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安徽铜陵新桥铜金矿床黄铁矿Rb/Sr同位素年龄数据——燕山晚期成矿作用的证据
引用本文:王彦斌,唐索寒,王进辉,曾普胜,杨竹森,蒙义峰,田世洪.安徽铜陵新桥铜金矿床黄铁矿Rb/Sr同位素年龄数据——燕山晚期成矿作用的证据[J].地质论评,2004,50(5):538-542.
作者姓名:王彦斌  唐索寒  王进辉  曾普胜  杨竹森  蒙义峰  田世洪
作者单位:1. 中国地质科学院地质研究所,北京,100037
2. 中国地质科学院矿产资源研究所,北京,100037
基金项目:国土资源部国际合作与科技司资助项目,地质大调查项目,国土资源部专项基金,20010209,200110000004,20010103,,,
摘    要:本文采用亚样品取样和Rb/Sr同位素方法对安徽铜陵新桥铜-硫铁-金矿床层状矿体矿石矿物--黄铁矿直接进行Rb-Sr等时线法测定,获得了112.6±7.8Ma的Rb-Sr等时线年龄,它代表了主成矿期成矿作用的时代.结合已有地质资料认为燕山晚期成矿作用在新桥铜-硫铁-金矿床的形成中居重要作用.

关 键 词:金矿床  黄铁矿  Rb-Sr等时线法  成矿作用  矿床地质  同位素年龄

Rb-Sr Dating the Pyrite of the Xinqiao Cu-S-Fe-Au Deposit, Tongling, Anhui Province
WANG Yanbin,TANG Suohan,WANG Jinhui,ZENG Pusheng,YANG Zhusen,MENG Yifeng,TIAN Shihong Institute of Geology,Chinese Academy of Geological Sciences,Beijing.Rb-Sr Dating the Pyrite of the Xinqiao Cu-S-Fe-Au Deposit, Tongling, Anhui Province[J].Geological Review,2004,50(5):538-542.
Authors:WANG Yanbin  TANG Suohan  WANG Jinhui  ZENG Pusheng  YANG Zhusen  MENG Yifeng  TIAN Shihong Institute of Geology  Chinese Academy of Geological Sciences  Beijing
Institution:WANG Yanbin,TANG Suohan,WANG Jinhui,ZENG Pusheng,YANG Zhusen,MENG Yifeng,TIAN Shihong Institute of Geology,Chinese Academy of Geological Sciences,Beijing, Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing
Abstract:Significant effort has been made in an attempt to date hydrotherrnal activity that generated the Xinqiao Cu-S-Fe-Au deposit in Tongling. New direct Rb-Sr dating of pyrite from the deposit provides direct timing constraints on sulfide and gold mineralization. Pyrite samples yield a Rb-Sr isochron age of 112. 6 + 7. 8Ma. It is concluded that the Xinqiao polymetallic deposit was formed by hydrotherrnal solutions related to late Yanshanian plutonism (110 Ma). Results obtained for the deposit indicate that the Rb-Sr geochronometer has a potential to directly date mineralization in stratabound sulfide deposits.
Keywords:Rb-Sr dating  pyrite  Tongling mineral district  Xinqiao Cu-S-Fe-Au deposit  Anhui
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