结果显示:该岩石属于钙碱性系列,富集轻稀土元素(LREE)和大离子亲石元素(Rb、U、Th),明显亏损重稀土元素(HREE)和高场强元素(Nb、Ta),表现出岛弧岩石的特征且源于亏损地幔,洋壳俯冲作用过程中地壳物质增生的重要组成的部分。…
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研究表明玄武岩首先风化形成蒙皂石族粘土矿物，在此过程中稀土元素没有明显的分馏作用，强风化的玄武岩重稀土元素强烈亏损；
It is concluded that the half-weathered basalts have not distinct REE fractionation and strong weathered basalts had HREE loss in the process of the basalts weathered to form smectite family minerals.
稀土元素球粒陨石标准化曲线显示轻稀土富集重稀土亏损；
The standard curve of chondrite of rare earth element reveals a deficit of light rare earth enriched the heavy one;
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