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    安徽铜陵新桥铜-硫-铁-金矿床中石英闪长岩和辉绿岩锆石SHRIMP年代学及其意义

    SHRIMP U-Pb geochronology of the Xinqiao Cu-S-Fe-Au deposit in the Tongling ore district, Anhui

    • 摘要: 提要:对安徽铜陵新桥铜-硫-铁-金矿床区内的石英闪长岩和辉绿岩中的锆石分别进行了SHRIMP 精确定年研究,石英闪长岩中锆石206Pb/238U年龄为(140.4±2.2) Ma,辉绿岩中锆石的年龄较复杂,其中发现了元古代锆石颗粒,其锆石207Pb/206Pb年龄为(2 261±14) Ma, (1 612±8) Ma,(919±12) Ma,(831±17) Ma。另外还有一组早古生代年龄的锆石,锆石206Pb/238U年龄为(443±13) Ma。以上这些新资料说明该区可能存在元古代基底的信息,且燕山期岩浆活动对本区成矿具有重要意义。

       

      Abstract: Abstract:High-precision SHRIMP U-Pb dating was performed on zircon from quartz diorite and diabase in the Xinqiao Cu-S-Fe-Au deposit, Tongling ore district, Anhui. Zircon from quartz diorite yielded a 206Pb/238U age of (140.4±2.2) Ma, while the zircon age of diabase is relatively complex. Several Proterozoic zircon grains were found in diabase, which yielded 207Pb/206Pb ages of (2 261±14) Ma, (1 612±8) Ma, (919±12) Ma and (831±17) Ma. In addition, there is also a group of Early Paleozoic zircon grains, whose 206Pb/238U age is (443±13) Ma. The above new data give the information of the possible existence of Proterozoic basement in this district, and Yanshanian magmatism is of great significance for mineralization in the district.

       

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