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Cordierite volatile content and the role of CO (sub 2) in high-grade metamorphism
Julie K. Vry, Philip E. Brown and John W. Valley
Cordierite volatile content and the role of CO (sub 2) in high-grade metamorphism
American Mineralogist (February 1990) 75 (1-2): 71-88
Cordierite volatile content and the role of CO (sub 2) in high-grade metamorphism
American Mineralogist (February 1990) 75 (1-2): 71-88
Index Terms/Descriptors
- amphibolite facies
- carbon dioxide
- cordierite
- electron probe data
- experimental studies
- facies
- fluid phase
- Fourier analysis
- geologic barometry
- grade
- granulite facies
- granulites
- high-grade metamorphism
- infrared spectra
- metamorphic rocks
- metamorphism
- minerals
- natural materials
- P-T conditions
- phase equilibria
- ring silicates
- silicates
- spectra
- volatiles
- water
Abstract
The channel H (sub 2) O, CO (sub 2) , and alkali contents of 33 natural cordierites have been analysed using a combination of Fourier-transform infrared spectroscopy (FTIR), electron- microprobe analysis, and chemical and isotopic techniques.
ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 75
Serial Issue: 1-2
Title: Cordierite volatile content and the role of CO (sub 2) in high-grade metamorphism
Affiliation: Univ. Wis., Dep. Geol. and Geophys.,
Madison, WI,
United States
Pages: 71-88
Published: 199002
Text Language: English
Publisher: Mineralogical Society of America,
Washington, DC,
United States
References: 79
Accession Number: 1990-026140
Categories: Igneous and metamorphic petrologyMineralogy of silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 3 tables
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United KingdomTwickenhamUKUnited Kingdom
Update Code: 1990
