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《JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY》 1997-01
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THE DEEP FLUID AND ITS ORE FORMING PROCESS OF THE AILAOSHAN GOLD METALLOGENIC BELT

He Mingyou, Hu Ruizhong (Institute of Geochemistry Academia Sinica, Guiyang)  
The deep fluid is a fluid of high temperature and high pressure from the depths, which contains a great quantity of mineralizers such as Cl -,CO 2 and S 2- . The gold metallogenic process is as follows. The deep fluid activates Au from the Au bearing bodies to be formed Au bearing fluid as it moves up along the intense permeable fault zone from the depths. In the Au bearing fluid, Au moves mainly as AuCl - 2,AuCl - 4,AuS - 2 ,AuS - 3 and AuSO 3- 3. The Au bearing fluid replaces strongly with wall rocks when it moves into ore forming environments. Au complex ions are resolved in replacement and enriched into the gold deposits.
【Fund】: 国家科委攀登计划资助“超大”项目
【CateGory Index】: P618.510.1
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