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- W2025117556 abstract "Rainbow stone, or colored limestone consists of four portions which differ in its color and chemical composition. They are black colored portion due to manganese dioxide (micro-manganese nodules), reddish brown portion due to iron oxides, pale yellowish pink portion due to aluminosilicate and some other compounds, and white portion due to calcite and/or proto-dolomite. The color of Rainbow stone is controlled mainly by Fe2O3 and MnO2 contents. Electron probe micro analyses (EPMA) clarify the existence of micro-manganese nodules in the black portion with iron oxides in its nucleus. Rhombohedral crystals of dolomite are observed with calcite. NaCl crystals, which are confirmed by X-ray diffraction analysis and EPMA, are incorporated into proto-dolomite almost regardless of its color. This shows that proto-dolomite on Daito Islands could have been formed through the evaporation of concentrated sea water." @default.
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- W2025117556 date "1985-01-01" @default.
- W2025117556 modified "2023-10-16" @default.
- W2025117556 title "Geochemical studies on the color and chemical composition of Rainbow stone in Kita and Minami Daito Islands." @default.
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- W2025117556 doi "https://doi.org/10.2343/geochemj.19.59" @default.
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