Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; August 1997; v. 82; no. 7-8; p. 677-681
This Article
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Order Hardcopy of Full Text via AGI/GeoRef
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Chrosch, J.
Right arrow Articles by Salje, E. K. H.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Anti-phase boundaries and phase transitions in titanite; an X-ray diffraction study

Jutta Chrosch, Ulrich Bismayer, and Ekhard K. H. Salje

University of Cambridge, Department of Earth Sciences, Cambridge, United Kingdom

X-ray diffraction rocking curves of titanite, CaTiSiO 5 , were measured using a novel high-resolution diffractometer. Three Bragg reflections were recorded as a function of temperature and their profiles analyzed in terms of a Gaussian Bragg peak and a diffuse scattering component with an overall Lorentzian shape. The temperature dependence of the Gaussian intensities of the rocking peaks of superstructure reflections, hkl with k+l odd, scale with the long-range order parameter as I infinity Q 2 infinity [T-T c ] (super 2beta ) , where beta = 0.14(1) is the effective order parameter exponent. The diffuse scattering intensity changes little with temperature at Tc -20 K. Strong diffuse scattering is found at T>T c with centers of their Lorentzian diffraction profiles shifted by Delta omega nearly equal 0.5 degrees with respect to the position of the equivalent Bragg peak. A second phase transition at 825 K is confirmed and the possibility of a third transition at approximately 1150 K is discussed.

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
Can MineralHome page
R. P. Liferovich, R. P. Liferovich, and R. H. Mitchell
SOLID SOLUTIONS OF NIOBIUM IN SYNTHETIC TITANITE
Can Mineral, October 1, 2006; 44(5): 1089 - 1097.
[Abstract] [Full Text] [PDF]


Home page
Mineral MagHome page
R. P. Liferovich and R. H. Mitchell
Crystal structure of a synthetic aluminoan tantalian titanite: a reconnaissance study
Mineralogical Magazine, February 1, 2006; 70(1): 115 - 121.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
R. Ellemann-Olesen and T. Malcherek
A high-temperature diffraction study of the solid solution CaTiOSiO4-CaTiOGeO4
American Mineralogist, August 1, 2005; 90(8-9): 1325 - 1334.
[Abstract] [Full Text] [PDF]


Home page
Can MineralHome page
R. P. Liferovich and R. H. Mitchell
COMPOSITION AND PARAGENESIS OF Na-, Nb- AND Zr-BEARING TITANITE FROM KHIBINA, RUSSIA, AND CRYSTAL-STRUCTURE DATA FOR SYNTHETIC ANALOGUES
Can Mineral, April 1, 2005; 43(2): 795 - 812.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
S. Rath, S. Rath, M. Kunz, and R. Miletich
Pressure-induced phase transition in malayaite, CaSnOSiO4
American Mineralogist, February 1, 2003; 88(2-3): 293 - 300.
[Abstract] [Full Text] [PDF]


Home page
Mineral MagHome page
T. Malcherek
Spontaneous strain in synthetic titanite, CaTiOSiO4
Mineralogical Magazine, December 1, 2001; 65(6): 709 - 715.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
M. Kunz, T. Arlt, and J. Stolz
In situ powder diffraction study of titanite (CaTiOSiO4) at high pressure and high temperature
American Mineralogist, October 1, 2000; 85(10): 1465 - 1473.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
S. A. Hayward, J. d. Cerro, and E. K.H. Salje
Antiferroelectric phase transition in titanite: Excess entropy and short range order
American Mineralogist, March 1, 2000; 85(3-4): 557 - 562.
[Abstract] [Full Text] [PDF]


Home page
Can MineralHome page
M. Zhang, E. K.H. Salje, T. Malcherek, U. Bismayer, and L. A. Groat
DEHYDRATION OF METAMICT TITANITE: AN INFRARED SPECTROSCOPIC STUDY
Can Mineral, February 1, 2000; 38(1): 119 - 130.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Mineralogical Society of America