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

American Mineralogist; October 2000; v. 85; no. 10; p. 1383-1389
© 2000 Mineralogical Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
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 Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (11)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Hassan, I.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Transmission electron microscopy and differential thermal studies of lazurite polymorphs

Ishmael Hassan*

Department of Earth and Environmental Sciences, University of Kuwait, P.O. Box 5969, Safat, 13060, Kuwait

Correspondence: * E-mail: ishmael{at}kuc01.kuniv.edu.kw

Transmission electron microscopy (TEM) and thermal (DTA-TG) analyses of lazurite, (Na,Ca)8[Al6Si6O24](SO4,S)2, indicate three forms: cubic, modulated, and orthorhombic. Cubic lazurite contains mainly [Na3Ca·SO4]3+ clusters that are disordered together with the O1 and O2 oxygen atoms, and no satellite reflections occur. In the modulated lazurite structure, [Na3Ca·SO4]3+ and [Na3Ca·S]3+ clusters are ordered and possibly cause ordering of the framework oxygen atoms on the O1 and O2 positions and produce satellite reflections. Different ordering of these clusters gives an orthorhombic supercell with parameters of 2d110 x 6d1Formula 0 x c with respect to the cubic subcell. The DTA-TG study indicates that the orthorhombic to the modulated phase transition occurs at a peak temperature of 489 °C. A single-crystal fragment of lazurite may contain all three phases, as was observed by TEM in this study. Such intergrowths indicate a continuous framework with different regions of the crystal containing different ordering and chemistries. Two new lazurite superstructures were observed with dimensions of 6d110 x 3d001, and 3d112 x 3dFormula11 with respect to the cubic subcell.




This article has been cited by other articles:


Home page
Can MineralHome page
S. M. Antao, I. Hassan, and J. B. Parise
CHROMATE ALUMINATE SODALITE, Ca8[Al12O24](CrO4)2: PHASE TRANSITIONS AND HIGH-TEMPERATURE STRUCTURAL EVOLUTION OF THE CUBIC PHASE
Can Mineral, August 1, 2004; 42(4): 1047 - 1056.
[Abstract] [Full Text] [PDF]


Home page
Mineral MagHome page
A. Di Muro, E. Bonaccorsi, and C. Principe
Complex colour and chemical zoning of sodalite-group phases in a hauynophyre lava from Mt. Vulture, Italy
Mineralogical Magazine, August 1, 2004; 68(4): 591 - 614.
[Abstract] [Full Text] [PDF]


Home page
Mineral MagHome page
I. Hassan, I. Hassan, S. M. Antao, and J. B. Parise
Hauyne: phase transition and high-temperature structures obtained from synchrotron radiation and Rietveld refinements
Mineralogical Magazine, June 1, 2004; 68(3): 499 - 513.
[Abstract] [Full Text] [PDF]


Home page
Can MineralHome page
S. M. Antao and I. Hassan
THERMAL BEHAVIOR OF SCAPOLITE Me79.6 AND Me33.3
Can Mineral, October 1, 2002; 40(5): 1395 - 1401.
[Abstract] [Full Text] [PDF]


Home page
Can MineralHome page
S. M. Antao, M. J. Duane, and I. Hassan
DTA, TG, AND XRD STUDIES OF STURMANITE AND ETTRINGITE
Can Mineral, October 1, 2002; 40(5): 1403 - 1409.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of America