Der Stabilit�tsbereich des Pyrophyllits unter dem Einflu� von S�uren
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/BF00518125.pdf
Reference27 articles.
1. Althaus, E.: Die Bildung von Pyrophyllit und Andalusit zwischen 2000 und 7000 Bar H2O-Druck. Naturwissenschaften 53, 105 (1966).
2. ?: Die Phasengrenze Andalusit/Sillimanit. Naturwissenschaften 53, 129 (1966).
3. ?:, u. H. G. F. Winkler: Experimentelle Gesteinsmetamorphose ? VI. Einfluß von Anionen auf metamorphe Mineralreaktionen. Geochim. et Cosmochim. Acta 26, 145?180 (1962).
4. Aramaki, S., and R. Roy: Revision of equilibrium diagram for the system Al2O3-SiO2. Nature 184, 631?632 (1959).
5. ? ?: A new polymorph of Al2SiO5 and further studies in the system Al2O3-SiO2-H2O. Am. Mineralogist 48, 1322?1347 (1963).
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1. Regional distribution of Al-silicates and metamorphic zonation in the low-grade Verrucano metasediments from the Northern Apennines, Italy;Journal of Metamorphic Geology;1986-08
2. A model system for mineral facies in pelitic schists;Contributions to Mineralogy and Petrology;1976-01
3. Remplacements isomorphiques par synthèses hydrothermales dans les silicates fluores: Topaze et zunyite;Chemical Geology;1973-12
4. A study of rock alteration process based on kinetics of hydrothermal experiment;Contributions to Mineralogy and Petrology;1971
5. Stabilit� des silicates d'alumine hydrat�s;Contributions to Mineralogy and Petrology;1969
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