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本文研究了元岭金矿含金单矿物黄铁矿和方铅矿的一般特点和微量元素及其变化规律，并发现：黄铁矿和方铝矿微量元素含量由早至晚的变化显示出亲石元素→亲石铁族元素→亲硫铁族元素→高温亲硫元素→低温亲硫元素逐次富集的过程，这与围岩蚀变和成矿溶液的变化惊人地相似，热液演化在岩石和矿物中的表现一致，金富集发生在铁族和亲硫元素交代之间或亲硫元素交代的早期
In this paper, the general characteristics and trace elements of gold-bearing mono-mineral pyrites and galena in the Yuanling gold deposit are studied. The results show that the content of trace elements in pyrite and galena changes from morning to late Pro-stone elements → pro-ferrite elements → pro-ferrosulfide elements → high temperature pro-sulfur elements → low-temperature pro-sulfur elements, which is strikingly similar to the alteration of wall rock alteration and ore-forming solution. The same performance in rocks and minerals, gold enrichment occurs in the iron family and the pro-sulfur elements exchanged or pro-sulfur elements in the early exchange