P–T–D Path of Eclogite from the Sambagawa Belt Deduced from Combination of Petrological and Microstructural Analyses
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/petrology/article-pdf/42/7/1225/13136033/421225.PDF
Reference33 articles.
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2. Aoya, M. & Wallis, S. R. (1999). Structural and microstructural constraints on the mechanism of eclogite formation in the Sambagawa belt, SW Japan. Journal of Structural Geology21, 1561–1573.
3. Banno, S. & Sakai, C. (1989). Geology and metamorphic evolution of the Sanbagawa metamorphic belt, Japan. In: Daly, J. S., Cliff, R. A. & Yardley, B. W. D. (eds) Evolution of Metamorphic Belts. Geological Society, London, Special Publications43, 519–532.
4. Ellis, D. J. & Green, D. H. (1979). An experimental study of the effect of Ca upon the garnet–clinopyroxene Fe–Mg exchange equilibria. Contributions to Mineralogy and Petrology71, 13–22.
5. Enami, M. (1982). Oligoclase–biotite zone of the Sanbagawa metamorphic terrain in the Besshi district, central Shikoku, Japan. Journal of the Geological Society of Japan88, 887–900 (in Japanese with English abstract).
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