ore-forming fluid evolution 成矿流体演化
Formation and evolution of granites in this region brought forth a great quantity of hydrothermal fluid and some of the ore-forming elements.
花岗岩的形成和演化为成矿带来了大量热流体及部分成矿元素。
The ore-forming fluid had weak reducibility. Race elements of arsenopyrite and pyrite were reduced by ore-forming fluid with the evolution. There were relatively high LREE and low HREE.
毒砂、黄铁矿微量元素含量呈现出随着成矿流体从早期到晚期的演化而减少，并普遍亏损高场强元素，富集LREE的特征；
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