Zircon geochronology in polymetamorphic gneisses in the Sveconorwegian orogen, SW Sweden: ion microprobe evidence for 1.46–1.42 and 0.98–0.96 Ga reworking-Reference-Cited by-同舟云学术

Zircon geochronology in polymetamorphic gneisses in the Sveconorwegian orogen, SW Sweden: ion microprobe evidence for 1.46–1.42 and 0.98–0.96 Ga reworking

Published:2002-01 Issue:3-4 Volume:113 Page:193-225
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Söderlund Ulf,Möller Charlotte,Andersson Jenny,Johansson Leif,Whitehouse Martin

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference72 articles.

1. The Gothian and Labradorian orogens, variations in accretionary tectonism along a late Paleoproterozoic Laurentia–Baltica margin;Åhäll;GFF,1997

3. Westward accretion of the Baltic Shield: Implications from the 1.6 Ga Åmål-Horred Belt, SW Sweden;Åhäll;Precambrian Res.,1995

4. Geochronology and structural setting of the 1.38 Ga Torpa granite; implications for the charnockite formation in SW Sweden;Åhäll;GFF,1997

5. Sveconorwegian (-Grenvillian) deformation, metamorphism and leucosome formation in SW Sweden, SW Baltic Shield: constraints from a Mesoproterozoic granite intrusion;Andersson;Precambrian Res.,1999

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