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acoustic
- 交错网格声波方程交错网格有限差分地震波场计算波场正演模拟。 -The CalCulation of the SeismiC Wave一 fieldwith Staggered-grid Finite difference Sheme
bigplot
- 声波方程正演模拟大模型样例。 包含三个地质层，分别对应速度可以自行修正。 震源函数是雷克子波。 C源程序，输出结果Matlab绘制。-Acoustic wave equation forward modeling big model of the sample. Consists of three geological layers, corresponding to the speed you can correct itself. Lake wavelet source func
wave
- 这个主要是讲解声波方程数值模拟的，实现了无反射波动正演，可应用与非均匀介质有两种吸收边界条件-This is mainly to explain the numerical simulation of acoustic wave equation, to achieve a non-reflective wave forward, can be applied with non-uniform medium, there are two absorbing boundary conditions
shengbosijie
- 自己利用有限差分法编写的时间二阶空间四阶的声波数值模拟正演程序，没有加入吸收边界-Write your own time using finite difference method of second spatial fourth-order acoustic wave simulation program, did not join absorbing boundary
regular
- 实现了规则网格下的声波波动方程有现车分正演模拟，时间2阶空间4阶-Achieve the acoustic wave equation under the rules of the grid there are cars of forward modeling, time 2 order spatial order 4
staggered-grid
- 实现了声波波动方程有限差分正演模拟，交错网格下，时间2阶空间10阶-Achieve the acoustic wave equation finite difference forward modeling, staggered under the grid, the time second-order space 10 order
wave1d
- 一维声波方程波动方程正演模拟，有输入输出接口-One-dimensional acoustic wave equation forward modeling equations, input and output interfaces
finitedif
- 有限差分正演模拟 声波 高阶 包含边界条件 震源方程-finite difference code with boundary condition and source function
FDM-shengbofangchengzhengyan
- 有限差分声波方程正演模拟，适合于做地震勘探初学者的学习-Acoustic wave equation finite difference forward modeling, suitable for beginners learning to do seismic exploration
shengbo
- 三维声波正演模拟的matlab程序 边界条件为pml- Three dimensional acoustic wave forward simulation of matlab program
seismic_wave
- 程序实现了均匀介质、分层介质中规则网格声波有限差分的正演模拟。(The program realizes the forward modeling of sound wave propagation in homogeneous medium and layer homogeneous medium using finite difference method with regular grid.)
wavefront
- 本实验应用声波方程作为正演模拟的波动方程，将所提供震源函数离散后绘图，并将给定两个二维速度 -深度模型，绘出图形。(In this experiment, we use the acoustic equation as the wave equation of forward modeling, draw the source function and draw it, and give two two-dimensional velocity depth models to draw the