The effect of fluid composition on the mechanism of the aragonite to calcite transition

Experiments 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 spectrosco...

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Main Authors: Perdikouri, C., Kasioptas, A., Putnis, Christine, Putnis, Andrew
Format: Conference Paper
Published: 2008
Online Access:http://hdl.handle.net/20.500.11937/39422
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author Perdikouri, C.
Kasioptas, A.
Putnis, Christine
Putnis, Andrew
author_facet Perdikouri, C.
Kasioptas, A.
Putnis, Christine
Putnis, Andrew
author_sort Perdikouri, C.
building Curtin Institutional Repository
collection Online Access
description Experiments 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. © 2008 The Mineralogical Society.
first_indexed 2025-11-14T08:58:40Z
format Conference Paper
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institution Curtin University Malaysia
institution_category Local University
last_indexed 2025-11-14T08:58:40Z
publishDate 2008
recordtype eprints
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spelling curtin-20.500.11937-394222017-09-13T14:24:48Z The effect of fluid composition on the mechanism of the aragonite to calcite transition Perdikouri, C. Kasioptas, A. Putnis, Christine Putnis, Andrew Experiments 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. © 2008 The Mineralogical Society. 2008 Conference Paper http://hdl.handle.net/20.500.11937/39422 10.1180/minmag.2008.072.1.111 restricted
spellingShingle Perdikouri, C.
Kasioptas, A.
Putnis, Christine
Putnis, Andrew
The effect of fluid composition on the mechanism of the aragonite to calcite transition
title The effect of fluid composition on the mechanism of the aragonite to calcite transition
title_full The effect of fluid composition on the mechanism of the aragonite to calcite transition
title_fullStr The effect of fluid composition on the mechanism of the aragonite to calcite transition
title_full_unstemmed The effect of fluid composition on the mechanism of the aragonite to calcite transition
title_short The effect of fluid composition on the mechanism of the aragonite to calcite transition
title_sort effect of fluid composition on the mechanism of the aragonite to calcite transition
url http://hdl.handle.net/20.500.11937/39422