Mineral paragenesis and fluid inclusion data of the Ohe polymetallic vein-type deposits, Hokkaido, Japan.
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The Ohe ore deposits, occurring in the Miocene volcanic pyroclastics and quartz diorite of the "Green Tuff" region in southwestern Hokkaido, belong to the epithermal fissure-filling vein-type of polymetallic character.<BR>This paper presents the data concerning the stages of mineralization, variation in metal content of the ores, ore mineralogy and fluid inclusions, mainly obtained for the representative Senzai vein.<BR>Four stages of mineralization can be discriminated based upon the structural and mineral paragenetic features of the vein. Among them Stages II and III represent the main mineralization, depositing major sulphides of Fe, Cu, Zn, Pb as well as rhodochrosite with various minor sulphides, Au-Ag minerals, Mn-minerals and wolframite. The Senzai vein has 6 major ore zones that have resulted from lateral and vertical changes in its mineralogy and metal content.<BR>The ranges of the homogenization temperature and salinity of fluid inclusions in the minerals of Stage II are 195°-314°C(259°C on the average), and 4.2-6.3wt.% (4.5wt.% on the average) equivalent to NaCl, respectively. The corresponding data for Stage III mineralization are 171°-285°C(211°C), and 1.6-3.1wt.% (2.5wt.%). Temperature gradients of the ore deposition are approximately 0.6°C and 1.5°C per 10 m at Stages II and III, respectively.<BR>The sulphur fugacity and the temperature estimated for a representative phase of the mineralization are in the range of 10<SUP> -15</SUP> to 10<SUP>-11</SUP> atm., and 187°-275°C, respectively.
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