Seismic evidence for hotspot-induced buoyant flow beneath the Reykjanes Ridge.
Volcanic hotspots and mid-ocean ridge spreading centers are the surface expressions of upwelling in Earth's mantle convection system, and their interaction provides unique information on upwelling dynamics. I investigated the influence of the Iceland hotspot on the adjacent mid-Atlantic spreading center using phase-delay times of seismic surface waves, which show anomalous polarization anisotropy-a delay-time discrepancy between waves with different polarizations. This anisotropy implies that the hotspot induces buoyancy-driven upwelling in the mantle beneath the ridge.
Gaherty
J B
JB
School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA.