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《Journal of Mineralogy and Petrology》 2011-01
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WU Hai-zhi,HAN Run-sheng,WU Peng TANG Guo,LIANG Xu-wen(Faculty of Land Resources Engineering,Kunming University of Science and Technology;Southwest Institute of Geological Survey,China Non-ferrous Metals Resource Geological Survey,Kunming 650093,China)  
The study and comparison of fluid inclusions with different texture,structure and mineralization intensities in the Haojiahe copper deposit in Yunnan Province revealed that their formation is closely related to the evolution of ore-forming fluids in different rock forming and ore forming stages.Three stages of ore-forming fluid are recorded during the formation of copper deposit.First is the rock-forming period(Th-homogeneous temperature:84 ℃~162 ℃),second is the main reworked period(Th:145 ℃~227 ℃) and the last is the secondary reworked period(Th:129 ℃~177 ℃).The salinity(NaCl) of fluid inclusions of these three stages ranges from 4% to 10%,the gaseous phase of fluid inclusions were mainly composed of H2O,and the minor compositions contained CH4 and CO2.Ore source bed and some lean ore bodies of this sandstone-type copper deposit formed by the evolution of fluid during the rock-forming period,at the place of highly mineralization degree can even form disseminated or lamellar ores.Reworking mineralization fluid was the further evolution on the base of the rock-forming period fluid,which formed the final ore body controlled by structure and some banded or vein rich ores.
【Fund】: 全国危机矿山重大专项(20089943);; 云南省高校成矿动力学与隐伏矿预测创新团队项目(2010);; 云南省应用基础研究项目(2010ZC013)
【CateGory Index】: P618.41
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