摘要
通过对成矿流体的无机成分、同位素等特征及有机成分的光学、谱学特征的分析，认为成矿流体是一种复杂的流体，至少由两种流体组成，一种是与地层有关的油田卤水（有机流体），另一种是含ＳＯ２－４的流体。此外，大气降水也参与了成矿，并从无机和有机相互联系的观点出发，探讨了两种流体相互作用的过程。
This paper deals with the inorganic components,organic components and isotopic characteristics of oreforming fluid in detail.Results show that the oreforming fluid is very complex.At least two kinds of fluids are included in the oreforming fluid.One is the organic fluid (oilfield water) related to strata,the other is inorganic fluid dominant in SO2-4.Besides,meteoric water also participates in mineralization.From the view of interconnection of organism and inorganism,the paper discusses the interaction process of the two kinds of fluids and indicates the microscopic prospecting markers.
出处
《地质科技情报》
CAS
CSCD
北大核心
1998年第2期51-54,共4页
Geological Science and Technology Information
基金
国家教委博士点基金
地矿部生物成矿重点学科生长点基金
关键词
金矿床
成矿流体特征
流体包裹体
金牙金矿床
Jinya gold deposit,characteristics of oreforming fluid,fluid inclusion
