A Metastable Aluminosilica Compound for Aluminum and Water Transport to the Upper Mantle

It has been suggested that crystalline “phase egg,” AlSiO3OH, with a ratio Al/Si=1 could carry aluminum and water to the mantle but its natural occurrences are still speculative. An amorphous phase with a fixed and unique, deep metastable eutectic Al2Si2O7 composition was produced in laboratory expe...

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Main Authors: Frans J. M. Rietmeijer, Joseph A. Nuth
Format: Article
Language:English
Published: Wiley 2009-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2009/909431
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author Frans J. M. Rietmeijer
Joseph A. Nuth
author_facet Frans J. M. Rietmeijer
Joseph A. Nuth
author_sort Frans J. M. Rietmeijer
collection DOAJ
description It has been suggested that crystalline “phase egg,” AlSiO3OH, with a ratio Al/Si=1 could carry aluminum and water to the mantle but its natural occurrences are still speculative. An amorphous phase with a fixed and unique, deep metastable eutectic Al2Si2O7 composition was produced in laboratory experiments wherein conditions favored kinetically controlled formation of amorphous solids. This experimentally produced kaolinite-dehydroxylate is highly reactive and it is proposed as the precursor of phase egg in subducting slabs of crustal rocks. If so, metastable phases play a role in subduction zones and it then follows that the processes and resulting conditions in these environments can be nonuniform and discontinuous at least at micrometer scales.
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series International Journal of Geophysics
spelling doaj-art-cda6de357f3647e9b734bc39a6363e372025-02-03T01:32:54ZengWileyInternational Journal of Geophysics1687-885X1687-88682009-01-01200910.1155/2009/909431909431A Metastable Aluminosilica Compound for Aluminum and Water Transport to the Upper MantleFrans J. M. Rietmeijer0Joseph A. Nuth1Department of Earth and Planetary Sciences, University of New Mexico Albuquerque, NM 87131-0001, USAAstrochemistry Laboratory, Solar System Exploration Division, Code 691, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USAIt has been suggested that crystalline “phase egg,” AlSiO3OH, with a ratio Al/Si=1 could carry aluminum and water to the mantle but its natural occurrences are still speculative. An amorphous phase with a fixed and unique, deep metastable eutectic Al2Si2O7 composition was produced in laboratory experiments wherein conditions favored kinetically controlled formation of amorphous solids. This experimentally produced kaolinite-dehydroxylate is highly reactive and it is proposed as the precursor of phase egg in subducting slabs of crustal rocks. If so, metastable phases play a role in subduction zones and it then follows that the processes and resulting conditions in these environments can be nonuniform and discontinuous at least at micrometer scales.http://dx.doi.org/10.1155/2009/909431
spellingShingle Frans J. M. Rietmeijer
Joseph A. Nuth
A Metastable Aluminosilica Compound for Aluminum and Water Transport to the Upper Mantle
International Journal of Geophysics
title A Metastable Aluminosilica Compound for Aluminum and Water Transport to the Upper Mantle
title_full A Metastable Aluminosilica Compound for Aluminum and Water Transport to the Upper Mantle
title_fullStr A Metastable Aluminosilica Compound for Aluminum and Water Transport to the Upper Mantle
title_full_unstemmed A Metastable Aluminosilica Compound for Aluminum and Water Transport to the Upper Mantle
title_short A Metastable Aluminosilica Compound for Aluminum and Water Transport to the Upper Mantle
title_sort metastable aluminosilica compound for aluminum and water transport to the upper mantle
url http://dx.doi.org/10.1155/2009/909431
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