Growth and ordering processes in synthetic hydrothermal anorthite |
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Authors: | J Copreaux M Gandais S -C Dujon |
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Institution: | 1. Laboratoire de Minéralogie-Cristallographie, associé au CNRS, Universités P. et M. Curie (Paris VI) et Paris VII, 4 Place Jussieu, 05, Paris Cedex, France 2. Laboratoire de Géologie de l'Ecole Normale Supérieure, associé au CNRS, 24 Rue Lhomond, F-75005, Paris, France
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Abstract: | Anorthite crystals were synthetized from gel under hydrothermal conditions (P=1000 bar, T=700° C) with run durations from 2 h to 110 days. The products were observed at room temperature by optical microscopy, X-ray
powder diffraction and transmission electron microscopy (TEM). It has been shown that crystallization progresses as a function of time as follows: from t=2 h to t=7 days, the proportion of amorphous material decreases from 80 to 0 percent; the average crystal size grows from 1 to 20
μm; the number of crystals per unit volume decreases from 2.1011 to 5.108cm−3, indicating substantial recrystallization. The average A1, Si state of order increases with time and reaches a steady state
after seven days. The crystals exhibit a core few micrometers in diameter and a rim whose width increases with time from 1
to 10 μm. The core, highly disordered in Al, Si, displays weak b reflexions and small antiphase domains (APDs), the rim, more ordered in Al, Si, differs from the core by sharp b reflexions and larger APDs extending radially.
Both macroscopic results and microscopic observations show that crystals grow by two successive processes: at first, nucleation
and growth from gel giving rise to the core, then recrystallization giving rise to the rim. |
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