搜索资源列表
Synthetic
- 人工合成记录的程序，子波为Ricker子波-synthetic documented procedure for the wave-wave Ricker
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
ziboazheji$xiangguan
- 雷克子波函数，褶积过程子函数，两序列相关函数三个C程序 -The Ricker wave function, the convolution process subfunction, the correlation function of the two sequences three C program
hecheng_dizhenjilu
- 通过卷积实现合成地震记录的制作，其中所运用子波为雷克子波，也可根据自己的需要进行相应修改 -Achieved by convolution the synthetic seismogram production , including the use of sub- wave Ricker wave , but also according to their needs accordingly modified
rk
- 雷克子波，地震记录处理中必须用到的很有用的子波，是合成记录的关键-Ricker wavelet, seismic recording process must be used very useful sub-wave synthetic seismogram is the key
Ricker_model
- 用褶积模型编写的地震合成记录，适用于自激自收情况，子波选用雷克子波-Convolution model prepared by synthetic seismic records for self-excited self closing conditions Ricker wavelets wave selection
wavelet
- 地震数据处理中常用的子波，包括雷克子波，带通子波，Klauder wavelet等-Commonly used in seismic data processing wavelets, including Ricker wave bandpass wavelets, Klauder wavelet, etc.
seismic-data-syn
- 反射系数与地震子波褶积合成地震记录，p，d，s分别是预设地层纵波速度、密度、及横波速度模型。其中包含可以改变主频的ricker子波，avopp是提取反射系数的程序。wigb可以对其中的多道进行强化显示。-Reflection coefficient and the convolution synthetic seismogram, the seismic wavelet p, d, s are preset formation p-wave velocity, density, and shea
shenboRTm
- 内容包括声波的rtm，ricker子波以及plotimage。另外还有相关的一些论文-Including acoustic rtm, ricker wavelets and plotimage. There are also some related papers
ricker-and-klauder
- 地震子波MATLAB成图，包括ricker子波和klauder子波。-Seismic wavelet MATLAB mapping, including ricker klauder wavelet and wavelet.
model
- 利用褶积原理合成地震记录，震源子波用的是雷克子波，适合初学者进行练习使用。-Use convolution principle of synthetic seismograms, with the source wavelet is Ricker wave, suitable for beginners to practice use.
matlab Ricker
- 地震勘探 AVO正演 雷克子波 运用雷克子波和反射系数进行褶积得到合成地震记录(matlab ricker The seismic record obtained by convolution of rec wavelet and reflection coefficient is one-dimensional, and the AVO response can be identified by the seismic record)