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Single-zircon Pb evaporation geochronology constrains basement cover relationships in the Lower Hecla Hoek Complex of northern Ny Friesland, Svalbard
Uppsala University.
Uppsala University.
Uppsala University.
Uppsala University.
1997 (English)In: CHEMICAL GEOLOGY, ISSN 0009-2541, Vol. 137, no 1-2, 117-134 p.Article in journal (Other scientific) Published
Abstract [en]

The Hecla Hoek Complex, a similar to 18-km-thick succession in the Svalbard Caledonian Eastern Terrane, has been interpreted to be a more or less continuous volcano-sedimentary sequence. Amphibolite-facies rocks in the lower parts appear to grade conforma

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 1997. Vol. 137, no 1-2, 117-134 p.
Keyword [en]
Pb evaporation ages; Svalbard; Ny Friesland; Hecla Hoek; detrital zircon; U-PB; ESKOLABREEN FORMATION; IMPROVED ACCURACY; SOUTHERN NY; SPITSBERGEN; CALEDONIDES; AGES; AR-40/AR-39; GRANITOIDS; ISOTOPE
Identifiers
URN: urn:nbn:se:uu:diva-28029OAI: oai:DiVA.org:uu-28029DiVA: diva2:55925
Note
Addresses: Hellman FJ, LUND UNIV, DEPT GEOL, SOLVEGATAN 13, S-22362 LUND, SWEDEN. UNIV UPPSALA, DEPT GEOPHYS, S-75236 UPPSALA, SWEDEN. SWEDISH MUSEUM NAT HIST, LAB ISOTOPE GEOL, S-10405 STOCKHOLM, SWEDEN.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-15

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