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《Earth Science Frontiers》 2004-02
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NEW ADVANCES IN RESEARCH OF TRACE GASEOUS COMPOSITIONS IN FLUID INCLUSIONS AND THEIR APPLICATIONS AS INDICATORS OF ORE-FORMING FLUID SOURCES AND PROCESSES

SUN Xiao-ming~(1,2), WANG Min, XUE Ting~1, SUN Kai~1(1.Department of Earth Sciences, Sun Yat-sen University, Guangzhou 510275,China;2.State Key Laboratory of Mineral Deposit Research of Nanjing University,Nanjing 210093, China)  
The N_2-Ar-He system is used to indicate the source of the hot springs and ore-forming fluids,CO_2/CH_4-N_2/Ar system is used when the He-content is lower than the detection limit and the N_2-Ar-He system is not valid. CO_2-CH_4-H_2 system is used to identify the boiling in an open or a closed system. Generally an open system is favorable for metallogenesis. CO_2-CH_4-C_2H_6 system can be applied to indicate the contribution of magmatism in ore-forming processes and discriminate the sources of the ore-forming fluid. CH_4-C_2H_6-C_3H_8 system is used to indicate whether a long way and large scale ore-forming fluid migration occurred when the fluid contains light hydrocarbon related to the decomposition of kerogen. C_2H_6-C_3H_8-C_6H_6 system is good at indicating the tectonic environment of the ore-forming fluids, because the C_2 H_6/C_3H_8 ratio varies greatly in island arcs and rift tectonic settings. Taking Changkeng (Ag, Au) and Songxi (Ag, Sb) deposits in Guangdong Province, China as examples, the authors briefly introduce the respective application of these systems.
【Fund】: 国家自然科学基金资助项目 ( 4 0 173 0 2 5 ;49773 195 ;495 0 2 0 2 9;4992 82 0 1) ;; 国家重点基础研究发展规划 ( 973 )资助项目 ( 2 0 0 2CB412 610 ) ;; 国家教育部跨世纪人才培养计划基金资助项目
【CateGory Index】: P593;P611
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