Re-Os precise dating of pyrite from the Xinqiao Cu-Au-Fe-S Deposit in Tongling.Anhui and its implications for mineralization
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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.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.
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Key words:
- Re-Os isotopic dating /
- Pyrite /
- The Xinqiao Ore Deposit /
- Tongling in Anhui /
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