Low temperature spectral studies of Mn3+-bearing andalusite and epidote type minerals in the range 30000–5000 cm−1

Author:

Smith G.,Hålenius U.,Langer K.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Reference33 articles.

1. Abs-Wurmbach I, Langer K, Tillmanns E (1977) Structure and polarized absorption spectra of Mn3+ substituted andalusites (viridines). Naturwissenschaften 64:527–528

2. Abs-Wurmbach I, Langer K, Seifert F, Tillmanns E (1981) The crystal chemistry of (Mn3+, Fe3+)-substituted andalusites (viridines and kanonaite), (Al1−x−y Mn x 3+ Fe y 3+ )2(O|SiO4): Crystal structure refinements, Mössbauer, and polarized optical absorption spectra. Z Kristallogr 155:81–113

3. Annersten H, Hålenius U (1976) Ion distribution in pink muscovite, a discussion. Am Mineral 61:1045–1050

4. Burns RG (1974) The polarized spectra of iron in silicates: olivine. A discussion of neglected contributions from Fe2+ions in M(1) sites. Am Mineral 59:625–629

5. Burns RG, Strens RGJ (1967) Structural interpretation of polarized absorption spectra of the Al-Fe-Mn-Cr epidotes. Mineral Mag 36:204–226

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