaki M.Hydrothermal Alteration and Mineralization of Middle Jurassic Dexing Porphyry Cu-Mo Deposit,Southeast China[J].Resource Geology,2007,57(4):409-426.
[22] 金章东,朱金初,李福春.德兴斑岩铜矿成矿过程的氧、锶、钕同位素证据[J].矿床地质,2002,21(4):341-349.
[23] Lu J J,Hua R M,Yao C L.Re-Os Age for Molybdenite from the Dexing Porphyry Cu-Au Deposit in Jiangxi Province,China[J].Geochimica et Cosmochimica Acta,2005,69(S1):A882.
[24] Li X F,Watanabe Y,Mao J W,et al.Sensitive High-resolution Ion Microprobe U-Pb Zircon and ⁴⁰Ar-³⁹Ar Muscovite Ages of the Yinshan Deposit in the Northeast Jiangxi Province,South China[J].Resource Geology,2007,57(3):325-337.
[25] 叶庆同.赣东北铅锌矿床成矿系列和成矿机理[M].北京:北京科学技术出版社,1987.
[26] 李传明.江西银山铜铅锌矿床成矿特征[J].地质与勘探,1986(6):3-8.
[27] 倪 培.闽浙赣相邻区铜金属矿床成矿规律总结研究报告[R].南京:南京大学,2009.
[28] Zhang D H,Xu G J,Zhang W H,et al.High Salinity Fluid Inclusions in the Yinshan Polymetallic Deposit from the Le-De Metallogenic Belt in Jiangxi Province,China:Their Origin and Implications for Ore Genesis[J].Ore Geology Reviews,2007,31(1/4):247-260.
[29] 杨 斌,彭省临,杨 牧,等.江西银山铜铅锌矿床热液对流与蚀变矿化分带机制[J].桂林工学院学报,2004,24(4):395-401.
[30] Zhang D H,Yu C W,Bao Z Y,et al.Ore Zoning and the Dynamics of Ore-forming Processes in the Yinshan Polymetallic Deposit in Dexing,Jiangxi[J].Chinese Journal of Geochemistry,1997,16(2):123-132.
[31] Zhang L G,Liu J X,Yu G X,et al.Hydrogen and Oxygen Isotopes Study on the Water-rock Interaction of the Yinshan(Cu-)Pb-Zn-Ag Ore Deposit,Jiangxi Province[J].Acta Geologica Sinica:English Edition,1996,9(3):274-289.
[32] 韦星林.金山金矿田地质特征及成矿地质作用[J].矿产与地质,1995,9(6):471-480.
[33] Li X F,Wang C Z,Hua R M,et al.Fluid Origin and Structural Enhancement During Progressively Localized Mineralization of the Jinshan Orogenic Gold Deposit,South China[J].Mineralium Deposita,2010(in press).
[34] 范宏瑞,李兆麟.金山金矿床地质特征成矿物理化学条件及成矿物质来源[J].地质科学,1992(增刊):147-160.
[35] 张文淮,谭铁龙.江西省金山金矿有机流体与金矿关系[J].矿床地质,1998,17(1):15-24.
[36] 邹焕炎.江西金山金矿韧性剪切带中有机质与金矿化的关系[J].黄金科技动态,1993(3):10-12.
[37] 黄宏立,杨文思.赣东北金山金矿床的地质特征及矿床成因[J].地质找矿论丛,1990,5(2):29-39.
[38] 杨卫明,李昌存,韩秀丽.金山金矿床流体包裹体研究[J].黄金,2000,21(6):9-11.
[39] 李晓峰,王春增,易先奎,等.德兴金山金矿田不同尺度构造特征及其与成矿作用的关系[J].地质论评,2007,53(6):774-782.
[40] 季峻峰,孙承辕,郑 晴.江西金山剪切带型金矿床中含金石英脉的成矿特征[J].地质论评,1994,40(4):361-367.
[41] 刘志远,金成洙,王荣湖,等.江西金山金矿床成矿流体地球化学及矿床成因讨论[J].地质找矿论丛,2005,20(2):93-99.
[42] Cooke D,Hollings P,Holliday J.Circum-Pacific Porphyry Copper,Gold and Molybdenum Deposits[C]∥Committee of 2008 Pacific Rim Congress.The Pacific Rim:Mineral Endowment,Discovery and Exploration Frontiers.Carlton South:Australasian Institute of Mining and Metallurgy,2008:7-14.
[43] Rebagliati C M,Payne J G.Summary Report on the Pebble Porphyry Copper-gold Project[R].Vancouver:Northern Dynasty Minerals Limited,2005.
[44] Lang J R,Rebagliati C M,Roberts K,et al.The Pebble Copper-gold-molybdenum Porphyry Deposit,Southwest Alaska,USA[C]∥Committee of 2008 Pacific Rim Congress.The Pacific Rim:Mineral Endowment,Discovery and Exploration Frontiers.Carlton South:Australasian Institute of Mining and Metallurgy,2008:27-32.
[45] Seedorff E,Dilles J H,Proffett J J M,et al.Porphyry Deposits:Characteristics and Origin of Hypogene Features[C]∥Hedenquist J W,Thompson J F H,Goldfarb R J,et al.Economic Geology,One Hundred Anniversary Volume 1905-2005.Washington:Society of Economic Geologists,2005:251-298.
[46] 张 旗,王 焰,钱 青,等.中国东部燕山期埃达克岩的特征及其构造-成矿意义[J].岩石学报,2001,17(2):236-244.
[47] Ishihara S.The Magnetite-series and Ilmenite-series Granitic Rocks[J].Mining Geology,1977,27:293-305.
[48] 徐克勤,胡受奚,孙明志,等.华南两个成因系列花岗岩及其成矿特征[J].矿床地质,1982,1(2):1-14.
[49] Heald P,Foley N K,Hayba D O.Comparative Anatomy of Volcanic-hosted Epithermal Deposits:Acid-sulfate and Adularia-sericite Types[J].Economic Geology,1987,82(1):1-26.
[50] Hedenquist J W,Arribas A J,Gonzales-Urien E.Exploration for Epithermal Gold Deposits[J].Reviews in Economic Geology,2000,13:245-277.
[51] Simmons S,White N C,John N C.Geological Characteristics of Epithermal Precious and Base Metal Deposits[C]∥Hedenquist J W,Thompson J F H,Goldfarb R J,et al.Economic Geology,One Hundred Anniversary Volume 1905-2005.Washington:Society of Economic Geologists,2005:485-522.
[52] Rui Z Y,Wang L S,Wu C Y,et al.Dexing Porphyry Copper Deposits in Jiangxi,China[C]∥Porter T M.Super Porphyry Copper and Gold Deposits:a Global Prospective.Adelaide:PGC Publishing,2005:409-421.
[53] 陈毓川,裴荣富,张宏良,等.南岭地区与中生代花岗岩类有关的有色及稀有金属矿床地质[M].北京:地质出版社,1989.
[54] 伍勤生,刘青莲.金山成矿年龄测定及矿床成因探讨[C]∥中国地质学会同位素地质专业委员会.第四届全国同位素地质年代学、同位素地球化学学术讨论会论文(摘要)汇编.杭州:中国地质学会同位素地质专业委员会,1989:20-25.
[55] 张金春.江西金山韧性剪切型金矿成矿地球化学研究[D].南京:南京大学,1994.
[56] 王秀璋,梁华英,单 强,等.金山金矿成矿年龄测定及华南加里东成金期的讨论[J].地质论评,1999,45(1):19-25.
[57] 毛光周,华仁民,龙光明,等.江西金山金矿成矿时代探讨——来自石英流体包裹体Rb-Sr年龄的证据[J].地质学报,2008,82(4):532-539.
[58] 毛景文,谢桂青,郭春丽,等.南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景[J].岩石学报,2007,23(10):2329-2338.
[59] 毛景文,谢桂青,郭春丽,等.华南地区中生代主要金属矿床时空分布规律和成矿环境[J].高校地质学报,2008,14(4):510-526.
[60] 董树文,张岳桥,龙长兴,等.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报,2007,81(11):1449-1461.
[61] Goldfarb R J,Baker T D,Groves D I,et al.Distribution,Character of Gold Deposits in Metamorphic Terranes[C]∥Hedenquist J W,Thompson J F H,Goldfarb R J,et al.Economic Geology,One Hundred Anniversary Volume 1905-2005.Washington:Society of Economic Geologists,2005:407-450.
[62] Zhou T H,Goldfarb R J,Phillips G N.Tectonics and Distribution of Gold Deposits in China:an Overview[J].Minera-lium Deposita,2002,37(3/4):249-282.
[63] Mao J W,Qiu Y M,Goldfarb R J,et al.Geology,Distribution,and Classification of Gold Deposits in the Western Qinling Belt,Central China[J].Mineralium Deposita,2002,37(3/4):352-377.
[64] Mao J W,Goldfarb R J,Zhang Z W,et al.Gold Deposits in the Xiaoqinling-Xiong'ershan Region,Qinling Mountains,Central China[J].Mineralium Deposita,2002,37(3/4):306-325.
[65] Hart C J R,Goldfarb R J,Qiu Y M,et al.Gold Deposits of the Northern Margin of the North China Craton:Multiple Late Paleozoic-Mesozoic Mineralizing Events[J].Mineralium Deposita,2002,37(3/4):326-351.
[66] Nie F J,Jiang S H,Liu Y.Intrusion-related Gold Deposits of North China Craton,People's Republic of China[J].Resource Geology,2003,54(3):299-324.
[67] 舒良树,周新民,邓 平,等.中国东南部中、新生代盆地特征与构造演化[J].地质通报,2004,23(9/10):876-884.
[68] 舒良树,王德滋.北美西部与中国东南部盆岭构造对比研究[J].高校地质学报,2006,12(1):1-13.
[69] Chen J F,Jahn B M.Crustal Evolution of Southeastern China:Nd and Sr Isotopic Evidence[J].Tectonophysics,1998,284(1/2):101-133.
[70] Hong D W,Xie X L,Zhang J S.Isotope Geochemistry of Granitoids in South China and Their Metallogeny[J].Resource Geology,1998,48(4):251-263.
[71] Li Z X,Li X H.Formation of the 1 300 km-wide Intracontinental Orogen and Postorogenic Magmatic Province in Mesozoic South China:a Flat-slab Subduction Model[J].Geology,2007,35(2):179-182.
[72] 许美辉.福建省永定地区早侏罗世双峰式火山岩及其构造环境[J].福建地质,1992,11(2):115-125.
[73] 赵振华,包志伟,张伯友.湘南中生代玄武岩类地球化学特征[J].中国科学(D辑),1998,28(增刊):7-14.
[74] 陶奎元,毛建仁,杨祝良,等.中国东南部中生代岩石构造组合和复合动力学过程的记录[J].地学前缘,1998,5(4):183-191.
[75] 陈培荣,孔兴功,王银喜,等.赣南燕山早期双峰式火山-侵入杂岩的Rb-Sr同位素定年及意义[J].高校地质学报,1999,5(4):378-383.
[76] 陈培荣,华仁民,章邦桐,等.南岭燕山早期后造山花岗岩类:岩石学制约和地球动力学背景[J].中国科学(D辑),2002,32(4):279-289.
[77] Wang Y J,Fan W M,Guo F,et al.Geochemistry of Mesozoic Mafic Rocks Adjacent to the Chenzhou-Linwu Fault,South China:Implications for the Lithospheric Boundary Between the Yangtze and Cathaysia Blocks[J].International Geological Review,2003,45(3):263-286.
[78] Li X H,Chen Z G,Liu D Y,et al.Jurassic Grabbro-Granite-Syenite Suites from Southern Jiangxi Province,SE China:Age,Origin,and Tectonic Significance[J].International Geology Review,2003,45(10):898-921.
[79] Zhou X M,Sun T,Shen W Z,et al.Petrogenesis of Mesozoic Granitoids and Volcanic Rocks in South China:a Response to Tectonic Evolution[J].Episodes,2006,29(1):26-33.
[80] 毛景文,谢桂青,李晓峰,等.华南地区中生代大规模成矿作用与岩石圈多阶段伸展[J].地学前缘,2004,11(1):45-55.
[81] 侯增谦,潘小菲,杨志明,等.初论大陆环境斑岩铜矿[J].现代地质,2007,21(2):332-351.
[82] Wang Q,Xu J F,Jian P,et al.Petrogenesis of Adakitic Porphyries in an Extensional Tectonic Setting,Dexing,South China:Implications for the Genesis of Porphyry Copper Mine-ralization[J].Journal of Petrology,2006,47(1):119-144.
[83] 郭春丽,毛景文,陈毓川.十杭带对南岭地区中侏罗世成岩成矿作用的制约——对与铜金银铅锌矿有关花岗闪长质岩体地球化学特征的总结[J].岩石学报,2010,26(3)(in press).
[84] Arnaud N O,Vidal P,Tapponnier P,et al.The High K₂O Volcanism of Northwestern Tibet:Geochemistry and Tectonic Implications[J].Earth and Planetary Science Letters,1992,111(2/4):351-367.
[85] Thompson A B.Fertility of Crustal Rocks During Anatexis[J].GSA Special Papers,1996,315:1-10.
[86] 孔 华,金振民,林源贤.道县玄武岩中麻粒岩包体的岩石学及年代学[J].长春科技大学学报,2000,30(2):115-119.
[87] Sen C,Dunn T.Dehydration Melting of a Basaltic Composition Amphibolite at 1.5 and 2.0 GPa:Implications for the Origin of Adakites[J].Contributions to Mineralogy and Petrology,1994,117(4):394-409.
[88] Rapp R P,Watson E B.Dehydration Melting of Metabasalt at 8～32 kbar:Implications for Continental Growth and Crust-mantle Recycling[J].Journal of Petrology,1995,36(4):891-931.

相似文献/References:

[1]代堰锫,张惠华,朱玉娣,等.扬子陆块西缘江浪穹窿及“里伍式”富铜矿床研究进展与问题[J].地球科学与环境学报,2016,38(01):66.
　DAI Yan-pei,ZHANG Hui-hua,ZHU Yu-di,et al.Review on Jianglang Dome and Liwu-type Cu-rich Deposit in the Western Margin of Yangtze Block[J].Journal of Earth Sciences and Environment,2016,38(01):66.
[2]李厚民,毛景文,张长青.滇黔交界地区玄武岩铜矿流体包裹体地球化学特征[J].地球科学与环境学报,2011,33(01):14.
　LI Hou-min,MAO Jing-wen,ZHANG Chang-qing.Geochemistry of Fluid Inclusions of the Basalt Copper Deposits in Adjacent Area of Northeastern Yunnan and Western Guizhou, China[J].Journal of Earth Sciences and Environment,2011,33(01):14.
[3]李文渊.现代海底热液成矿作用[J].地球科学与环境学报,2010,32(01):15.
　LI Wen-yuan.Hydrothermal Mineralization on the Modern Seafloor[J].Journal of Earth Sciences and Environment,2010,32(01):15.
[4]朱华平,孙丰月,李碧乐,等.青海驼路沟钴矿床流体 包裹体及成矿物理化学条件[J].地球科学与环境学报,2007,29(04):351.
　ZHU Hua-ping,SUN Feng-yue,LI Bi-le,et al.Fluid Inclusions Characteristics and Physicochemical Condition of Tuolugou Cobalt Deposit,Qinghai[J].Journal of Earth Sciences and Environment,2007,29(01):351.
[5]刘新会,刘爽,李渊,等.丁家山古楼山金矿床成矿流体储运规律[J].地球科学与环境学报,2006,28(01):24.
　LIU Xin-hui,LIU Shuang,LI Yuan,et al.Storage and Moving of Ore-forming Fluid of Dingjiashan-Gulushan Gold Deposit[J].Journal of Earth Sciences and Environment,2006,28(01):24.
[6]杨中宝,彭省临,胡祥昭,等.浏阳七宝山铜多金属矿床流体包裹体特征及成矿意义[J].地球科学与环境学报,2004,26(02):11.
　YANG Zhong-bao,PENG Sheng-lin,HU Xiang-zhao,et al.Ore-forming fluid inclusion characteristics and metallogen of the Qibaoshan Cu-polymetal deposit in Liuyang , Hunan[J].Journal of Earth Sciences and Environment,2004,26(01):11.
[7]韩文华,方维萱,张贵山,等.新疆萨热克砂砾岩型铜矿区碎裂岩化相特征[J].地球科学与环境学报,2017,39(03):397.
　HAN Wen-hua,FANG Wei-xuan,ZHANG Gui-shan,et al.Characteristics of Cataclastic Lithofacies in Sareke Glutenite-type Cu Mining Area of Xinjiang, China[J].Journal of Earth Sciences and Environment,2017,39(01):397.
[8]刘晓通,毛光周,王向军,等.山东沂沭断裂带中段南小尧金矿元素地球化学特征及其地质意义[J].地球科学与环境学报,2018,40(01):76.
　LIU Xiao-tong,MAO Guang-zhou,WANG Xiang-jun,et al.Elemental Geochemistry Characteristics and Their Geological Significance of Nanxiaoyao Gold Deposit in the Middle of Yishu Fault Zone, Shandong, China[J].Journal of Earth Sciences and Environment,2018,40(01):76.
[9]张革利,王瑞廷,田涛,等.陕西凤太矿集区东塘子铅锌矿床地质-地球化学特征与成因[J].地球科学与环境学报,2018,40(05):520.
　ZHANG Ge-li,WANG Rui-ting,TIAN Tao,et al.Geological-geochemical Characteristics and Genesis of Dongtangzi Pb-Zn Deposit in Fengxian-Taibai Ore Concentration Area of Shaanxi, China[J].Journal of Earth Sciences and Environment,2018,40(01):520.

备注/Memo

备注/Memo:

收稿日期:2010-01-15
基金项目: 国家重点基础研究发展计划项目(2007CB411405; 2007CB411407); 国家自然科学青年基金项目(40803008); 中国地质调查局项目(1212010634001)
作者简介: 毛景文(1956-),男,山西运城人,研究员,博士研究生导师,从事矿床学研究。E-mail:jingwenmao@263.net

常用功能

更新日期/Last Update: 2010-03-20