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A flow-foliated ignimbrite related to the Aland rapakivi granite in SW Finland
Uppsala University.
Uppsala University.
Uppsala University.
Uppsala University.
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1996 (English)In: TERRA NOVA, ISSN 0954-4879, Vol. 8, no 6, p. 548-557Article in journal (Other scientific) Published
Abstract [en]

A flow-foliated felsic ignimbrite constitutes the uppermost lithological unit of the 1.58 Gyr anorogenic magmatic rocks in SW Finland. The ignimbrite is derived from an explosive eruption of hot (approximate to 950 degrees C) phenocryst-bearing A-type (ra

Place, publisher, year, edition, pages
BLACKWELL SCIENCE LTD , 1996. Vol. 8, no 6, p. 548-557
Keywords [en]
FE-TI OXIDES; MAGMA; EQUILIBRIA; PYROXENES; OLIVINE; QUARTZ; ROCKS
Identifiers
URN: urn:nbn:se:uu:diva-27888OAI: oai:DiVA.org:uu-27888DiVA, id: diva2:55784
Note
Addresses: Eklund O, TURKU UNIV, DEPT GEOL, FIN-20014 TURKU, FINLAND. ST PETERSBURG STATE UNIV, GEOL FAC, DEPT MINERAL, ST PETERSBURG 199034, RUSSIA. ABO AKAD UNIV, DEPT GEOL & MINERAL, FIN-20500 TURKU, FINLAND. UNIV UPPSALA, INST EARTH SCI, S-75236 UPPSAAvailable from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-15

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