Data of the fluid inclusion studies•which have been carried out up to date in Japan, are briefly summarized, and the result is discussed from the standpoint of mineral exploration. Homogenization tempera• tures of fluid inclusions in vein-type deposits of Tertiary and Late Cretaceous age, range between 130° and 360°C, but th…
Fluid inclusions in quartz phenocrysts of quartz porphyry, quartz veinlets cutting quartz porphyry, and quartz and sphalerite in ores, were studied by the heating-stage and freezing-stage methods. Polyphase fluid. inclusions carrying transparent cubic crys• tals were especially found …