Mantle flow geometry from ridge to trench beneath the Gorda–Juan de Fuca plate system
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/ngeo2569.pdf
Reference40 articles.
1. Conrad, C., Behn, M. & Silver, P. Global mantle flow and the development of seismic anisotropy: Differences between the oceanic and continental upper mantle. J. Geophys. Res. 112, B07317 (2007).
2. Toomey, D. et al. The Cascadia initiative: A sea change in seismological studies of subduction zones. Oceanography 27, 138–150 (2014).
3. Riddihough, R. Recent movements of the Juan de Fuca plate system. J. Geophys. Res. 89, 6980–6994 (1984).
4. Eakin, C. et al. Seismic anisotropy beneath Cascadia and the Mendocino triple junction: Interaction of the subducting slab with mantle flow. Earth Planet Sci. Lett. 297, 627–632 (2010).
5. Currie, C. et al. Shear wave anisotropy beneath the Cascadia subduction zone and western North American craton. Geophys. J. Int. 157, 341–353 (2004).
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