Results 91 to 100 of about 204 (113)
Seismological support for the metastable superplume model, sharp features, and phase changes within the lower mantle. [PDF]
Sun D, Tan E, Helmberger D, Gurnis M.
europepmc +1 more source
Temperature profile in the lowermost mantle from seismological and mineral physics joint modeling. [PDF]
Kawai K, Tsuchiya T.
europepmc +1 more source
Seismic low-velocity equatorial torus in the Earth's outer core: Evidence from the late-coda correlation wavefield. [PDF]
Ma X, Tkalčić H.
europepmc +1 more source
Mapping structures on the core–mantle boundary using Sdiff postcursors: Part II. Application to the Hawaiian ULVZ [PDF]
SUMMARY We present a new data set of nearly 100 earthquakes which show clear evidence of the Hawaiian ultra-low velocity zone (ULVZ) in the S core-diffracted phase (Sdiff), representing the most comprehensive Sdiff data set of a ULVZ to date.
Thomas Bodin, Sanne Cottaar, Carl Martin
exaly +4 more sources
A high-resolution map of Hawaiian ULVZ morphology from ScS phases [PDF]
We use core reflected ScS waves sensitive to a broad region of the core-mantle boundary beneath Hawaii to create the first high-resolution map of the Hawaiian ultralow-velocity zone (ULVZ).
Sima Mousavi, Sanne Cottaar, Zhi Li
exaly +3 more sources
Much of our knowledge on deep Earth structure is based on detailed analyses of seismic waveforms that often have small amplitude arrivals on seismograms; therefore, stacking is essential to obtain reliable signals above the noise level.
Samantha Hansen +2 more
exaly +2 more sources
Seismic Observation of a New ULVZ Beneath the Southern Pacific [PDF]
We present new observations of core‐diffracted shear waves which contain anomalous waveforms sampling the lowermost mantle beneath the southern Pacific region.
Sanne Cottaar, Zhi Li, Carl Martin
exaly +4 more sources
Detection of a ULVZ in the Central Pacific using high frequency Sdiff postcursors
In recent decades, ultra-low velocity zones (ULVZs) – thin patches of strongly reduced seismic velocity atop the core-mantle boundary (CMB) – have been inferred from observations of a variety of seismic phases.
Sanne Cottaar +2 more
exaly +1 more source

