The pleochroism of a gem-quality enstatite in the region of the OH stretching frequency, with a stereochemical interpretation-Reference-Cited by-同舟云学术

The pleochroism of a gem-quality enstatite in the region of the OH stretching frequency, with a stereochemical interpretation

Published:1986 Issue:1 Volume:35 Page:19-25
ISSN:0041-3763
Container-title:TMPM Tschermaks Mineralogische und Petrographische Mitteilungen
language:en
Short-container-title:TMPM Tschermaks Petr. Mitt.

Author:

Beran A.,Zemann J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF01081915.pdf

Reference20 articles.

1. Beran, A., 1976: Messung des ultrarot-Pleochroismus von Mineralen. XIV. Der Pleochroismus der OH-Streckfrequenz in Diopsid. Tschermaks Min. Petr. Mitt.23, 79?85.

2. ?,Götzinger, M., Zemann, J., 1981: Infrarotspektroskopische Untersuchungen über den OH-Gehalt von Pyroxenen und Cyaniten in Gesteinen. Fortschr. Min.59, Beih. 1, 16?18.

3. ?, 1983: A model of the OH positions in olivine, derived from infrared-spectroscopic investigations. Phys. Chem. Min.9, 57?60.

4. Deer, W. A., Howie, R. A., Zussman, J., 1963: Rock-forming Minerals. Vol. 2. Chain Silicates. London: Longmans, Green and Co.

5. Single-chain Silicates;W. A. Deer,1978

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