Digitale Medien
Springer
Contributions to mineralogy and petrology
41 (1973), S. 273-276
ISSN:
1432-0967
Quelle:
Springer Online Journal Archives 1860-2000
Thema:
Geologie und Paläontologie
Notizen:
Abstract The colour of chromium-bearing pyrope-rich garnets may be red or green depending upon the Cr-O distance which varies with the chemical composition. Red garnets become green when the crystal field parameter δ0 for substitutional Cr3+ decreases below 17200 cm−1 corresponding to about 1970 Å.
Materialart:
Digitale Medien
URL:
http://dx.doi.org/10.1007/BF00371036
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