Single crystal infrared spectra in the range of OH fundamentals of paragenetic garnet, omphacite and kyanite in an eklogitic mantle xenolith-Reference-Cited by-同舟云学术

Single crystal infrared spectra in the range of OH fundamentals of paragenetic garnet, omphacite and kyanite in an eklogitic mantle xenolith

Published:1993 Issue:2-4 Volume:48 Page:257-268
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Mineralogy and Petrology

Author:

Beran A.,Langer K.,Andrut M.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF01163102.pdf

Reference35 articles.

1. Ackermann L, Cemic L, Langer K (1983) Hydrogarnet substitution in pyrope: a possible location for {?water? in the mantle}. Earth Planet Sci Letters 62: 208?214

2. Aires RD, Rossman GR (1984) The hydrous component in garnets: pyralspites. Am Mineral 69: 1116?1126

3. Andrut M, Langer K, Sobolev NV (1991) Optical spectra and partitioning of Cr3+ in the high-pressure paragenesis pyr/cpx/ky of a mantle eclogite. Terra Abstr 3 (1): 67 S5/20

4. Bell DR, Rossman GR (1992a) Water in Earth's mantle: the role of nominally anhydrous minerals. Science 255: 1391?1397

5. Bell DR, Rossman GR (1992b) The distribution of hydroxyl in garnets from the subcontinental mantle of southern Africa. Contrib Mineral Petrol 111: 161?178

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