Plume-like upper mantle instabilities drive subduction initiation
Author:
Affiliation:
1. iSteP, UMR 7193, Case 129, CNRS; Université Pierre et Marie Curie; Paris; France
2. Netherlands Centre for Integrated Solid Earth Sciences, Faculty of Earth and Life Sciences; VU University Amsterdam; Amsterdam; Netherlands
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/gl1003/2009GL041535/2009GL041535.pdf
Reference29 articles.
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2. Burov , E. 2007 The role of the gravitational instabilities, the density structure and the extension rate in the evolution of slow continental margins G. D. Karner G. Manatschal L. M. Pinheiro Geol. Soc. Spec. Publ. 282 139 156
3. The equivalent elastic thickness (Te), seismicity and the long-term rheology of continental lithosphere: Time to burn out “crème brûlée”?: Insights from large-scale geodynamic modeling;Burov;Tectonophysics,2009
4. Controls of mantle plumes and lithospheric folding on modes of intra-plate continental tectonics: Differences and similarities;Burov;Geophys. J. Int.,2009
5. The plume head-lithosphere interaction using a tectonically realistic formulation for the lithosphere;Burov;Geophys. J. Int.,2005
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