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《GEOLOGY-GEOCHEMISTRY》 1997-01
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ORGANIC MATTER IN HYDROTHERMAL ORE-FORMING FLUID

Zhuang Hanping; Lu Jialan (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Wushan, Guangzhou, 510640)Wen Hanjie ;Mao huahai (Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550002)  
The predominant organic matter in hydrothermal ore-forming fluid varies with temperature from humic substance (t 50℃), carboxylic acids (t = 80 ~ 140℃), crude oil (t = 120 ~ 180℃), to water-soluble mehane (t = 180 ~300℃). Humic substance plays an important role in the formation of prime ore source. Humic substance may be responsible for reducing the diagenetic environment due to its deoxidization when condensating into kerogen, and this environmnt is favorable to protecting metal elements from being dispersed during the diagenesis of ore source.Carboxylic acids are derived from kerogen at the early stage of evolution. Oilfield brines which are rich in such organic acids may be oreforming fluid responsible for the MVT Ph-Zn deposits. When reaching a certain degree of maturation,crude oil may be an important organic composition of hydrothermal ore-forming fluids of gold and mercury. And for low-middle temperature ore-forming fiuids of meals such as Cu, U, and Au, water-soluble methane tnay be a main organic constituent: The evolution stage of organic matter in sedimentary rocks results in the type of organic componerits in fluids, and the mineralizing differentiation of metals may be attributed to sedimentary formation type, partitioning coefficients of metals between oil and water, and tectonic background.
【CateGory Index】: P59
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