Inspired by a 2012 paper that proposed a correlation between such hotspots and the velocity of seismic waves moving through Earth's interior, UC Santa Barbara geochemist Matthew Jackson teamed with the authors of the original paper — Thorsten Becker of the University of Texas at Austin and Jasper Konter of the University of Hawaii — to show that only the hottest hotspots with
the slowest wave velocity draw from the primitive reservoir formed early in the planet's history.
Not exact matches
The relatively small rock bodies are termed «ultra-low
velocity zones» because seismic
waves greatly
slow down as they pass through them.
Led by Carnegie's Ho - kwang «Dave» Mao, the research team believes that as much as 300 million tons of water could be carried down into Earth's interior every year and generate deep, massive reservoirs of iron dioxide, which could be the source of the ultralow
velocity zones that
slow down seismic
waves at the core - mantle boundary.
These seismic measurements enabled scientists to visualize these ultralow
velocity zones in some regions along the core - mantle boundary, by observing the
slowing down of seismic
waves passing through them.
Led by Geophysical Laboratory's Ho - kwang «Dave» Mao, the research team believes that as much as 300 million tons of water could be carried down into Earth's interior every year and generate deep, massive reservoirs of iron dioxide, which could be the source of the ultralow
velocity zones that
slow down seismic
waves at the core - mantle boundary.