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Distribution of recent volcanism and the morphology of seamounts and ridges in the GLIMPSE study area: Implications for the lithospheric cracking hypothesis for the origin of intraplate, non-hot spot volcanic chains
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Distribution of recent volcanism and the morphology of seamounts and ridges in the GLIMPSE study area: Implications for the lithospheric cracking hypothesis for the origin of intraplate, non-hot spot volcanic chains

Donald W. Forsyth, Nicholas Harmon, Daniel S. Scheirer and Robert A. Duncan
Journal of Geophysical Research: Solid Earth, Vol.111(B11), pp.B11407-n/a
Forsyth, D. W., N. Harmon, D. S. Scheirer, and R. A. Duncan (2006), Distribution of recent volcanism and the morphology of seamounts and ridges in the GLIMPSE study area: Implications for the lithospheric cracking hypothesis for the origin of intraplate, non-hot spot volcanic chains, J. Geophys. Res., 111, B11407, doi:10.1029/2005JB004075.
25/11/2006

Abstract

intraplate volcanism lithospheric cracking seamounts
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https://doi.org/10.1029/2005JB004075View
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