A TEM study of disequilibrium plagioclase breakdown at high pressure: the role of infiltrating fluid-Reference-Cited by-同舟云学术

A TEM study of disequilibrium plagioclase breakdown at high pressure: the role of infiltrating fluid

Published:1989-04 Issue:4 Volume:101 Page:426-437
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Wayte Gavin J.,Worden Richard H.,Rubie David C.,Droop Giles T. R.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00372216.pdf

Reference34 articles.

1. Barnicoat AC, Fry N (1986) High-pressure metamorphism in the Zermatt-Saas ophiolite zone, Switzerland. J Geol Soc London 143:607?618

2. Bearth P (1967) Die Ophiolithe der Zone von Zermatt-Saas Fee. Beitr Geol Karte Schweiz NF 132

3. Bocquet J, Delaloye M, Hunziker JC, Krummenacher D (1974) K-Ar and Rb-Sr dating of blue amphiboles, micas and associated minerals from the Western Alps. Contrib Mineral Petrol 47:7?26

4. Carpenter MA, Ferry JM (1984) Constraints on the thermodynamic mixing properties of plagioclase feldspars. Contrib Mineral Petrol 87:138?148

5. Carpenter MA, McConnell JDC (1984) Experimental determination of the C¯1?I¯1 transformation in intermediate plagioclase feldspars. Am Mineral 69:112?121

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