Messung des Ultrarot-Pleochroismus von Mineralen XII. Der Pleochroismus der OH-Streckfrequenz in Disthen-Reference-Cited by-同舟云学术

Messung des Ultrarot-Pleochroismus von Mineralen XII. Der Pleochroismus der OH-Streckfrequenz in Disthen

Published:1971 Issue:3 Volume:16 Page:129-135
ISSN:0041-3763
Container-title:TMPM Tschermaks Mineralogische und Petrographische Mitteilungen
language:de
Short-container-title:TMPM Tschermaks Petr. Mitt.

Author:

Beran A.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF01134164.pdf

Reference12 articles.

1. Beran, A., 1970: Ultrarotspektroskopischer Nachweis von OH-Gruppen in den Mineralen der ?Al2SiO5?-Modifikationen. Anz. Österr. Akad. Wiss., Math.-naturwiss. Kl., Jg. 1970, 184?185.

2. ? undJ. Zemann, 1969: Messung des Ultrarot-Pleochroismus von Mineralen. VIII. Der Pleochroismus der OH-Streckfrequenz in Andalusit. Tschermaks Min. Petr. Mitt.13, 285?292.

3. Burnham, C. W., 1963: Refinement of the crystal structure of kyanite. Z. Krist.118, 337?360.

4. Eigenfeld, I., undF. Machatschki, 1957: Über den angeblichen Alkaligehalt des Disthens. Anz. Österr. Akad. Wiss., Math.-naturwiss. Kl.94, 151?152.

5. Faye, G. H., andE. H. Nickel, 1969: On the origin of colour and pleochroism of kyanite. Canad. Min.10, 35?46.

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