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

American Mineralogist; April 2002; v. 87; no. 4; p. 462-477
© 2002 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 (3)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Najorka, J.
Right arrow Articles by Heinrich, W.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Composition of synthetic tremolite-tschermakite solid solutions in amphibole + anorthite-and amphibole + zoisite-bearing assemblages

Jens Najorka*, Matthias Gottschalk and Wilhelm Heinrich

GeoForschungszentrum Potsdam, Telegrafenberg, 14473 Potsdam, Germany

The composition of synthetic amphiboles was investigated experimentally along the tremolite-tschermakite join in the system CaO-MgO-Al2O3-SiO2-H2O-Br2. Compositions of these amphiboles were studied within the phase assemblages: amphibole-anorthite-quartz-diopside (I), amphibole-anorthite-quartz-talc (II), amphibole-anorthite-quartz-enstatite (III), amphibole-anorthite-talc-clinochlore (IV), amphibole-zoisite-talc-quartz (V), and amphibole-zoisite-talc-clinochlore (VI). Assemblages were synthesized from oxide-hydroxide mixtures in the presence of a CaBr2-bearing solution between 600–800 °C and 200–2000 MPa. Solid phases were investigated using SEM, HRTEM, EMP, and XRD techniques. EMP data show that the amphiboles produced are solid solutions of the ternary system tremolite-tschermakite-cummingtonite. Enstatite, diopside, talc, and clinochlore showed small deviations from their respective end-member compositions due to incorporation of some Al.

The thermodynamic properties of the tschermakite end-member and the mixing properties along the tremolite-tschermakite join were extracted from corresponding exchange reactions of the unreversed synthesized phase assemblages I–VI. Various ideal mixing models were tested for Al-Mg and Al-Si substitution at octahedral M2 and M3 sites and at tetrahedral T1-sites. Best fits were obtained for a two-site coupled model, resulting in {Delta}fHts0 = –12528.3 ± 11.7 kJ/mol and Sts0 = 556.5 ± 12.0 J/(mol·K) for the tschermakite end-member. Similar calculations were carried out for magnesiohornblende, and values of {Delta}fHMghb0 = –12418.7 ± 5.9 kJ/mol and SMghb0 = 562.8 ± 6.1 J/(mol·K) were extracted. Calculated phase relations and amphibole compositions agree well with experimental data if the derived thermodynamic data of tschermakite and a two-site mixing model for Al incorporation in amphibole solid solutions are applied.




This article has been cited by other articles:


Home page
Reviews in Mineralogy and GeochemistryHome page
W. V. Maresch and M. Czank
The Significance of the Reaction Path in Synthesizing Single-Phase Amphibole of Defined Composition
Reviews in Mineralogy and Geochemistry, October 1, 2007; 67(1): 287 - 322.
[Full Text] [PDF]


Home page
American MineralogistHome page
S. Bhadra and A. Bhattacharya
The barometer tremolite + tschermakite + 2 albite = 2 pargasite + 8 quartz: Constraints from experimental data at unit silica activity, with application to garnet-free natural assemblages
American Mineralogist, April 1, 2007; 92(4): 491 - 502.
[Abstract] [Full Text] [PDF]


Home page
Reviews in Mineralogy and GeochemistryHome page
S. Poli and M. W. Schmidt
Experimental Subsolidus Studies on Epidote Minerals
Reviews in Mineralogy and Geochemistry, January 1, 2004; 56(1): 171 - 195.
[Full Text] [PDF]




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