| Reference Type | Journal (article/letter/editorial) |
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| Title | The effect of fluid composition on the mechanism of the aragonite to calcite transition |
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| Journal | Mineralogical Magazine |
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| Authors | Perdikouri, C. | Author |
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| Kasioptas, A. | Author |
| Putnis, C. V. | Author |
| Putnis, A. | Author |
| Year | 2008 (February) | Volume | 72 |
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| Issue | 1 |
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| Publisher | Mineralogical Society |
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| DOI | doi:10.1180/minmag.2008.072.1.111Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 243796 | Long-form Identifier | mindat:1:5:243796:9 |
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| GUID | 0 |
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| Full Reference | Perdikouri, C., Kasioptas, A., Putnis, C. V., Putnis, A. (2008) The effect of fluid composition on the mechanism of the aragonite to calcite transition. Mineralogical Magazine, 72 (1) 111-114 doi:10.1180/minmag.2008.072.1.111 |
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| Plain Text | Perdikouri, C., Kasioptas, A., Putnis, C. V., Putnis, A. (2008) The effect of fluid composition on the mechanism of the aragonite to calcite transition. Mineralogical Magazine, 72 (1) 111-114 doi:10.1180/minmag.2008.072.1.111 |
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| Abstract/Notes | AbstractExperiments were performed to investigate the transformation of natural aragonite crystals to calcite by reaction with aqueous solutions of calcium carbonate at hydrothermal conditions for different periods of time. X-ray powder diffraction (XRD), scanning electron microscopy (SEM), Raman spectroscopy and Laser ablation inductively coupled mass spectrometry (LA-ICP-MS) were used to characterize the reaction product. The results indicate that the replacement of aragonite by calcite follows an interface-coupled dissolution-precipitation mechanism. |
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