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ricker
- 地震中的雷克子波，可以根据需要进一步开发！-Lake of the seismic wavelet, based on the need for further development!
AnalyticAnelastic
- 二维粘弹性介质中波的传播的解析形式。应用Carcione等在1988年发表的《WAVE PROPAGATION SIMULATION IN A LINEAR VISCOELASTIC MEDIUM》一文中的方法，更加详细的介绍见英文描述。该代码对于做波场模拟的同学有很好的参考价值。- MATLABscr ipt for obtaning the analytical solution for 2D wave propagation in a viscoelastic medium, based
Analytical_Poroelastic
- 各向同性空隙介质中波的传播的解析形式，应用下文的方法： Dai, N., Vafidis, A. & Kanasewich, E.R., 1995. Wave propagation in heterogeneous, porous media: A velocity-stress, finite-difference method, Geophysics, 60, 327-340. 更加详细的介绍见英文描述，该代码对于做波场模拟的同学有很好的参考价值。-MATLAB scr ip
souceanalycse
- 主要针对震源雷克子波的空间衰减因子对正演模拟的影响所进行的有限差分正演-The main source of space for Ricker wave attenuation factor of the forward modeling conducted by finite difference forward
Richar-wavelet
- 雷克子波是地震勘探中广泛应用的一种子波，作为震源向地下传播，经过反射界面后反射回地面被接受。-Ricker wavelets wave is a widely used in seismic exploration, communication to the ground as the source, after reflection interface reflection back to the ground to be accepted.
zheji
- 利用反褶进行的褶积运算合成地震记录。子波使用雷克子波，长度为Nw，Nt为反射系数长度，Nx为道数。提供四个地下模型：水平界面，两层水平界面，绕射界面和倾斜界面。输出二进制文件。-Use convolution operation performed deconvolution synthetic seismogram. Ricker wavelets using wave length Nw, Nt is the reflection coefficient length, Nx is the