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从金在地球中各部分的分布量可知,金是富集在地球深部的一种深成元素,通过岩浆活动和热液作用,使金从地幔物质中被携带至地壳上部并富集成矿。本文探讨在岩浆活动和热液作用过程中,有关金的地球化学及成矿作用问题。
From the distribution of gold in various parts of the earth, gold is a deep element enriched in the Earth’s deep earth. Gold is carried from the mantle material to the upper part of the crust and enriched in mineralization through magmatic activities and hydrothermal fluids. This article explores the geochemical and mineralization implications of gold during magmatic activities and hydrothermal processes.