广西德保铜锡矿床辉钼矿Re-Os同位素定年及对加里东期成矿的探讨
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引用本文:王永磊,王登红,张长青,屈文俊,胡艳春.2010.Molybdenite Re-Os isochron age of Debao Cu-Sn deposit in Guangxi and relation to Caledonian mineralization[J].Mineral Deposits,29(5):881~889
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Author NameAffiliation
王永磊,王登红,张长青 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开放实验室 
屈文俊 国家地质实验测试中心 
胡艳春 山东省第一地质矿产勘查院资源公司 
基金项目:本文得到中央级公益性科研院所基本科研业务费专项资金资助项目(K0907)和全国危机矿山接替资源找矿项目(桂东-粤西地区铅锌金等矿床成矿规律总结研究,项目编码20089946)的联合资助
中文摘要:广西德保铜锡矿床为一矽卡岩型矿床。笔者对采自该矿床的7件不同矿化类型的辉钼矿样品,进行了Re-Os同位素定年,获得的模式年龄为(429.5±5.9)~(440.0±6.9)Ma。其中,采自含矿石英脉的6件辉钼矿样品的Re-Os模式年龄加权平均值为(435.0±2.5)Ma,等时线年龄为(445±11)Ma,表明该地区曾于晚奥陶世—早志留世发生过成矿作用,是华南加里东运动的产物。文章提供了关于右江地区加里东期成矿作用的信息,深化了对该地区成矿演化历史的认识,进而强调了对于寻找钦甲式Cu_Sn矿床的意义。
中文关键词:地质学  Re-Os等时线  铜-锡矿床  加里东期  德保  广西
 
Molybdenite Re-Os isochron age of Debao Cu-Sn deposit in Guangxi and relation to Caledonian mineralization
Abstract:The Debao Cu_Sn deposit is a skarn type deposit. Seven molybdenite-bearing samples of different mineralizing types were selected for precise Re-Os dating, and the dating results yielded model ages ranging from (429.5±5.9) to (440.0±6.9) Ma. The molybdenite from quartz veins yielded an isochron age of (445±11) Ma, which indicates that mineralization took place in the Late Ordovician to Early Silurian period. The results provide the information of Caledonian mineralization and deepen the understanding of the ore-forming evolutionary history in Youjiang area. The authors hold that the significance of looking for Qinjia-type Cu-Sn deposits should be emphasized in Youjiang area.
keywords:geology, Re-Os isochron, Cu-Sn deposit, Caledonian, Debao, Guangxi
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