Monoclinic members of the epidote group: effects of the AI ? Fe3+ ? Fe2+ substitution and of the entry of REE3+-Reference-Cited by-同舟云学术

Monoclinic members of the epidote group: effects of the AI ? Fe3+ ? Fe2+ substitution and of the entry of REE3+

Published:1995-03 Issue:1-3 Volume:53 Page:133-153
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Mineralogy and Petrology

Author:

Bonazzi P.,Menchetti S.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF01171952.pdf

Reference79 articles.

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2. Akasaka M, Sakakibara M, Togari K (1988) Piemontite from the manganiferous hematite ore deposits in Tokoro Belt, Hokkaido, Japan. Minerai Petrol 38: 105?116

3. Ashley PM, Martin JE (1987) Chromium bearing minerais from a metamorphosed hydrothermal alteration zone in the Archaean of Western Australia. N Jb Minerai Abh 1987: 81?111

4. Banno Y (1993) Chromian sodic pyzoxene, phengite and allanite from the Sanbagawa blueschists in the eastern Kii Peninsula, Central Japan. Minerai J 16: 306?317

5. Belov NV, Rumanova JM (1953) The crystal structure of epidote Ca2Al2 FeSi3O12(OH). Dokl Akad Nauk SSSR 89: 853?856 (quoted in Struct Rep 17: 567?568)

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