1.80–1.75 Ga granite suites in the west Troms Basement Complex, northern Norway: Palaeoproterozoic magma emplacement during advancing accretionary orogeny, from field observations

Author:

Bergh S.G.,Haaland L.,Arbaret L.,Coint N.,Forien M.

Funder

UiT Arctic University of Norway

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference111 articles.

1. Long-term convergence along SW Fennoscandia: 330 my. of Proterozoic crustal growth;Åhäll;Precambr. Res.,2008

2. Growth-related 1.85–1.55 Ga magmatism in the Baltic shield: a review addressing the tectonic characteristics of Svecofennian, TIB 1-related, and Gothian events;Åhäll;GFF,2000

3. Geochemical classification of plutonic rocks in central and northern Sweden: rapporter och meddelanden 106;Ahl;Sver. Geol. Und.,2001

4. Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon;Andersen;J. Geol. Soc. London,2009

5. Andersson, U.B., Eklund, O., Claeson, D.T., 2004. Geochemical character of the mafic hybrid magmatism in the Småland-Värmland belt. Special Paper 37 In: Högdahl, K., Andersson, U.B., Eklund, O. (Eds.), The Transscandinavian Igneous Belt (TIB) in Sweden: A Review of Its Character and Evolution, Geological Survey of Finland, pp. 47–55.

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