An efficient implementation of the free surface boundary condition in 2-D and 3-D elastic cases

Earth and Planetary Sciences

• Boundary Condition 100%
• Finite Difference Method 50%
• Elasticity 50%
• Heterogeneous Medium 50%
• Earth Surface 50%
• Receiver 50%
• Seismogram 50%
• Wave Modeling 50%
• Model 50%
• Cost 50%
• Inversion 50%
• Increasing 50%
• Approach 50%
• Estimate 50%
• Difference 50%
• Amplitude 50%
• Seismic Wave 50%
• Rayleigh Wave 50%
• Information 50%