Long-term convergence along SW Fennoscandia: 330 m.y. of Proterozoic crustal growth [Precam Res 161 (2008) 452

Long-term convergence along SW Fennoscandia: 330 m.y. of Proterozoic crustal growth [Precam Res 161 (2008) 452–472]

Published:2008-06 Issue:3-4 Volume:163 Page:402-421
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Åhäll Karl-Inge,Connelly James N.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference129 articles.

1. Pillow lava in the Stora Le-Marstrand formation, southwestern Sweden;Åhäll;GFF,1984

2. Åhäll, K.-I., 1990. An investigation of the Proterozoic Stenungssund granitoid, SW Sweden; conflicting geochronological and field evidence. In: Gower, C.F., Rivers, T., and Ryan, B. (Eds.), Mid-Proterozoic Laurentia-Baltica. Geological Association of Canada Special Paper 38, pp. 117–129.

3. Intermittent 1.53–1.13Ga magmatism in western Baltica; age constraints and correlations within a postulated supercontinent;Åhäll;Precambrian Res.,1998

4. Age, tectonic setting and provenance of Östfold-Marstrand belt supracrustals: westward crustal growth of the Baltic Shield at 1760Ma;Åhäll;Precambrian Res.,1989

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

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