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Graftonite-beusite in Sweden: Primary phases, products of exsolution, and distribution in zoned populations of granitic pegmatites
Uppsala University.
Uppsala University.
Uppsala University.
Uppsala University.
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1998 (English)In: CANADIAN MINERALOGIST, ISSN 0008-4476, Vol. 36, 377-394 p.Article in journal (Other scientific) Published
Abstract [en]

Graftonite - beusite is relatively widespread in the LCT family of granitic pegmatites of the Bothnian basin and of the Uto - Mysingen field in Sweden. It commonly constitutes the matrix containing either coarse lamellae of sarcopside, which in turn hosts

Place, publisher, year, edition, pages
MINERALOGICAL ASSOC CANADA , 1998. Vol. 36, 377-394 p.
Keyword [en]
graftonite; beusite; triphylite; sarcopside; phosphates; exsolution; granitic pegmatite; regional zoning; Sweden; NORTHWEST-TERRITORIES; CRYSTAL-STRUCTURE; FIELD; GEOCHEMISTRY; PETROLOGY; FELDSPAR; AGES
Identifiers
URN: urn:nbn:se:uu:diva-27801OAI: oai:DiVA.org:uu-27801DiVA: diva2:55697
Note
Addresses: Smeds SA, Uppsala Univ, Inst Earth Sci, Villavagen 16, SE-75236 Uppsala, Sweden. Uppsala Univ, Inst Earth Sci, SE-75236 Uppsala, Sweden. Univ Manitoba, Dept Geol Sci, Winnipeg, MB R3T 2N2, Canada. Smithsonian Inst, Dept Mineral Sci, Washington,Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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