Phase equilibria for graphitic metapelite including solution of CO2 in melt and cordierite: implications for dehydration, partial melting and graphite precipitation-Reference-Cited by-同舟云学术

Phase equilibria for graphitic metapelite including solution of CO2 in melt and cordierite: implications for dehydration, partial melting and graphite precipitation

Published:2013-08-26 Issue:8 Volume:31 Page:843-862
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J. Meta. Geol.

Author:

Chu X.¹,Ague J. J.¹²

Affiliation:

1. Department of Geology and Geophysics; Yale University; P.O. Box 208109 New Haven CT 06520-8109 USA

2. Peabody Museum of Natural History; Yale University; New Haven CT 06511 USA

Funder

National Science Foundation Directorate of Geosciences

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12047/fullpdf

Reference106 articles.

1. Simple models of coupled fluid infiltration and redox reactions in the crust;Ague;Contributions to Mineralogy and Petrology,1998

2. Release of CO2 from carbonate rocks during regional metamorphism of lithologically heterogeneous crust;Ague;Geology,2000

3. High fO2 during silimanite zone metamorphism of part of the Barrovian type locality, Glen Clova, Scotland;Ague;Journal of Petrology,2001

4. Discovery of ultrahigh-temperature metamorphism in the Acadian orogeny, Connecticut, USA;Ague;Geology,2013

5. The high temperature behavior of water and carbon dioxide in cordierite and beryl;Aines;American Mineralogist,1984

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