Earth and Planetary Sciences
Adjoint Method
67%
Adjoints
91%
Africa
6%
Anelasticity
17%
Arizona
9%
Bathymeter
27%
Bolivia
10%
Centroid Moment Tensor
17%
Continuum Mechanics
19%
Core-Mantle Boundary
20%
Coupled Mode
10%
Cross Correlation
17%
Crosstalk
5%
Crustal Thickness
7%
Degree of Freedom
14%
Diffraction
50%
Directivity
8%
Distributed Memory
9%
Earth Mantle
17%
Earth Surface
5%
Eigenvector
6%
Elastic Wave
10%
Equation of Motion
28%
Fault Geometry
6%
Forward Modeling
21%
Full-Waveform Inversion
70%
Geographical Variation
6%
Geological Structure
8%
Geopotential
7%
Gravity Anomaly
6%
Ground Motion
22%
Harmonics
13%
Helioseismology
5%
Iceland
7%
Infinite Element Method
7%
Inner Core
40%
Inverse Problem
21%
Japan
10%
Laplace Equation
5%
Love Wave
14%
Mantle Structure
13%
Mathematical Method
11%
Microseism
9%
Moment Tensor
14%
Mountain Range
7%
Natural Gas Exploration
8%
Near-Surface Geology
15%
Ocean Tide
7%
Oil Exploration
8%
Pacific Ocean
6%
Parallel Computer
14%
Rayleigh Wave
10%
Reaction Time
12%
Real Time
9%
Rheology
10%
Scattering
6%
Sea Bed
8%
Sedimentary Basin
12%
Seismic Attenuation
6%
Seismic Data
27%
Seismic Monitoring
6%
Seismic Noise
6%
Seismic Tomography
21%
Seismic Wave
52%
Seismic Wave Propagation
100%
Seismicity
10%
Seismogram
25%
Seismographs
8%
Seismology
50%
Solar Interior
8%
Source Parameter
8%
Southern California
10%
Subduction Zone
5%
Surface Wave
88%
Synthetic Seismogram
50%
Taiwan
12%
Tibet
14%
Time Function
5%
Tomography
79%
Travel Time
18%
United States
7%
United States of America
9%
Upper Mantle
9%
Vertical Seismic Profile
7%
Wave Equation
22%
Wave Velocity
25%
Waveform Modeling
10%
Waveguide
7%
Keyphrases
Adjoint Method
11%
Adjoint Tomography
9%
Anisotropy
14%
Anomalous Splitting
5%
Attenuation
7%
Bathymetry
6%
Beowulf
9%
Diagonal Mass Matrix
7%
Earth Model
12%
Earth Simulator
11%
Earth's Free Oscillations
6%
Earth's Inner Core
6%
Earth's Mantle
7%
Earthquake
7%
Elastic Full-waveform Inversion
5%
Elastic Modulus
9%
Elasticity Tensor
6%
Equations of Motion
8%
Finite Element Method
8%
Finite Frequency
6%
Frequency Sensitivity
6%
Full-waveform Inversion
6%
HPC Cluster
5%
Inner Core
9%
Irregular Topography
5%
Lateral Heterogeneity
7%
Lithospheric Foundering
14%
Misfit Function
7%
Parallel Computer
5%
Pseudospectral Method
9%
Seismic Wave Propagation
22%
Seismic Waves
7%
Seismology
9%
Sensitivity Kernel
6%
Southern California
9%
Spectral Element
8%
Spectral Element Method
27%
Spectral Element Simulation
9%
Stress Dependence
9%
Surface Waves
8%
Synthetic Seismogram
9%
Third-order Elasticity
7%
Three-dimensional Seismic
6%
Tibet
14%
Travel Time
6%
Underthrusting
14%
Velocity Model
6%
Wave Propagation
9%
Wave Speed
5%
Weak Formulation
9%
Engineering
Anisotropic
22%
Axisymmetric
7%
Azimuthal
8%
Compressional Wave
14%
Computational Cost
8%
Constrains
6%
Cross-Coupling
6%
Eigenvector
10%
Element Method
45%
Finite Element Method
8%
Free Surface
7%
Frequency Kernel
6%
Full-Waveform Inversion
10%
Gauss
12%
Geometrical Spreading
7%
Global Scale
5%
Harmonics
6%
Illustrates
7%
Induced Stress
9%
Infinite Element
14%
Internals
19%
Interpolants
7%
Magnetic Field
7%
Mass Matrix
11%
Model Parameter
10%
Normal Modes
37%
Parallel Computer
8%
Phase Speed
10%
Rheology
5%
Seismic Wave Propagation
33%
Shear Wave
12%
Stress Measure
9%
Tensor Moment
12%
Time Domain
6%
Young's Modulus
11%
