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湖南龙山锑金矿床白云母~(40)Ar-~(39)Ar年代学及其意义初探
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  • 英文篇名:Preliminary study on muscovite ~(40)Ar-~(39)Ar geochronology and its significance of the Longshan Sb-Au deposit in Hunan Province
  • 作者:张志远 ; 谢桂青 ; 李惠纯 ; 李伟
  • 英文作者:ZHANG ZhiYuan;XIE GuiQing;LI HuiChun;LI Wei;MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences;304 Brigade,the Bureau of Geology for Nuclear Industry of Hunan Province;Faculty of Earth Resources,China University of Geosciences;
  • 关键词:40Ar-39Ar同位素年龄 ; 白云母 ; 龙山锑金矿床 ; 构造背景 ; 湘中地区
  • 英文关键词:40Ar-39Ar isotope age;;Muscovite;;Longshan Sb-Au deposit;;Tectonic framework;;Central Hunan Province
  • 中文刊名:YSXB
  • 英文刊名:Acta Petrologica Sinica
  • 机构:中国地质科学院矿产资源研究所,国土资源部成矿作用与资源评价重点实验室;湖南省核工业地质局三〇四大队;中国地质大学资源学院;
  • 出版日期:2018-09-15
  • 出版单位:岩石学报
  • 年:2018
  • 期:v.34
  • 基金:国家“973”计划项目(2014CB440902)资助
  • 语种:中文;
  • 页:YSXB201809003
  • 页数:13
  • CN:09
  • ISSN:11-1922/P
  • 分类号:37-49
摘要
龙山锑金矿是湘中Sb-Au矿集区内规模最大的脉状锑金矿床,但其精确的成矿时代尚未厘定。本次工作发现该矿床第Ⅰ成矿阶段的石英硫化物脉中发育少量的热液白云母。通过40Ar-39Ar年代学测定,确定了白云母的~(40)Ar-~(39)Ar同位素坪年龄为162. 5±1. 8Ma,相应的等时线年龄为161. 1±1. 2Ma(MSWD=1. 0),反等时线年龄为161. 1±1. 2Ma(MSWD=1. 0)。根据矿物共生组合特征,认为白云母的~(40)Ar-~(39)Ar坪年龄能代表龙山锑金矿床的成矿年龄。结合湘中地区其他锑(金)矿床的年代学研究成果,本文认为,该地区在155~162Ma之间有一次热液成矿事件,与南岭地区165~150Ma与花岗岩有关的钨锡多金属矿床的成矿时代相一致。湘中地区已有的S同位素地球化学和地球物理学资料表明,该地区锑金矿床的形成可能与岩浆作用有关,类似于南岭地区晚侏罗世钨锡多金属矿床的构造背景。
        The Longshan Sb-Au deposit is the largest lode-type Sb-Au deposit in the central Hunan Province Sb-Au oreconcentration area,while the precise geochronology has not been confirmed. This work found an amount of hydrothermal muscovite occurred in quartz sulfide veins in the first stage of mineralization. By the ~(40) Ar-~(39) Ar chronology study,we confirm that the muscovite yielded a ~(40) Ar-~(39) Ar plateau age of 162. 5 ± 1. 8 Ma,with an isochron age of 161. 1 ± 1. 2 Ma( MSWD = 1. 03) and an inverse isochron age of 161. 1 ± 1. 2 Ma( MSWD = 1. 01). Based on the characteristics of mineral assemblages,we infer that the ~(40) Ar-~(39) Ar system in muscovite remain to be closed with ore deposition,and constrain the formation of the Longshan Sb-Au deposit. In combination with geochronology research of other antimony( gold) deposits in the central Hunan Province,this paper argues that there was a relatively large hydrothermal mineralization event between the 155 ~ 162 Ma in this area. And the result is coincident with a large number of tungsten tin polymetallic deposits related to granite formed in 165 ~ 150 Ma in Nanling region. Integrated study of available S isotopic geochemistry and geophysical evidences,we conclude that the formation of Sb-Au deposits in central Hunan Province was related to the magmatism,similar to the tectonic background of the Late Jurassic tungsten tin polymetallic deposits in Nanling region.
引文
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