The transformation of MFI to β-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.
L. Xiaoyang, S. Wenhui, Z. Xudong and W. Yifeng, J. Chem. Soc., Chem. Commun., 1993, 891 DOI: 10.1039/C39930000891
To request permission to reproduce material from this article, please go to the Copyright Clearance Center request page.
If you are an author contributing to an RSC publication, you do not need to request permission provided correct acknowledgement is given.
If you are the author of this article, you do not need to request permission to reproduce figures and diagrams provided correct acknowledgement is given. If you want to reproduce the whole article in a third-party publication (excluding your thesis/dissertation for which permission is not required) please go to the Copyright Clearance Center request page.
Read more about how to correctly acknowledge RSC content.
Please wait while we load your content...