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安徽铜陵新桥Cu-Au-Fe-S矿床黄铁矿Re-Os定年及成矿意义
引用本文:谢建成,杨晓勇,杜建国,杜小伟,肖益林,屈文俊,孙卫东.安徽铜陵新桥Cu-Au-Fe-S矿床黄铁矿Re-Os定年及成矿意义[J].地质科学,2009,44(1):183-192.
作者姓名:谢建成  杨晓勇  杜建国  杜小伟  肖益林  屈文俊  孙卫东
作者单位:1. 中国科学技术大学地球和空间科学学院, 合肥, 230026; 2. 安徽省地质调查院, 合肥, 230001; 3. 国家地质实验测试中心, 北京, 100037; 4. 中国科学院广州地球化学研究所, 广州, 510640
基金项目:中国科学院知识创新工程项目 
摘    要:安徽铜陵地区是长江中下游Cu-Au-Fe-S成矿带中的一个重要成矿区,新桥大型Cu-Au-Fe-S矿床为其重要的矿床之一.运用Re-Os同位素定年方法对该矿床中矿石的黄铁矿进行了精确定年测定,首次获得了黄铁矿的Re-Os等时线年龄为126±11Ma,初始OS值1.2±1.9(MSWD=2.6),属早白垩世,代表了铁硫化物的成矿年龄.结合前人的精确同位素定年结果,认为铜陵地区存在两种成矿事件,一种是与Cu-Au-Mo矿有关的成矿事件,代表的铜钼金硫化物的成矿年龄为138.0~140.0 Ma;另一种与铁矿有关的成矿事件,代表的铁硫化物的成矿年龄为112.6~126 Ma.

关 键 词:Re-Os  同位素定年  黄铁矿  新桥矿床  安徽铜陵
收稿时间:2007-10-29
修稿时间:2007-10-29;

Re-Os precise dating of pyrite from the Xinqiao Cu-Au-Fe-S Deposit in Tongling.Anhui and its implications for mineralization
Xie Jiancheng,Yang Xiaoyong,Du Jianguo,Du Xiaowei,Xiao Yilin,Qu Wenjun,Sun Weidong.Re-Os precise dating of pyrite from the Xinqiao Cu-Au-Fe-S Deposit in Tongling.Anhui and its implications for mineralization[J].Chinese Journal of Geology,2009,44(1):183-192.
Authors:Xie Jiancheng  Yang Xiaoyong  Du Jianguo  Du Xiaowei  Xiao Yilin  Qu Wenjun  Sun Weidong
Institution:1. School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026; 2. Anhui Academy of Geological Survey, Hefei 230001; 3. National Research Center of Geoanalysis, Chinese Academy of Ceologicad Sciences, Beijing 100037; 4. Cuangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640
Abstract:The Tongling region of Anhui province is an important ore district of the famous MiddleLower Yangtze Cu-Au-Fe-S metallogenic belt in China.The Xinqiao Cu-Au-Fe-S ore deposit is a representative one in Tongling region.In this study,6 pyrite samples from pyrite ore were collected in Xinqiao Ore Deposit for Re-Os precise dating.The results yielded a Re-Os isochron age of 126±11 Ma with initial Os value being 1.2±1.9(MSWD=2.6),which recorded the ore-forming age of Fe-sulfide.To synthesize other isotopic datings, the paper thought that there exited two ore-forming events in Tongling region:one was related to Cu-Au-Mo deposits with ore-forming age being 138.0~140.0 Ma, and another was related to iron deposits with oreforming age being 112.6~126 Ma.
Keywords:Re-Os
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