ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
湖南古台山金锑矿床成矿流体He-Ar、Sr同位素地球化学及深部找矿意义
  
关键词:deep prospecting  He-Ar isotope  Sr isotope  source of ore-forming fluid  Gutaishan Au-Sb deposit  Xuefeng arc structure belt
基金项目:国家重点研发计划“深地资源勘查开采”重点专项课题(编号: 2017YFC0601506);湖南省自然资源厅科研项目(编号: 2017-03; 2019-02);湖南省地质院科研项目(编号: 201701; 2017-01-01; 201902-01; 201912)
作者单位E-mail
孙骥 湖南省地质调查院 410014679@qq.com 
周超 湖南省地质调查院  
陆文 湖南省地质调查院  
郭爱民 湖南省地质调查院  
肖荣 湖南省地质调查院  
隗含涛 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室  
谭仕敏 湖南省地质调查院
中南大学地球科学与信息物理学院 
 
贾朋远 湖南省地质调查院  
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摘要:
He-Ar-Sr Isotope Geochemistry of Ore-forming Fluids in the Gutaishan Au-Sb Deposit in Hunan Province and Its Significance for Deep Prospecting
      The Gutaishan quartz vein type gold-antimony deposit is a representative deposit in the middle of Xuefeng arc structure belt. The deposit, located in the external contact zone of Baimashan composite granite mass, is hosted within Nanhua Changan Formation and Qingbaikouan Wuqiangxi Formation. This paper reports He-Ar and Sr isotopic data of fluid inclusions trapped by arsenopyrite and quartz, respectively. It is shown that the 3He/4He ratios are in the range of 0.011~0.038 Ra, and 40Ar/36Ar ratios vary from 414.4 to 732.6. The results suggest that the ore-forming fluids were dominated by continental crust fluids and some meteoric water in the metallogenic process. 87Rb/86Sr ratios are in the range of 0.013~0.956, and 87Sr/86Sr ratios are in the range of 0.725 29 ~ 0.732 45. Calculation shows that the initial 87Rb/86Sr ratio was 223.6 Ma (i.e. ISr-223.6) when the deposit was formed. The ISr-223.6 values range from 0.723 60 to 0.731 67, with an average of 0.727 44. A comparison with the associated lithologies of Baimashan granite mass, Banxi Group and Lengjiaxi Group shows that the ore-forming fluids could not merely sourced from the Indosinian granitoids. Instead, it is shown that Indosinian granitoids provided ore fluids which upwardly moved and interacted with the underlying sedimentary rocks to form the Gutaishan Au-Sb deposit. The isotope geochemical characteristics of He-Ar reveal that, in prospecting for resources in Banxi Group, the underlying strata of the Chang’an Formation have better potential than the upper strata.
SUN Ji,ZHOU Chao,LU Wen,GUO Ai-min,XIAO Rong,WEI Han-tao,TAN Shi-min,JIA Peng-yuan.2020.He-Ar-Sr Isotope Geochemistry of Ore-forming Fluids in the Gutaishan Au-Sb Deposit in Hunan Province and Its Significance for Deep Prospecting[J].Acta Geoscientica Sinica,41(2):267-279.
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