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- Upper mantle discontinuities
- Upper mantle composition
- Upper mantle velocity models
- Model of Gutenberg discontinuity by Gaherty et
al. (1999)
- Velocity change due to anisotropy change
- ScS reverberation phases
- Z, R, T and L, Q, T coordinate systems
- PKPPKP and PP
- SS and PP long-period stacks
- YKA location
- YKA configuration
- Tw~st array configuration
- Source locations of YKA dataset
- YKA reflection point location
- PP Fresnel zone
- Source locations of the Tw~st array dataset
- Tw~st array reflection point location
- Filter effects
- frequency-wavenumber analysis: Examples
- IASP91 travel time curves
- Sliding-window fk-analysis resolution test
- fk-analysis slowness resolution test
- Sliding-window fk-analysis backazimuth resolution test
- Snapshots of sliding-window fk-analysis for real event
- Seismogram and vespagram example
- PP - P travel times study
- Seafloor age in the region studied
- Results for shallow reflectors
- Vertical cross section for shallow reflections
- PP and P
P polarity study
- Polarity studies of shallow reflectors
- Results for Lehmann discontinuity
- Vertical cross section for Lehmann discontinuity
- Vertical cross section for intermediate depths
- Results for 410 km discontinuity
- Vertical cross section for reflections from the 410 km
discontinuity
- Vertical cross section for reflections from the 410 km discontinuity
at the tip of the Hawaiian chain
- Vespagram for SS underside reflections
- Particle motion for station 5150
- Depth variations of shallow discontinuities
- 4th-root vespagrams of synthetic seismograms and real
data
- Laminated models of Lehmann discontinuity
- 210 km reflection points near the Kurile subduction zone
- Effect of increasing width of a discontinuity
- Synthetic seismograms for variations of gradient thickness and
impedance contrast
- Thickness and velocity jump across the Lehmann
discontinuity
- Location of 410 reflections near the Kurile subduction
zone
- Structure of the 410-km discontinuity by Flanagan and Shearer
(1999)
- Synthetic seismograms for 410-km discontinuity models
- Synthetic seismograms for different models of the 660
- Grid search for gradient and impedance change at 660
2000-09-05