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矿床地质  2009 

与云南个旧超大型锡矿床有关的花岗岩锆石U-Pb定年及意义

Keywords: 地球化学,花岗岩,锆石U_Pb年龄,动力学背景,云南个旧

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Abstract:

云南个旧地区发育大量与成矿时空密切相关的火成岩,包括玄武岩、辉长岩、花岗岩和正长岩,花岗岩被认为是个旧地区与成矿关系最密切的侵入岩。文章首次采用LA_ICP_MS和SHRIMPU_Pb方法对研究区内的花岗岩进行了精确定年,数据表明,不同类型的花岗岩同时或近于同时形成。龙岔河似斑状花岗岩主要形成于(82.0±0.3)~(83.2±1.4)Ma,马拉格_松树脚似斑状花岗岩形成于(82.8±1.7)Ma,老厂似斑状花岗岩形成于(83.3±1.6)Ma,白沙冲等粒花岗岩形成于(77.4±2.5)Ma,均集中形成于晚白垩世。结合前人的研究成果和本次新获得的数据,矿区内岩浆作用发生的时限基本可以限定在76~85Ma之间,与整个华南西部地区成岩成矿时代吻合。年代学研究表明,个旧地区燕山晚期的构造背景与滇东南_桂西地区相同,而与红河断裂以西的藏南_三江锡矿带具有较明显的不同。

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