| Reference Type | Journal (article/letter/editorial) |
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| Title | The oriented transformation of aragonite into calcite |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Dasgupta, D. R. | Author |
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| Year | 1964 (June) | Volume | 33 |
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| Issue | 265 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_33/33-265-924.pdf+ |
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| DOI | doi:10.1180/minmag.1964.033.265.09Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5803 | Long-form Identifier | mindat:1:5:5803:6 |
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| GUID | 0 |
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| Full Reference | Dasgupta, D. R. (1964) The oriented transformation of aragonite into calcite. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (265) 924-928 doi:10.1180/minmag.1964.033.265.09 |
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| Plain Text | Dasgupta, D. R. (1964) The oriented transformation of aragonite into calcite. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (265) 924-928 doi:10.1180/minmag.1964.033.265.09 |
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| In | (1962) Mineralogical Magazine Vol. 33 (265) Mineralogical Society |
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| Abstract/Notes | SummaryThe oriented transformation of aragonite to calcite has been studied by X-rays. The [100], [110], and [001] directions of aragonite become [101̄0], [011̄0], and [0001] of calcite. The transformation was completed by a re-orientation of the CO3 groups about the [001] direction of aragonite through an angle of 30°, different rows of CO3 being turned in opposite directions, together with a displacement along the same direction. The layers of Ca ions also are shifted along the basal plane of calcite so that their arrangement perpendicular to the [0001] direction of calcite becomes ABCABCA… instead of ABABABA… as in aragonite. |
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