Abstract:Based on the study of inclusion typehomogenization temperature salinity pressure inclu sion composition and H.O isotopes, the authors consider that Xiayingfang gold deposit is characterized by typical porphyry-type deposit, Ore-forming fluid, which was mixed with a little of meteoric water in main metallogenic stage, mainly came from crust-mantle mis-melting magma. The rich ore district can be indicated by boiling inclusion group multifalies inclusion with daughter crystal and inclusion with richful CO2. Three dimensional space variety of homogenization temperature contour line can determain rich ore area and orebody occurence.
栾文楼, 于耀先. 河北平泉下营坊金矿床流体包裹体地球化学及其找矿意义[J]. 地质与资源, 1995, 4(3): 161-167.
Luan Wenlo, Yu Yaoxian. GEOCHEMISTRY OF FLUID INCLUSION OF XIAYINGFANG GOLD DEPOSIT IN PINGQUAN OF HEBEI PROVINCE AND ORE-SEARCHING SIGNIFICANCE. GEOLOGY AND RESOURCES, 1995, 4(3): 161-167.