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玉龙斑岩铜矿带莽总含矿斑岩体岩石学特征及锆石U-Pb年龄研究

, PP. 300-306

Keywords: 斑岩铜钼矿床,成矿年龄,钾质碱性岩,西藏

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Abstract:

莽总斑岩铜钼矿床位于玉龙斑岩铜矿带中部,含矿岩体侵入下二叠统和上三叠统火山岩和硅质沉积岩中。含矿岩体出露面积约0.27km2,普遍发生蚀变,可分为早晚两个阶段。本文分析了含矿岩体化学组成及用锆石LA?ICP?MSU?Pb年龄分析斑岩体形成时代。早阶段岩体主要为花岗闪长斑岩,晚阶段岩体为石英二长斑岩及碱长花岗斑岩,晚阶段岩体相对富SiO2及K2O。莽总含矿斑岩体锆石LA?ICP?MSU?Pb年龄为(37.6±0.2)Ma,MSWD=1.41。据莽总含矿岩体形成时代及结合藏东地区在始新世至渐新世时的构造环境,提出莽总含矿岩体形成于扭压构造背景,和印度板块与欧亚板块产生的左行走滑断裂活动有关。

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