Tonian and Silurian magmatism in Nordaustlandet: Svalbard’s place in the Caledonian orogen

Author:

McClelland* William C.1,von Gosen* Werner2,Piepjohn* Karsten3

Affiliation:

1. University of Iowa, Department of Earth and Environmental Sciences, Iowa City, Iowa 52242, USA

2. Geozentrum Nordbayern, Krustendynamik, Friedrich-Alexander-Universität Erlangen-Nürnberg, D-91054 Erlangen, Germany

3. Bundesanstalt für Geowissenschaften und Rohstoffe (BGR), Geologie der Energierohstoffe, Polargeologie, D-30655 Hannover, Germany

Publisher

Geological Society of America

Reference97 articles.

1. Evidence for simultaneous contraction and extension at different crustal levels during the Caledonian orogeny in NE Greenland;Andresen,2007

2. Late Ordovician to Silurian ensialic magmatism in Liverpool Land, East Greenland;Augland;new evidence extending the northeastern branch of the continental Laurentian magmatic arc: Geological Magazine,2012

3. Timing of magmatism following initial convergence at a passive margin, southwestern US Cordillera, and ages of lower crustal magma sources;Barth;The Journal of Geology,2006

4. Coupled elemental and isotopic analyses of polygenetic zircons from granitic rocks by ion microprobe, with implications for melt evolution and the sources of granitic magmas;Barth;Chemical Geology,2010

5. Stratigraphic record of Neoproterozoic ice sheet collapse: the Kapp Lyell diamictite sequence;Bjørnerud;SW Spitsbergen, Svalbard: Geological Magazine,2010

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