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- W2326011729 startingPage "232" @default.
- W2326011729 abstract "The Kômori Ultrabasic Mass is located in the northern side of the Maizuru Zone, Kyoto Prefecture. It is mainly composed of serpentinized dunite being accompanied with such rocks as peridotite, pyroxenite, gabbro, diabase and albitite. At Komori mine, the writer found apophyllite in a druse of albitite in serpentinite mass. Near the Komori ore mineral deposit, serpentinization is remarkably observed. Apophyllite crystals are colorless and their maximum size is 2mm in length. The optical properties are variable; uniaxial positive, uniaxial negative or biaxial positive; these crystals coexist in a druse and the uniaxial positive crystals are often enclosed regularly in the uniaxial negative crystals. Refractive indices and X-ray powder patterns are well coincident with data of apophyllite so far reported. Thermal analysis data are also shown in this paper." @default.
- W2326011729 created "2016-06-24" @default.
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- W2326011729 date "1967-01-01" @default.
- W2326011729 modified "2023-09-25" @default.
- W2326011729 title "Apophyllite found in the Kômori Ultrabasic Mass" @default.
- W2326011729 cites W2799196682 @default.
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- W2326011729 doi "https://doi.org/10.2465/ganko1941.57.232" @default.
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