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zhengyan
- 有限差分二阶二维声波方程正演模拟，加吸收边界变速剖面研究。 -Two-dimensional acoustic wave equation finite-difference second-order absorbing boundary variable cross-section study of Canadian
FDM2d
- 用二阶有限差分法的中心差分格式来模拟二维均匀介质中声波传播，震源子波是雷克子波-Finite difference method with second order central difference scheme to simulate two-dimensional wave propagation in uniform media, the source wavelet is a Ricker wave
FDM4d
- 用有限差分法的四阶差分格式模拟声波在二维均匀介质中的传播，不带吸收边界条件，震波是雷克子波-Finite difference method of fourth order difference scheme for two-dimensional simulation of acoustic wave propagation in uniform medium, without absorbing boundary condition, shock wave is Ricker
fd1
- 二维声波数值模拟正演程序，利用有限差分法，没有加入吸收边界-Numerical simulation of two-dimensional acoustic forward procedure, using the finite difference method, did not join absorbing boundary
fd
- 有限差分声波波动方程正演。主要用于地震勘探正演-Finite difference method of acoustic wave equation forward modeling
fd_forward
- 15度声波方程有限差分波场模拟，为有限差分偏移做正演资料准备。-Finite difference wave field simulation of 15 degree equation
SOFI3D
- 基于MPI的三维声波（粘弹性）有限差分正演模拟- 3-D viscoelastic, elastic, and acoustic wave simulation
SOFI2D
- 二维粘弹性声波方程有限差分模拟，可以模拟SV波- 2-D viscoelastic and elastic wave simulations for P- and SV-waves
code
- 二阶声波方程有限差分模拟和偏移成像的程序 文件说明： 数据为二进制，主程序用fdtrm.f90，数据为su格式，主程序用fdrtm_su.f90； boundary.f90人工边界条件，傍轴近似。propagator.f90是传播算子； wavelet.f90是震源。makefile中是编译命令。 -acoustic wave equation modeling and imaging with finite difference method
forward_12
- 该程序实现了声波方程空间高阶有限差分模拟，运用无分裂的PML边界降低了分裂边界的复杂程度(The program realizes the high order finite difference simulation of the acoustic equation space, the degree of complexity of the splitting boundary is reduced by using the non splitting PML boundary.)
地震波正演模拟
- 地震声波数值模拟，正演模拟，雷克子波，有限差分法，matlab