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矿床地质  2006 

湘南荷花坪锡多金属矿床地质特征及辉钼矿Re-Os测年

Keywords: 地球化学,矿床特征,Re-Os年龄,荷花坪锡多金属矿,湘南地区

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Abstract:

荷花坪锡多金属矿是近年来在湘南地区王仙岭岩体南东接触带新发现的一个具大型规模的矿床,主要由含锡矽卡岩和锡石_硫化物两类矿石组成。文章在研究和介绍矿床地质特征的基础上,对早期形成的矽卡岩矿石中的5个辉钼矿样品进行了Re-Os年龄测定,获得矽卡岩期成矿年龄为(224.0±1.9)Ma(n=5,MSWD=0.54),表明早期成矿作用发生在印支期,这是首次在南岭地区确认存在中生代早期锡矿化作用。晚期锡石_硫化物成矿作用中,燕山晚期的花岗斑岩脉被卷入其中,表明区内还存在燕山晚期的第二次叠加成矿作用。

References

[1]  毛景文,李红艳,裴荣富.1995.湖南千里山花岗岩的Nd-Sr同位素及岩石成因研究[J].矿床地质,14(3):235-242.
[2]  毛景文,李红艳,宋学信,芮柏.1998.湖南柿竹园钨锡铋多金属矿床地质特征与地球化学[M].北京:地质出版社.1~183.
[3]  毛景文,李晓峰,Bemd Lehmann,陈文,蓝晓明,魏绍六.2004.湖南芙蓉锡矿床锡矿石和有关花岗岩的40Ar-39Ar年龄及其地球学意义[J].矿床地质,23(2):164~175.
[4]  屈文俊,杜安道.2003.高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼-锇地质年龄[J].岩矿测试,22(4):254~257.
[5]  王昌烈,罗仕徽,胥友志,孙一虹,谢慈国,张重铭,徐文光,任湘眉.1987.柿竹园钨锡钼铋多金属矿床地质[M].北京:地质出版社.
[6]  王书凤,张绮玲.1988.柿竹园矿床地质引论[M].北京:北京科学技术出版社.
[7]  王岳军,范蔚茗,梁新权,彭头平,石玉若.2005.湖南印支期花岗岩SHRIMP锆石U-Pb年龄及其成因启示[J].科学通报,50(12):1259~1266.
[8]  赵振华,包志伟,张伯友,熊小林.2000.柿竹园超大型钨多金属矿床形成的壳幔相互作用背景[J].中国科学(D辑),30(增刊):161~168.
[9]  李红艳,毛景文,孙亚利,邹晓秋,何红蓼,杜安道.1996.柿竹园钨多金属矿Re-Os同位素等时线年龄研究[J].地质论评,42(3):261-267.
[10]  刘义茂,戴橦模,卢焕章,胥友志,王昌烈,康卫清.1997.千里山花岗岩成岩成矿的Ar-Ar和Sm-Nd同位素年龄[J].中国科学(D辑),27(5):425~430.
[11]  Chen Y C,Mao J W and Zou T R.1995.Metallogenic series of ore deposits and metallogenic evolution through geological history in North Guangxi[M].Nanning:Guangxi Sci.& Technol.Press.1~433(in Chinese).
[12]  Du A D,He H L,Yin N W,Zou X Q,Sun Y L,Sun D Z,Chen S Z and Qu W J.1994.A study on the rhenium-osmium geochronometry of molybdenites[J].Acta Geologica Sinica,68 (4):339 ~ 347 (in Chinese with English abstract).
[13]  Du A D,Zhao D M,Wang S X,Sun D Z and Liu D Y.2001.Precise Re-Os dating for molybdenite by ID-NTIMS with tube sample preparation[J].Rock & Mineral Analysis,20(4):247~252(in Chinese with English abstract).
[14]  Du A D,Wu S Q,Sun D Z,Richard M H S,John M and Dmitry M.2004.Preparation and certification of Re-Os dating reference materials:Molybdenite HLP and JDC[J].Geostandard & Geoanalytical Research,28 (1):41~52.
[15]  Guo F,Fan W M,Lin G and Lin Y X.1997.Sm-Nd dating and petrogenesis of Mesozoic gabbro xenolith in Daoxian County,Hunan Province[J].Chinese Sci.Bull.,42(17):1661~1663(in Chinese).
[16]  Li C L,Zhong C S,Wang F Z and Liu C F.2001.Geochemistry and petrogenesis of Mesozoic basaltic rocks and their deep source enclaves in Northern Guangxi-Sourthern Hunan[J].Acta Petrologica et Mineralogica,20 (2):112 ~ 122 (in Chinese with English abstract).
[17]  Li H Y,Mao J W,Sun Y L,Zou X Q,He H L and Du A D.1996.Re-Os isotopic chronology of molybdenites in the Shizhuyuan polymetallic tungsten deposit[J].Geol.Rev.,42(3):261~ 263 (in Chinese with English abstract).
[18]  Liu Y M,Dai T M,Lu H Z,Xu Y Z,Wang C L and Kang W Q.1997.Ar/Ar and Sm-Nd isotopic ages of the lithogenesis and mineralization of the Q ianlishan granite[J].Sci.in China (Series D),27(5):425~430(in Chinese).
[19]  Ludwig K R.1999.Using isoplot/EX,version 2.0:A geochronolgical toolkit for Microsoft excel[M].Berkeley:Geochronological Center,Special Publication,1a.47.
[20]  Mao J W,Li H Y and Pei R F.1995.Nd-Sr isotopic and petrogenitic studies of the Qianlishan granite stock,Hunan Province[J].Mineral Deposits,14(3):235~242(in Chinese with English abstract).
[21]  Mao J W,Li H Y,Song X X and Rui B.1998.Geology and geochemistry of the Shizhuyuan W-Sn-Bi-polymetallic deposits,Hunan,China[M].Beijing:Geol.Pub.House.183p(in Chinese with English abstract).
[22]  Mao J W,Li X F,Bernd L,Chen W,Lan X M and Wei S L.2004.40Ar-39Ar dating of tin ores and related granite in Furong tin orefield,Hunan Province,and its geodynamic significance[J].Mineral Deposits,23 (2):164175 (in Chinese with English abstract).
[23]  Qu W J and Du A D.2003.The electrochemical behavior of dopamine on Poly (cinchomeronic acid) modified glassy carbon electrode and its detection[J].Rock & Mineral Analysis,22(4):254~~257(in Chinese and English abstract).
[24]  Shirey S B and Walker R J.1995.Carius tube digestion for low-blank rhenium-osmium analysis,Anal[J].Chem.,67:2136~2141.
[25]  Wang C L,Luo S H,Xu Y Z,Sun Y H,Xie C G,Zhan C M,Xu W G and Ren X M.1987.Geology of Shizhuyuan W-Sn-Mo-Bi polymetal deposit[M].Beijing:Geol.Pub.House (in Chinese with English abstract).
[26]  Wang S F and Zhang Q L.1988.Geology of Shizhuyuan deposit[M].Beijing:Beijing Sci.& Technol.Press(in Chinese with English abstract).
[27]  Wang Y J,Fan W M,Liang X Q,Peng T P and Shi Y R.2005.SHRIMP U-Pb zircon dating of Indosinian granites in Hunan Province and its petrogenetic implications[J].Chinese Sci.Bull.,50(12):1259~1266(in Chinese).
[28]  Zhao Z H,Bao Z W,Zhang B Y and Xiong X L.2000.Crust-mantle interaction of the Shizhuyuan super large polymetallic tungsten deposit[J].Sci.in China (Series D),30(Supp.):161~168(in Chinese).
[29]  陈毓川,毛景文,邹天人.1995.桂北地区矿床成矿系列和成矿历史演化轨迹[M].南宁:广西科学技术出版社.1~433.
[30]  杜安道,何红蓼,殷宁万,邹晓秋,孙亚利,孙德忠,陈少珍,屈文俊.1994.辉钼矿的铼-锇同位素地质年龄测定方法研究[J].地质学报,68(4):339~347.
[31]  更多...
[32]  杜安道,赵敦敏,王淑贤,孙德忠,刘敦一.2001.Carius管溶样和负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄[J].岩矿测试,20(4):247~252.
[33]  郭峰,范蔚茗,林舸,林源贤.1997.湘南道县中生代辉长岩包体的Sm-Nd定年和岩石成因[J].科学通报,42(17):1661~1663.
[34]  李昌年,钟称生,王方正,刘春芳.2001.桂北-湘南中生代玄武质岩石及其深源包体的地球化学性质和岩石成因探讨[J].岩石矿物学杂志,20(2):112~122.

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