Das $$P{\text{ - }}T{\text{ - }}X_{{\text{CO}}_{\text{2}} } $$ Stabilitätsfeld von Lawsonit-Reference-Cited by-同舟云学术

Das $$P{\text{ - }}T{\text{ - }}X_{{\text{CO}}_{\text{2}} } $$ Stabilitätsfeld von Lawsonit

Published:1972-02 Issue:2 Volume:34 Page:116-134
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:de
Short-container-title:Contr. Mineral. and Petrol.

Author:

Nitsch Karl -Heinz

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00373768.pdf

Reference25 articles.

1. Althaus, E.: Die Bildung von Pyrophyllit und Andalusit zwischen 2000 und 7000 Bar H2O-Druck. Naturwissenschaften 53, 105/106 (1966).

2. —: Experimentelle Bestimmung des Stabilitätsbereiches von Disthen (Cyanit). Naturwissenschaften 54, 42/43 (1967).

3. —: Das System Al2O3-SiO2-H2O. Experimentelle Untersuchungen und Folgerungen für die Petrogenese der metamorphen Gesteine. Neues Jahrb. Mineral. Abhandl. 111, 74–161 (1969).

4. Crawford, W., Fyfe, W.S.: Lawsonite equilibria. Am. J. Sci. 263, 262–270 (1965).

5. Ernst, W.G.: Significance of phengitic micas from low-grade schists. Am. Mineralogist. 48, 1357–1373 (1963).

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