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本文主要通过对比分析研究热泉软泥中的金含量与有机质及含硫化合物的相关性。并测定泉水及软泥中含金量和软泥中有机碳含量，以及对抽提物中的饱和烃和芳烃族组分进行色谱—质谱分析，最后得出的结论：有机质的沉积环境为还原—强还原，有机质属于腐泥－腐殖型，接近和达到了成熟阶段。软泥中金含量与有机质的性质无明显相关关系，与有机碳含量也无明显相关关系，而与其成熟度相关密切。样品分析证实软泥中含硫化合物与金含量呈正相关性。对比分析了水及软泥中金含量，认为两者之间也无明显相关关系
This paper mainly through the comparative analysis of hot spring slime in the gold content and organic matter and sulfur compounds correlation. And determining the gold content in the spring water and slime and the organic carbon content in the slime, as well as the chromatographic-mass spectrometric analysis of the saturated and aromatic components in the extract. Finally, the conclusion is drawn that the depositional environment of the organic matter is reduction-strong Reduction, organic matter belongs to the sapropel-humus type, approaching and reaching the maturity stage. There is no significant correlation between the gold content in slime and the nature of organic matter, and there is no significant correlation between the gold content in slime and the organic carbon content, but closely related to its maturity. Sample analysis confirmed a positive correlation between sulfur compounds and gold content in slime. Comparative analysis of gold and water in the mud, that there is no significant correlation between the two