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bigmodel
- 声波方程正演模拟包含波前快照和地震记录。采用时间二阶空间四阶的精度。以雷克子波为震源函数-Acoustic wave equation contains forward modeling and seismic records before the snapshot. Second order in space using the time fourth-order accuracy. Wave function for the source to Ricker
T-method.rar
- 试射法——射线追踪程序。 可分别做直达波,折射波,反射波。 射线正演模拟入门程序之一!!,Test method- ray-tracing procedures. Can be done direct wave, refracted wave, reflected wave. Ray is one of forward modeling procedure entry! !
ELASTIC_2D_PML
- 在二维介质下,引入PML边界条件的弹性波方程正演模拟-In a two-dimensional media, the introduction of the PML boundary conditions for the elastic wave equation forward modeling
Youxianchafen
- 此程序用Fortran语言编写,为弹性波动方程在均匀介质中的有限差分解,可进行地震波的正演模拟-This procedure Fortran language used for the elastic wave equation in inhomogeneous media in the finite difference decomposition can be carried out seismic forward modeling
jiaocuo2_10jie
- 弹性波方程的地震波场的正演模拟,采用的是高阶精度--10阶,但是还没加边界-Elastic wave equation of seismic wave field forward modeling, using the high-order accuracy- 10 bands, but not Canadian border
Finitedifferencemodeling
- 有限差分进行地震波正演模拟的源代码,可以修改模型参数,另附有剖面的现实软件!-Finite-difference modeling of seismic wave is the source code, you can modify the model parameters, attached a profile of the reality of the software!
ray__tracing__fortran
- 主要用于地震正演,适当修改可以用作电磁波的正演-Mainly used in seismic modeling, appropriate changes can be used as electromagnetic wave forward
B3D
- 地震勘探3维波动方程边界元正演模拟程序 源代码,非常经典-Seismic 3-dimensional wave equation boundary element forward modeling program source code, very classic
finite_difference11
- 声波方程规则网格的PML边界条件正演模拟 -acoustic wave equation modeling
3D-FD-time-domain-modeling
- 3D finite-difference time-domain modeling of acoustic wave propagation base on domain decomposition
crack_KTB
- 岩石物理建模的程序,在弹性参数与物性参数关机,以及横波速度估算等领域可以应用-Rock physics modeling procedures, shut down in the elastic parameters and material parameters, and the shear wave velocity estimation can be applied to the field
Acoustic_Model_Hybrid-ABC
- 实现2D声波方程正演,用于地球物理勘探中的声波正演-Achieve 2D acoustic wave equation forward modeling for geophysical exploration sonic Forward
Phase-shifting-prestack-modeling
- 用相位移加实现速度纵横向变化、复杂陡倾地质模型的正流模拟,为复杂波场的地震、地质解释提供了精确、实用的方法。一般情况下,相位移延拓方法对徒倾斜地层成像精度高、稳定性好、计算快,但实现速度的横向变化困难;而频率、空间域的有限差分法算法简单、稳定性好、能适应速度的纵横向任意变化,但偏移陡断地层存在很多问题-Using phase shift and realization of vertical velocity variations, complex flow simulation of stee
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
Wave-equation-forward-modeling
- C++的波动方程正演,有限差分,虚谱法。二维,三维都有-Wave equation forward modeling
forward.tar
- 勘探地球物理中的地震波传播模型正演问题相关程序-Exploration Geophysics forward modeling of seismic wave propagation problems associated program
separation-of-p-and-s-wave
- 二维交错网格纵横波分离的弹性波正演模拟 matlab仿真-Two-dimensional staggered grid of p-wave elastic wave forward modeling of the separation of the matlab simulation
elastic-wave-forward-modeling
- 地球物理专业旋转交错网格弹性波正演模拟实验 matlab仿真 -Geophysical professional rotary staggered grid elastic wave forward modeling matlab simulation experiment
wm
- 水面无人艇(Unmanned Surface Vehicle)的航迹控制对提升无人艇艇载设备 侦察观测效果以及多任务作战能力具有十分ffi要的意义。由于受到风、浪、流等 干扰环境影响,水而无人艇将产生六自由度的操纵运动,具有很强的非线性和随 机性。这将致使无人艇的航向航迹及姿态控制具有一定的难度,因此需要对水面 无人艇建立六自由度操纵模型,更好地实现对无人艇的控制。 采用经典的MMG分离建模思想,依托浜本刚实提出的水平附体坐标系,建 立
chengxu
- 波动方程正演模拟,交错网格二阶和四阶,和规则网格。适合新手学习。-Wave equation forward modeling, suitable for beginners to learn.