A Correlation Between Ultra-Low Basal Velocities in the Mantle and Hot Spots
Q. Williams,
J. Revenaugh,
E. Garnero
*
The statistical correlation between the locations of hot spots at
the surface of Earth and the distribution of ultra-low-velocity zones
at the base of the mantle has about a 1 percent chance of arising
randomly. This correlation is more significant than that between hot
spots and negative velocity anomalies in tomographic models of deep
mantle compressional and shear velocity. This correlation is consistent
with the notion that many hot spots originate in a low-velocity,
probably partially molten layer at the core-mantle boundary and undergo
little lateral deflection on ascent.
Department of Earth Sciences and Institute of Tectonics,
University of California, Santa Cruz, CA 95064, USA.
*
Present address: Seismological Laboratory, University of California,
Berkeley, CA 94720, USA.