Global Mantle Structure

Photos

Imaging the Anisotropic Shear-wave Velocity Structure of the Earth’s Mantle
The Global Short-Period Wavefield Modeled with a Monte Carlo Seismic Phonon Method
Investigating Attenuation and Velocity Structure from Surface-Wave Amplitudes
Study of Earth’s Layered Structure on a Global Scale Using Broadband Seismic Datasets - fig. 1
Study of Earth’s Layered Structure on a Global Scale Using Broadband Seismic Datasets - fig. 2
Study of Earth’s Layered Structure on a Global Scale Using Broadband Seismic Datasets - fig. 3
Seismic Evidence for Accumulated Oceanic Crust Above the 660-km Discontinuity Beneath Southern Africa - fig. 1
Seismic Evidence for Accumulated Oceanic Crust Above the 660-km Discontinuity Beneath Southern Africa - fig. 2
A Three-Dimensional Radially-Anisotropic Model of Shear Velocity in the Whole Mantle - fig. 2
A Three-Dimensional Radially-Anisotropic Model of Shear Velocity in the Whole Mantle -fig. 1
Discovery of Strong Upper Mantle Reflectors From Back-Scattering of Near-Podal PKPPKP Waves Using Data Acquired From IRIS - fig. 1
Discovery of Strong Upper Mantle Reflectors From Back-Scattering of Near-Podal PKPPKP Waves Using Data Acquired From IRIS - fig. 2
Global Analysis of Upper Mantle Anisotropy Using Automated SKS Splitting Measurements
Global Tomographic Model of Q in the Upper Mantle Obtained Using Long-period Waveform Data
Global Anisotropy and the Thickness of Continents
Seismic Investigation of Upper and Lower Mantle Boundary Layering
SH Velocity and Compositional Models Near the 660-km Discontinuity Beneath South America
New Measurements of Radial Mode Eigenfrequencies
Whole-Mantle 3D Seismic Attenuation: Evidence for Global Mass Flux
Using IRIS Digital Data to Determine the Radial Attenuation Structure of the Lower Mantle
Probing the Earth’s Interior by Stacking Stacked Short-Period Seismic Array Data
Compressional-Wave Studies on the Frequency Dependence of and Lateral Variations in Mantle Attenuation - fig. 1
Compressional-Wave Studies on the Frequency Dependence of and Lateral Variations in Mantle Attenuation - fig. 2

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