We examine upper mantle anisotropy across the Hawaiian Swell by analyzing shear wave
splitting of teleseismic SKSwaves recorded by the PLUME broadband land and ocean …

[1] Walker et al.[2001](hereinafter referred to as WBK) suggest a ''parabolic asthenospheric
flow''model to explain observations of shear-wave splitting in the upper mantle around …

We utilized recordings of seismic shear phases provided by several North American
broadband seismometer arrays to provide unique constraints on shear wave anisotropy …

We present models of the 3-D shear velocity structure of the lithosphere and asthenosphere
beneath the Hawaiian hotspot and surrounding region. The models are derived from long …

Seismic anisotropy allows us to study mantle deformation, and it can thus help to constrain
mantle flow in the vicinity of hotspots. Hypotheses for the cause of seismic anisotropy in this …

Data from two broadband, ocean‐bottom seismographic stations deployed∼ 225 km
southwest of Oahu, Hawaii during the Ocean Seismic Network Pilot Experiment provide …

We infer the lithospheric structure beneath the Hawaiian Swell based on a joint inversion of
ambient noise and teleseismic Rayleigh waves collected during the PLUME experiment …

We employ P to S converted waveforms to investigate effects of the hot mantle plume on
seismic discontinuities of the crust and upper mantle. We observe the Moho at depths …

We review evidence for plumelike upwellings beneath the Eifel, Great Basin, Hawaii, Afar,
and Iceland hotspots by using teleseismic shear wave splitting to resolve the anisotropy …

Split shear wave arrivals are analyzed in seismograms from local earthquakes in southern
Hawaii recorded at five temporary arrays and one permanent network station. We identify …