江西省于都县盘古山钨铋(碲)矿床地质特征及成矿年代学研究
摘要
盘古山钨铋矿床位于南岭成矿带东段的赣县-于都钨多金属矿集区,为一赋存于隐伏岩体外接触带的石英脉大型钨铋(碲)矿床。笔者采集了该矿区内2条不同地质产状黑钨矿-石英脉中的辉钼矿样品,进行了辉钼矿Re-Os同位素测试,获得其等时线年龄为(157.75±0.76)Ma(MSWD=0.99)和(158.8±5.7)Ma(MSWD=1.7)。测试结果显示,这2组矿脉是同一时期的成矿产物,均形成于燕山早期,属南岭EW向构造-岩浆带作用的产物。
The Pangushan tungsten ore deposit is a large-size wolframite-quartz vein type W-Bi(Te) ore deposit in the exocontact zone of the buried rock body within the eastern part of the Nanling metallogenic belt.The authors collected molybdenite samples from the W-bearing quartz veins of different geological modes of occurrence.Re-Os isotopic dating yielded isochron ages of molybdenite(157.75±0.76) Ma(MSWD=0.99) and(158.8±5.7) Ma(MSWD=1.7).The ages indicate that these two mineralized veins belong to the same product and were formed in the same period,i.e.,Early Yanshanian.The study also provides useful evidence that the ore deposit is the product of Nanling EW-trending tectonic-magmatic belt.
The Pangushan tungsten ore deposit is a large-size wolframite-quartz vein type W-Bi(Te) ore deposit in the exocontact zone of the buried rock body within the eastern part of the Nanling metallogenic belt.The authors collected molybdenite samples from the W-bearing quartz veins of different geological modes of occurrence.Re-Os isotopic dating yielded isochron ages of molybdenite(157.75±0.76) Ma(MSWD=0.99) and(158.8±5.7) Ma(MSWD=1.7).The ages indicate that these two mineralized veins belong to the same product and were formed in the same period,i.e.,Early Yanshanian.The study also provides useful evidence that the ore deposit is the product of Nanling EW-trending tectonic-magmatic belt.
引文
①江西盘古山钨业有限公司.2005.江西省于都县盘古山钨矿资源潜力调查报告.内部资料.
①江西盘古山钨业有限公司.2005.江西省于都县盘古山钨矿资源潜力调查报告.内部资料.图2据报告插图修改.
①江西盘古山钨业有限公司.2005.江西省于都县盘古山钨矿资源潜力调查报告.内部资料.
①江西盘古山钨业有限公司.2005.江西省于都县盘古山钨矿资源潜力调查报告.内部资料.
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①江西盘古山钨业有限公司.2005.江西省于都县盘古山钨矿资源潜力调查报告.内部资料.
①江西盘古山钨业有限公司.2005.江西省于都县盘古山钨矿资源潜力调查报告.内部资料.
Cai J M,Liu R L,Zeng G S,et al.1981.Study on fluid inclusion andits relation to mineralization of Pangushan tungsten deposit,JiangxiProvince,China[J].Journal of Chengdu University of Technology(Science&Technology Edition),2:99-103(in Chinese with Eng-lish abstract).
Chen Z H,Wang D H,Qu WJ,Chen Y C,Wang P A,XuJ X,ZhangJ J and Xu ML.2006.Geological characteristics and mineralizationage of the Taoxikeng tungstenite deposit in Chongyi County,JiangxiProvince[J].Geological Bulletin of China,25(4):496-501(in Chi-nese with English abstract).
Du A D,He HL,Yin N W,Zou X Q,Sun Y L,Sun D Z,Chen S Zand Qu WJ.1994.Astudy onthe rhenium-osmiumgeochronometryof molybdenites[J].Acta Geologica Sinica,68(4):339-347(in Chi-nese with English abstract).
Du A,Wu S,Wang S,Qu W,Markey R,Stain H,MorganJ and Ma-linovskiy D.2004.Preparation and certification of Re-Os dating re-ference materials:Molybdenite HLP and JDC[J].Geostandard andGeoanalytical Research,28(1):41-52.
Du A D,Zhao D M,Wang S X,Sun D Z and Liu D Y.2001.PreciseRe-Os dating for molybdenite by ID-NTI MS with carius tube samplepreparation[J].Rock and Mineral Analysis,20(4):247-252(inChinese with English abstract).
Feng C Y,Feng Y D,XuJ X,Zeng Z L,She HQ,Zhang D Q,Qu WJ and Du A D.2007a.Isotope chronological evidence for UpperJurassic petrogenesis and mineralization of altered granite-type tung-sten depositsinthe Zhangtiantang area,southern Jiangxi[J].Geolo-gyin China,34(4):642-650(in Chinese with English abstract).
Feng C Y,XuJ X,Zeng Z L,Zhang D Q,Qu WJ,She HQ,Li J W,Li D X,Du A Dand Dong YJ.2007b.Zircon SHRI MP U-Pb andmolybdenite Re-Os datingin Tianmenshan-Hongtaoling tungsten-tinorefield,Southern Jiangxi Province,China,andits geological impli-cation[J].Acta Geologica Sinica,81(7):952-963(in Chinese withEnglish abstract).
Han J Z,Hu X Mand Liu S L.1984.The contrals of strata over tung-sten ore deposits as viewedfromtungsten abundancesinthe strata ofsouthern Jianxi[J].Geochimica,(2):176-179(in Chinese withEnglish abstract).
Li HY,Mao J W,Sun Y L,Zou X Q,He HL and Du A D.1996.Re-Os isotopic chronology of molybdenites in the Shizhuyuan poly-metallic tungsten deposit,southern Hunan[J].Geological Review,42(3):261-267(in Chinese with English abstract).
Li S Band Zeng Z L.2006.The analysis of ore-forming geological condi-tions in southern Jiangxi province and its guidance significance fortungsten prospecting[J].Journal of East China Institute of Technol-ogy,(S1):28-37(in Chinese with English abstract).
Mao J W,Chen Y C,ZhouJ Xand Yang B C.1995.Geology,mineral-ogy,and geochemistry of the Dashuigoutelluriumdeposit in ShimianCounty,Sichuan[J].Acta Geosicientia Sinica,6(3):276-290(inChinese with English abstract).
Mao J W,Holly Stein,Du A D,Zhou T F,Mei Y X,Li Y F,Zang WS and Li J W.2004a.Molybdenite Re-Os precise dating for molyb-denite from Cu-Au-Mo deposits in the middle-lower reaches ofYangtze River Belt and its implications for mineralization[J].ActaGeologica Sinica,78(1):122-128(in Chinese with English ab-stract).
Mao J Wand Li Y Q.2001.Fluid inclusions of the Dongping gold tel-luride deposit in Hebei Province,China:Involvement of mantle fluidin metallogenesis[J].Mineral Deposits,20(1):24-36(in Chinesewith English abstract).
Mao J Wand Wei J X.2000.Heliumand argon isotopic components offluidinclusions and tracing to the source of metallogenic fluidsin theDashuigou telluriumdeposit of Sichuan Province[J].Acta Geosicien-tia Sinica,21(1):58-61(in Chinese with English abstract).
Mao J W,Xie G Q,Li X F,Zhang C Qand Mei Y X.2004b.Mesozoiclarge scalce mineralization and multiple lithospheric extension insouth China[J].Earth Science Frontiers,11(1):45-54(in Chinesewith English abstract).
Mao J W,Zhang Z C and Zhang Z H.1999.Re-Os isotopic dating ofmolybdenites in the Xiaoliugou W(Mo)deposit in the northern Qi-lian moutains andits geological significance[J].Geochimica et Cos-mochimica Acta,63(11-12):1815-1818.
Qu WJ and Du A D.2003.Highly precise Re-Os dating of molybdeniteby ICP-MS with carius tube sample digestion[J].Rock and MineralAnalysis,22(4):254-257(in Chinese with English abstract).
RenY C,Cheng M Qand Wang C C.1986.Characteristics and verticalzoning of tungsten bismuth minerals in the Pangushan quartz veintype tungsten deposit of Jianxi province[J].Mineral Deposits,5(2):63-74(in Chinese with English abstract).
Ren Y C.1998.Restudy of bismuth sulfosalt mineralsin Pangushan wol-framquartz vein deposit,Jianxi Province[J].Contributions to Ge-ology and Mineral Resources Research,13(4):1-17(in Chinesewith English abstract).
Shirey S B and Walker R.J.1995.Carius tube digestion for low-blankrhenium-osmiumanalysis[J].Anal.Chem.,67:2136-2141.
Smoliar MI,Walker RJ and Morgan J W.1996.Re-Os ages of groupⅡA,ⅢA,ⅣAandⅥBiron meteorites[J].Science,271:1099-1102.
Tan YJ,Tong Q Q,Pi J M,et al.2002.Geological-geochemical fea-tures of ore-near hydrothermal alteration rocks in Pangushan tung-sten deposit[J].China Tungsten Industry,17(5):21-26(in Chi-nese with English abstract).
Wang X D,Ni P,Zhang BSand Wang T G.2010.Fluidinclusionstud-ies of the Pangushan quartz-vein type tungsten deposit in southernJiangxi Province[J].Acta Petrologica et Mineralogical,29(5):539-550(in Chinese with English abstract).
Xu J X.2009.Research on metallogenic series of ore deposit andits met-allogenic rulein Gannanregion-the east part of Nanling[D].Beijing:Chinese Academy of Geological Sciences.233p(in Chinese withEnglish abstract).
Xu Y,Zhu D B,Lai Z J,et al.2006.Geological characteristics and re-gional metallogenic regulation of Pangushan-Tieshanlong ore districtin Jianxi Province[A].In:Chen Y C,ed.Preceedings of8th Na-tional Conference of Mineral Deposits,China.The8th NationalConference of Mineral Deposits,China[C].Beijing:Geol.Pub.House.610-612(in Chinese).
Xu Y Gand Zeng Z L.2006.Division of Wand Sn multimetal mineral-ization region and its ore-searching direction in South Jiangxi[J].Resources Survey&Environment,27(4):290-296(in Chinesewith English abstract).
Ye J Y,Deng G Z,Pi J M,et al.2000.An analysis onthe characteris-tics of deep deposit of Pangushan tungsten mine and the vistas ofprospecting[J].China Tungsten Industry,15(4):17-19(in Chi-nese with English abstract).
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