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《GEOTECTONICA ET METALLOGENIA》 2000-03
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FLUID INCLUSION CHARACTERISTICS AND ITS METALLOGENIC SIGNIFICANCE OF THE DAPINGZHANG CU- POLYMETAL DEPOSIT IN SIMAO,WESTERN YUNNAN

LI Feng, ZHUANG Feng- liang ( Dept. of Earth Science,Kunming Univ.of Science and Technol.,Kunming 650093,China)  
The Dapingzhang Cu- polymetal deposit was composed of massive sulfide ore beds and veinlet- disseminated sulfide orebodies.Compared with the former,the inclusion in the latter was characterized by its complex assemblage in types,and higher homogenization temperature,salinity and trapped pressure.Such variations in different orebodies were related to the evolution of ore- forming solutions.Based on the studies of composition,H- and O- isotopes of fluid inclusions,it can be deduced that ore- forming fluid was characterized as being rich in K+ ,Na+ ,Cl- ,,F- ,CO2 and CO,and belongs to the K- type solution,epi- to mesothermal in nature,moderately salinity and high pressure,mainly derived from sea water mixed with magmatic water.
【Fund】: 云南省自然科学基金资助项目!(97D031M)
【CateGory Index】: P611
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