TRANSFORMATION OF MFI TO BETA-QUARTZ AND COESITE UNDER HIGH-PRESSURE AND HIGH-TEMPERATURE

JOURNAL OF THE CHEMICAL SOCIETY-CHEMICAL COMMUNICATIONS（1993）

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摘要

The transformation of MFI to beta-quartz, stable at room temperature, and coesite stable under high pressure and high temperature, is observed; the quartz and coesite phases are characterized by X-ray powder diffraction, thermogravimetric analysis and differential thermal analysis.

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