Abstract:Izu Peninsula in central Japan, the northern tip of the Izu-Bonin arc, hosts numerous epithermal Au-Ag vein deposits of low-sulfidation style. All have similar vein textures, mineralogy, and alteration. Geochemical data from fluid inclusions in vein quartz, the mineralogy and mineral chemistry of alteration, and stable isotope data indicate that auriferous hydrothermal activity occurred under subaerial conditions. The K-Ar ages of auriferous vein minerals are <1.5 Ma, indicating that the mineralization took pl… Show more
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