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- W2380498430 abstract "The early stage fluid inclusions in the mineralized porphyry in contact zone (also on the edge of the breccia pipe) are dominated by CO_2-H_2O type,and the inclusions in none- or weakly mineralized porphyry from the inner rock body are by hypersaline H_2O-NaCl type.It illustrated that the fluid derived from alkali-rich magma had fractionated into CO_2-rich and hypersaline phases in its early stage,and the ore-forming metals were initially transplanted in the CO_2-rich phase,which occurred at the exterior of the fluid.Therefore,a conclusion might be drawn that the exo-contact zone and nearby was the favorable position for ore formation.The secondary fluid inclusions in quartz phanerocryst in altered rock samples from the inner rock body can approximately be divided into four generations.According to the result of microthermometry,estimation of the formation temperature and pressure,homogenization temperature-salty relation,and P-T plot of H_2O-NaCl system,the four generations of fluid inclusions reflected the change processes of environmental conditions (relative to the trapped fluids) and corresponding geological processes." @default.
- W2380498430 created "2016-06-24" @default.
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- W2380498430 date "2005-01-01" @default.
- W2380498430 modified "2023-09-25" @default.
- W2380498430 title "STUDY OF THE FLUID INCLUSIONS IN ALTERED PORPHYRES IN THE BEIYA GOLD DEPOSIT, WSTERN YUNNAN" @default.
- W2380498430 hasPublicationYear "2005" @default.
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