True Polar Wander: A Key Indicator for Plate Configuration and Mantle Convection During the Late Neoproterozoic
Author:
Affiliation:
1. Centre for Earth Evolution and Dynamics; University of Oslo; Oslo Norway
2. Institut de Physique du Globe de Paris-Sorbonne Paris Cité; Université Paris Diderot; Paris France
Funder
Institut National des Sciences de l'Univers, Centre National de la Recherche Scientifique
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018GC007490/fullpdf
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3. The 616 Ma old Egersund basaltic dike swarm, SW Norway, and late Neoproterozoic opening of the Iapetus Ocean;Bingen;The Journal of Geology,1998
4. The stress regime associated with continental break-up;Bott;Geological Society, London, Special Publications,1992
5. A review of Wilson cycle plate margins: A role for mantle plumes in continental break-up along sutures?;Buiter;Gondwana Research,2014
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