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地质论评  2009 

贵州罗甸晚二叠世辉绿岩及其区域构造意义

Keywords: 辉绿岩,地球化学特征,构造环境,罗甸地区

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Abstract:

黔东南罗甸辉绿岩为拉斑系列岩石,其主量元素以高TiO2(2.36%~2.57%)、高CaO(9.40%~10.31%)、低MgO(5.65%~6.93%),低碱且Na2O>K2O为特征;稀土含量(ΣREE=164.9×10-6~187.3×10-6)较高,反映轻稀土富集,重稀土亏损;Eu正异常(δEu=1.22~1.26),球粒陨石标准化配分曲线具有右倾分布特征。对辉绿岩中锆石进行的LA-ICP-MSU-Pb定年分析获得其谐和图下交点年龄为255.0±0.62Ma,代表岩体结晶时代。结合区域地质分析认为,罗甸辉绿岩可能起源于接近于原始的地幔橄榄岩的部分熔融作用,岩浆在快速上升过程中可能受到地壳物质的混染。罗甸辉绿岩具有与峨眉山玄武岩相似的地球化学特征,其形成年龄与峨眉山玄武岩的主喷发期基本同时。综合分析认为,黔东南晚二叠世辉绿岩是峨眉山玄武岩同质异相岩浆活动的产物,黔东南罗甸―望谟一带处于峨眉山玄武质岩浆活动的东部边缘地带。

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