Collisional Orogeny in the Scandinavian Caledonides: Drilling the Main Caledonian Décollement and into the Basement of the Fennoscandian Shield
Project Acronym: COSC-1 | State: Post Moratorium | Expedition ID: 5054
The COSC project focuses on the mid Paleozoic Caledonide Orogen in Scandinavia in order to better understand orogenic processes, both in the past and in today's active mountain belts.
The Scandinavian Caledonides provide a particularly well preserved example of Paleozoic plate collision, with the underthrusting of continent Baltica beneath Laurentia and thickening of the continental crust to at least 100 km. In the Scandes, the surface geology in combination with geophysical data provide control of the geometry of the Caledonian structure, both of the allochthon and the underlying parautochthon-autochthon, and define the targets for drilling. The drillholes themselves will help us to better define the structure and physical conditions of the allochthons and underlying parautochthon during nappe emplacement.
Click here for information on the second phase of the COSC project.
Keywords: Europe, Sweden, Basement Deformation, Foreland, Natural Hazards, Paleoenvironment, Paleozoic, Post-weichselian Temperature Development
Cores are stored at Federal Institute for Geosciences and Natural Resources, Spandau, Germany
Project Management
Project Details
Project Location
Project Timeline
Moratorium Phase 1
1 March 2015 - 1 March 2017
Sampling Party Phase 1
2 - 6 February 2015 in Berlin-Spandau, Germany
Drilling Phase 1
8 May - 26 August 2014
Full Proposal Phase 1 Approved
Workshop Held
21-25 June 2010 in Åre, Sweden