Pseudomorphic replacement of single calcium carbonate crystals by polycrystalline apatite

During chemical weathering and natural hydrothermal reactions, apatite can form by replacing calcium carbonates. In hydrothermal experiments in which aragonite and calcite single crystals have been reacted with phosphate solutions, the carbonates are replaced by polycrystalline hydroxylapatite (HAP)...

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Main Authors: Kasioptas, A., Perdikouri, C., Putnis, Christine, Putnis, Andrew
Format: Conference Paper
Published: 2008
Online Access:http://hdl.handle.net/20.500.11937/14216
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author Kasioptas, A.
Perdikouri, C.
Putnis, Christine
Putnis, Andrew
author_facet Kasioptas, A.
Perdikouri, C.
Putnis, Christine
Putnis, Andrew
author_sort Kasioptas, A.
building Curtin Institutional Repository
collection Online Access
description During chemical weathering and natural hydrothermal reactions, apatite can form by replacing calcium carbonates. In hydrothermal experiments in which aragonite and calcite single crystals have been reacted with phosphate solutions, the carbonates are replaced by polycrystalline hydroxylapatite (HAP). In both cases the crystals have retained their overall morphology while their compositions have changed significantly. The HAP appears to have a crystallographic relationship to the parent carbonate crystals. The textural relationships are consistent with an interface-coupled dissolution-precipitation mechanism. Structural relationships and relative molar volumes and solubilities appear to be factors that greatly affect replacement reactions. © 2008 The Mineralogical Society.
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spelling curtin-20.500.11937-142162017-09-13T14:05:40Z Pseudomorphic replacement of single calcium carbonate crystals by polycrystalline apatite Kasioptas, A. Perdikouri, C. Putnis, Christine Putnis, Andrew During chemical weathering and natural hydrothermal reactions, apatite can form by replacing calcium carbonates. In hydrothermal experiments in which aragonite and calcite single crystals have been reacted with phosphate solutions, the carbonates are replaced by polycrystalline hydroxylapatite (HAP). In both cases the crystals have retained their overall morphology while their compositions have changed significantly. The HAP appears to have a crystallographic relationship to the parent carbonate crystals. The textural relationships are consistent with an interface-coupled dissolution-precipitation mechanism. Structural relationships and relative molar volumes and solubilities appear to be factors that greatly affect replacement reactions. © 2008 The Mineralogical Society. 2008 Conference Paper http://hdl.handle.net/20.500.11937/14216 10.1180/minmag.2008.072.1.77 restricted
spellingShingle Kasioptas, A.
Perdikouri, C.
Putnis, Christine
Putnis, Andrew
Pseudomorphic replacement of single calcium carbonate crystals by polycrystalline apatite
title Pseudomorphic replacement of single calcium carbonate crystals by polycrystalline apatite
title_full Pseudomorphic replacement of single calcium carbonate crystals by polycrystalline apatite
title_fullStr Pseudomorphic replacement of single calcium carbonate crystals by polycrystalline apatite
title_full_unstemmed Pseudomorphic replacement of single calcium carbonate crystals by polycrystalline apatite
title_short Pseudomorphic replacement of single calcium carbonate crystals by polycrystalline apatite
title_sort pseudomorphic replacement of single calcium carbonate crystals by polycrystalline apatite
url http://hdl.handle.net/20.500.11937/14216