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The origin of rapakivi texture by sub-isothermal decompression
Uppsala University.
Uppsala University.
1999 (English)In: PRECAMBRIAN RESEARCH, ISSN 0301-9268, Vol. 95, no 1-2, 129-146 p.Article in journal (Other scientific) Published
Abstract [en]

The rapakivi texture (plagioclase-mantled K-feldspar ovoids, rounded quartz megacrysts and euhedral plagioclase megacrysts in a more fine-grained granitic matrix) has been studied in five Proterozoic (1.64-1.55 Ga) anorogenic rapakivi granite batholiths i

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 1999. Vol. 95, no 1-2, 129-146 p.
Keyword [en]
Fennoscandian shield; Finland; geothermobarometry; intensive parameter; rapakivi granite; rapakivi texture; CALCIC AMPHIBOLE EQUILIBRIA; IN-HORNBLENDE BAROMETER; PLAGIOCLASE GEOTHERMOMETER; SW FINLAND; GRANITE; MAGMAS; TEMPERATURE; ANORTHOSITE; CONSTRAINT
URN: urn:nbn:se:uu:diva-27392OAI: oai:DiVA.org:uu-27392DiVA: diva2:55287
Addresses: Shebanov AD, Univ Uppsala, Inst Geosci, Villavagen 16, S-75239 Uppsala, Sweden. Univ Turku, Dept Geol, Turku 20014, Finland. Abo Akad Univ, Dept Geol & Mineral, SF-20500 Turku, Finland.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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