Origin of ocean island basalts in the West African passive margin without mantle plume involvement
Author:
Funder
MEXT | Japan Society for the Promotion of Science
Publisher
Springer Science and Business Media LLC
Subject
General Physics and Astronomy,General Biochemistry, Genetics and Molecular Biology,General Chemistry
Link
http://www.nature.com/articles/s41467-019-10832-7.pdf
Reference70 articles.
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2. Richards, M. A., Duncan, R. A. & Courtillot, V. E. Flood basalts and hot-spot tracks: plume heads and tails. Science 246, 103–107 (1989).
3. Foulger, G. R. & Natland, J. H. Is “hotspot” volcanism a consequence of plate tectonics? Science 300, 921–922 (2003).
4. Ballmer, M. D. et al. Non-hotspot volcano chains originating from small-scale sublithospheric convection. Geophys. Res. Lett. 34, L23310 (2007).
5. Conrad, C. P. et al. Shear-driven upwelling induced by lateral viscosity variations and asthenospheric shear: a mechanism for intraplate volcanism. Phys. Earth Planet. Inter. 178, 162–175 (2010).
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