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- W2328816920 abstract "Nine kinds of ore minerals and eleven kinds of gangue minerals are observed on examing ores from the Omine mine under a microscope as mentioned in the previous report. Of the ore minerals, chalcopyrite contained three, cubanite, four, pyrrhotite and sphalerite, two minerals formed by unmixing, so that at least the following eleven unmixing textures can be distinguised: 1) Banded or lattice-shaped cubanite in chalcopyrite. 2) Banded lamellar chalcopyrite in cubanite. 3) Curving hair-like or vermicular py ?? rhotite in chalcopyrite. 4) Vein-shaped or lamellar pyrrhotite in cubanite. 5) “Sphalerite star” in chalcopyrite. 6) Chalcopyrite emulsion in sphalerite. 7) Banded or lattice-shaped pentlandite in pyrrhotite. 8) Lamellar or lattice-shaped pentlandite in cubanite. 9) Lamellar or vein-shaped violarite in pyrrhotite. 10) Pyrrhotite emulsion in sphalerite. 11) Lamellar or lattice-shaped sphalerite in pyrrhotite. Of the above, 1), 3), 5), 6), and 7) have been reported from many mines, and have been proven as intergrowths formed by unmixing by means of thermal experiment, 4) and 10) are only assumed to represent unmixing textures but not yet confirmed experimentally. The others have not been noted in the past. They appear, to be unmixing textures under a microscope, but strictly speaking, their nature must be confirmed by future experiment." @default.
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- W2328816920 date "1953-01-01" @default.
- W2328816920 modified "2023-10-04" @default.
- W2328816920 title "On the Unmixing Intergrowths of the Copper Ores from the Ômine Mine" @default.
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- W2328816920 doi "https://doi.org/10.2465/ganko1941.37.9" @default.
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