Sveconorwegian massif-type anorthosites and related granitoids result from post-collisional melting of a continental arc root

Author:

Vander Auwera J.,Bolle O.,Bingen B.,Liégeois J.-P.,Bogaerts M.,Duchesne J.C.,De Waele B.,Longhi J.

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference166 articles.

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2. Provenance characteristics of Mesoproterozoic metasedimentary rocks from Telemark, South Norway: a Nd-isotope mass-balance model;Andersen;Precambrian Research,2003

3. Precambrian multi-stage crustal evolution in the Bamble sector of south Norway: Pb isotopic evidence from a Sveconorwegian deep-seated granitic intrusion;Andersen;Chemical Geology (Isotope Geoscience Section),1994

4. Metamorphism, provenance ages and source characteristics of Precambrian clastic metasediments in the Bamble sector, south Norway;Andersen;Petrology,1995

5. Nature and distribution of deep crustal reservoirs in the southwestern part of the Baltic shield: evidence from Nd, Sr and Pb isotope data on late Sveconorwegian granites;Andersen;Journal of the Geological Society,2001

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