Westward growth of the baltic shield
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference53 articles.
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1. Continental growth and reworking on the edge of the Columbia and Rodinia supercontinents; 1.86–0.9 Ga accretionary orogeny in southwest Fennoscandia;International Geology Review;2014-11-26
2. Geochronology of carbonatites from the Canadian and Baltic Shields, and the Canadian Cordillera: clues to mantle evolution;Mineralogy and Petrology;2009-06-23
3. Continental margin magmatism and migmatisation in the west-central Fennoscandian Shield;Lithos;2008-05
4. Mafic plutonic rocks in a continental-arc setting: geochemistry of 1.87-1.78 Ga rocks from south-central Sweden and models of their palaeotectonic setting;Geological Journal;2008
5. Characterization of the Paleoproterozoic Mantle beneath the Fennoscandian Shield: Geochemistry and Isotope Geology (Nd, Sr) of ~ 1.8 Ga Mafic Plutonic Rocks from the Transscandinavian Igneous Belt in Southeast Sweden;International Geology Review;2007-07
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