Skip Navigation


Journal of Petrology Advance Access originally published online on October 21, 2005
Journal of Petrology 2006 47(2):385-408; doi:10.1093/petrology/egi079
This Article
Right arrow Full Text Freely available
Right arrow FREE Full Text (PDF) Freely available
Right arrow All Versions of this Article:
47/2/385    most recent
egi079v1
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Add to My Personal Archive
Right arrow Download to citation manager
Right arrow Search for citing articles in:
ISI Web of Science (13)
Right arrowRequest Permissions
Google Scholar
Right arrow Articles by WEI, C.
Right arrow Articles by POWELL, R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Social Bookmarking
 Add to CiteULike   Add to Connotea   Add to Del.icio.us  
What's this?

© The Author 2005. Published by Oxford University Press. All rights reserved. For Permissions, please e-mail: journals.permissions@oxfordjournals.org

Calculated Phase Relations in the System NCKFMASH (Na2O–CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O) for High-Pressure Metapelites

CHUNJING WEI1,* and ROGER POWELL2

1 MOE KEY LABORATORY OF OROGENIC BELTS AND CRUSTAL EVOLUTION, SCHOOL OF EARTH AND SPACE SCIENCES, PEKING UNIVERSITY, BEIJING 100871, P.R. CHINA
2 SCHOOL OF EARTH SCIENCES, UNIVERSITY OF MELBOURNE, MELBOURNE, VIC. 3010, AUSTRALIA

RECEIVED APRIL 1, 2005; ACCEPTED SEPTEMBER 21, 2005

Petrogenetic grids in the system NCKFMASH (Na2O–CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O) and the subsystems NCKMASH and NCKFASH calculated with the software THERMOCALC 3.1 are presented for the PT range 7–30 kbar and 450–680°C, for assemblages involving garnet, chloritoid, biotite, carpholite, talc, chlorite, kyanite, staurolite, paragonite, glaucophane, jadeite, omphacite, diopsidic pyroxene, plagioclase, zoisite and lawsonite, with phengite, quartz/coesite and H2O in excess. These grids, together with calculated compatibility diagrams and PT and TXCa and PXCa pseudosections for different bulk-rock compositions, show that incorporation of Ca into the NKFMASH system leads to many of the NKFMASH invariant equilibria moving to lower pressure and/or lower temperature, which results, in most cases, in the stability of jadeite and garnet being enlarged, but in the reduction of stability of glaucophane, plagioclase and AFM phases. The effect of Ca on the stability of paragonite is dependent on mineral assemblage at different PT conditions. The calculated NCKFMASH diagrams are powerful in delineating the phase equilibria and PT conditions of natural pelitic assemblages. Moreover, contours of the calculated phengite Si isopleths in PT and PXCa pseudosections confirm that phengite barometry in NCKFMASH is strongly dependent on mineral assemblage.

KEY WORDS: phase relations; metapelites; NCKFMASH; THERMOCALC; phengite geobarometry


* Corresponding author. Telephone: 86-10-62754157. Fax: 86-10-62751159. E-mail: cjwei{at}pku.edu.cn


Add to CiteULike CiteULike   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us    What's this?


This article has been cited by other articles:


Home page
J PetrologyHome page
C. Wei, W. Wang, G. L. Clarke, L. Zhang, and S. Song
Metamorphism of High/ultrahigh-pressure Pelitic-Felsic Schist in the South Tianshan Orogen, NW China: Phase Equilibria and P-T Path
J. Petrology, October 1, 2009; 50(10): 1973 - 1991.
[Abstract] [Full Text] [PDF]


Home page
Reviews in Mineralogy and GeochemistryHome page
J. L. Anderson, A. P. Barth, J. L. Wooden, and F. Mazdab
Thermometers and Thermobarometers in Granitic Systems
Reviews in Mineralogy and Geochemistry, January 1, 2008; 69(1): 121 - 142.
[Full Text] [PDF]


Home page
J PetrologyHome page
J.-J. YANG and R. POWELL
Calculated Phase Relations in the System Na2O-CaO-K2O-FeO-MgO-Al2O3-SiO2-H2O with Applications to UHP Eclogites and Whiteschists
J. Petrology, October 1, 2006; 47(10): 2047 - 2071.
[Abstract] [Full Text] [PDF]



Disclaimer: Please note that abstracts for content published before 1996 were created through digital scanning and may therefore not exactly replicate the text of the original print issues. All efforts have been made to ensure accuracy, but the Publisher will not be held responsible for any remaining inaccuracies. If you require any further clarification, please contact our Customer Services Department.