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ISOTOPE STUDIES OF GRANITOIDS FROM THE BANGENHUK FORMATION, NY-FRIESLAND CALEDONIDES, SVALBARD
Uppsala University.
Uppsala University.
Uppsala University.
Uppsala University.
1995 (English)In: GEOLOGICAL MAGAZINE, ISSN 0016-7568, Vol. 132, no 3, 303-320 p.Article in journal (Other scientific) Published
Abstract [en]

The Caledonian Hecla Hoek succession in Ny Friesland, eastern Svalbard has been interpreted, for many decades, to be a continuous stratigraphic sequence. Early Palaeozoic and Neoproterozoic strata in its upper parts pass more or less conformably down into

Place, publisher, year, edition, pages
CAMBRIDGE UNIV PRESS , 1995. Vol. 132, no 3, 303-320 p.
Keyword [en]
ZIRCON AGES; EVOLUTION; PB; GEOCHRONOLOGY; ROCK
Identifiers
URN: urn:nbn:se:uu:diva-28040OAI: oai:DiVA.org:uu-28040DiVA: diva2:55936
Note
Addresses: JOHANSSON A, SWEDISH MUSEUM NAT HIST, ISOTOPE GEOL LAB, BOX 50007, S-10405 STOCKHOLM, SWEDEN. UNIV UPPSALA, DEPT GEOPHYS, S-75122 UPPSALA, SWEDEN. UNIV GOTHENBURG, DEPT GEOL, S-41296 GOTHENBURG, SWEDEN. LUND UNIV, DEPT GEOL, S-22362 LUND, SWEDEAvailable from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-16

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