The ore-forming fluid distribution and evolution of interstratified skarn copper-gold deposits in Shizishan ore-field of Tongling, Anhui Province
The studies on mineral inclusions have revealed that the ore-forming fluid distributed regularities in space and evolution consistently in time for the interstratified skarn copper-gold deposits in Shizishan ore-field of Tongling.Particularly, the migration of the ore- forming fluids is in the condition of equal temperature field in different mineralization stages. The mixing and evolution of two end-members fluids at least occur in mineralization process but mainly magmatic hydrothermal solution. All of the stratified skarn deposits were controlled by universal tectonicmagma activities.
ore-forming fluid distribution and evolution interstratifield skarn copper-gold deposit Shizishan ore-field of Tongling
Xiaochun Xu Sanming Lu Guozhen Chu Wentao Wu Shenlian Ren
School of Nature Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China
国际会议
第八届国际矿床地质会议(Proceedings of the Eighth Biennial SGA Meeting)
北京
英文
132-135
2005-08-18(万方平台首次上网日期,不代表论文的发表时间)