日本 大谷鑛山産 pyrrhotite의 性質

Polymorphic variations of pyrrhotite as related to tungsten-tin-copper mineralization at the Ohtani mine, Japan

The ore deposit of the Ohtani mine is one of representatives of plutonic tungsten-tin veins related genetically to acidic magmatism of Late Cretaceous in the Inner zone of Southwest Japan. Based on macrostructures of vein filling, three major mineralization stages are distinguished by major tectonic breaks. The constituents of ore minerals are scheelite, cassiterite, chalcopyrite, pyrrhotite, sphalerite, with small amounts of cubanite, stannite, galena, native bismuth, bismuthinite, arsenopyrite and pyrite. The relationship between the polymorphic variations of pyrrhotite and the kinds of the associated characteristic of ore mineral, in relation with hypogene mineralization, has been demonstrated. Pyrrhotite of stage Ⅰ is predominantly of the hexagonal phase (Hpo＞Mpo). Pyrrhotite of stage Ⅱ is mainly of the monoclinic phase (Hpo≤Mpo). Pyrrhotite of stage Ⅲ is a single monoclinic phase (Hpo≪Mpo). The compositions of the hexagonal pyrrhotite decrease in Fe content ranging from 47.44 atom % Fe in stage Ⅰ to 46.88 atom % Fe in stage Ⅲ.