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低温热液条件下有机质富集金机理的实验研究 总被引:13,自引:0,他引:13
本文在低温(40—200℃)热液条件下,对不同成熟度的有机质与含金溶液[AuCl_4~-,Au(HS)_2~-]之间的相互作用进行了实验研究。研究观察到在低温热液体系中有机质直接参与了从含金溶液中将游离的金离子固定下来的作用。有机质从溶液中富集金可认为有两种不同性质的作用:第一种是在早期沉积成岩作用阶段(T<120°)时,有机质与含金热液主要发生凝聚作用,使溶液中的金由离子状态从无机相转化到有机相中;第二种是在变生或变质作用阶段(T>120℃)时,有机质与含金热液主要发生氧化还原沉淀作用,还原作用的结果导致元素金的沉淀,同时有机质被氧化、分解。 相似文献
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Thermal simulation experiments were conducted to understand the productivity of hydrocarbons andtheir nature. It is shown by the experimental results that coal resinite has a high productivity of hydro-carbons and may be a good source rock, resulting in light oils of low maturity in early stage. Naturalgases generated from coal resinite are rich in high molecular weight gas hydrocarbons (C_2~+), up to 19%(V/V). So, if natural gases were generated from coal formation which is rich in resinites, they cannotbe recognized as dry gases as normal. Characteristics of liquid hydrocarbons generated from coal resinitesare: (i) main composition of aromatics in extracts, of which the amount will increase with increasingmaturity; (ii) major compounds of diterpenoids in aliphatics. 相似文献
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