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Core-Mantle Boundary

Photos

Lateral Variation of the D” Discontinuity Beneath the Pacific - fig. 1	Lateral Variation of the D” Discontinuity Beneath the Pacific - fig. 2	Observation of P-Wave Velocity Discontinuities in D’’ Beneath Southeast Asia Using Migration Techniques	Lowermost Mantle Anisotropy Beneath the Central Pacific
A Strong Lateral Shear Velocity Gradient and Anisotropy Heterogeneity in the Lowermost Mantle Beneath the Southern Pacific - fig	A Strong Lateral Shear Velocity Gradient and Anisotropy Heterogeneity in the Lowermost Mantle Beneath the Southern Pacific - fig	D” Shear Velocity Heterogeneity, Anistropy, and Discontinuity Structure Beneath the Caribbean - fig. 1	D” Shear Velocity Heterogeneity, Anistropy, and Discontinuity Structure Beneath the Caribbean-fig. 2
Isotropy or Weak Vertical Transverse Isotropy in D” Under the Atlantic - fig. 1	Isotropy or Weak Vertical Transverse Isotropy in D” Under the Atlantic - fig. 2	Finite-Frequency Tomography of D” Shear Velocity Heterogeneity Beneath the Caribbean	Sharp Lateral Boundaries in the D” Region
Using Array Methods to Investigate Possible Causes for PKP Deviations	A Step in the D” Discontinuity Imaged by Kirchoff Migration Through 3D Tomographic Models - fig. 1	A Step in the D” Discontinuity Imaged by Kirchoff Migration Through 3D Tomographic Models - fig. 2	Lateral Variation of P- and S-Wave Velocity Discontinuities in the Lower Mantle Beneath the Cocos Plate - l
Lateral Variation of P- and S-Wave Velocity Discontinuities in the Lower Mantle Beneath the Cocos Plate - r	Lateral Variation of the D” Discontinuity Beneath the COCOS Plate - fig. 1	Lateral Variation of the D” Discontinuity Beneath the COCOS Plate - fig. 2	MGLF_Fig.jpg
D” Anistropy From Lamellae and Transverse Isotropy - fig. 1	D” Anistropy From Lamellae and Transverse Isotropy - fig. 2	Examining the Base of the Mantle Using IRIS FLED PASSCAL Data - fig. 1	Examining the Base of the Mantle Using IRIS FLED PASSCAL Data - fig. 2
Detection of an Ultralow Velocity Zone at the CMB Using Diffracted PKKPab Waves - fig1 $Detection of an Ultralow Velocity Zone at the CMB Using Diffracted PKKPab Waves - fig1$	Detection of an Ultralow Velocity Zone at the CMB Using Diffracted PKKPab Waves-fig.2 $Detection of an Ultralow Velocity Zone at the CMB Using Diffracted PKKPab Waves-fig.2$	Migration of the Lowermost Mantle Structure Under the COCOS - fig. 1	Migration of the Lowermost Mantle Structure Under the COCOS - fig. 2
A Seismological Determination of the Temperature Gradient in D” Beneath the Western Pacific

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