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Protogine Zone
Projet ANR ASTER Rapport De Tâche 4 Potentialité De Stocks Géologiques De Terres Rares En Europe Et Au Groenland Rapport Final
Tectonic Regimes in the Baltic Shield During the Last 1200 Ma • a Review
Lund, Sweden, January 8–10 2014
A Four-Phase Model for the Sveconorwegian Orogeny, SW Scandinavia 43
The Protogine Zone. Geology and Mobility During the Last 1.5 Ga ^ O
93529 Karolina Bjärnborg
Dating Methods and Geochronology of Fractures and Movements in Bedrock: a Review
Oskarshamn Site Investigation. Bedrock Geology
Domain IP Tomography for Bedrock Characterisation at Önneslöv, Southern Sweden
Guide for Geological Nomenclature in Sweden
U-Pb Zircon Geochronology of Granitic and Syenitoid Rocks Across the Southern Part of the Sveconorwegian Orogen
The Mesoproterozoic in the Nordic Countries
Geologi for Samfunnet
U-Pb Zircon Age of C. 1 440 Ma Syenogranite Within the Protogine
Article in Press
The Mesoproterozoic Hallandian Event - a Region-Scale Orogenic Event in the Fennoscandian Shield
Geochronology of Gneisses Adjacent to the Mylonite Zone in Southwestern Sweden: Evidence of a Tectonic Window?
Lund, Sweden, January 8–10 2014
Top View
Proterozoic Crustal Evolution in Southcentral Fennoscandia Karin
Guide for Geological Nomenclature in Sweden
Crustal Structure and Regional Tectonics of SE Sweden and the Baltic Sea
Neoproterozoic Palaeomagnetic Directions in Rocks from a Key Section of the Protogine Zone, Southern Sweden
Geochemistry and Petrology of Mafic Proterozoic and Permian Dykes on Bornholm, Denmark: Four Episodes of Magmatism on the Margin of the Baltic Shield
Nijland-TG-101-1993-Copy.Pdf
The Geological History of the Baltic Sea a Review of the Literature and Investigation Tools
Europe's Rare Earth Element Resource Potential: an Overview of REE Metallogenetic Provinces and Their Geodynamic Setting
Rapakivi Granites and Related Rocks in Central Sweden 7Th Interna TionAl SymPoSium on RapAKiVi GranItes July 24-26 1996, UniVerSity of HelSinKi, FinLand
In Scania, S Sweden: Evidence for Two Pulses at 191-178 Ma and 110 Ma, and Their Relation to the Break- up of Pangea