搜索资源列表
sunday
- 当把m个信号叠加在一起时,经倒谱分析是能检测出其基频。但倒谱分析主要是用在同态滤波中,可用于某些信号的解褶积。例如提供的语音信号,就能通过倒谱把频谱中的包络和基频频谱分离,
xiangguan
- 一种反褶积程序所要的算法可直接使用次程序,谢谢使用,欢迎联系
fanzheji
- 一个反褶积的VC++例子,简单明了,很适合刚刚开始学习信号分析的人
稀疏脉冲盲源反褶积
- 稀疏脉冲盲源反褶积
wuFengTTFZJ1
- 本程序主要是对资料进行同台反褶积,对资料进行处理,提高资料的分辨率,能更好的观察到其中的细节部分。-This program information on the same stage deconvolution, data processing to improve the resolution of the data, the details of which can better observed.
work3
- 计算普通褶积与循环褶积,分别使用时间域与频率域两种方法进行正、反演计算,指出循环褶积计算时所存在的边界效应现象;编写一个做相关分析的源程序-Ordinary convolution and circular convolution, respectively, using the two methods of time domain and frequency domain inversion calculation, pointing out that the phenomenon of ci
one_demison_seismicrecord
- 褶积合成一维地震记录,速度和反射系数值自己给出-Convolution synthesis of one-dimensional seismic records, speed and reflectance values given
zhejixiugai
- 用于计算两个未知长度信号的褶积程序,它可以作为反滤波中的一个小模块使用-Used to calculate the two signals of unknown length convolution procedure, it can act as inverse filtering in a small module
Least-square-deconvolution
- 最小平方反褶积的相关程序,可用于相关地震资料的处理和分析-Least squares deconvolution procedures, can be used for correlation of seismic data processing and analysis
Untitled6
- 预测反褶积matlab编码,适合初学者学习和使用-predictive deconvlution
A-one-dimensional-convolution
- 一维褶积 雷克子波与地层序数 地震资料正演方法-One-dimensional convolution Ricker wave formation ordinal
dizhengdao
- 合成地震记录是用声波测井或垂直地震剖面资料经过人工合成转换成的地震记录(地震道) 合成记录的制作是一个简化的一维正演的过程,合成记录F(t)是地震子波S(t)与反射系数R(t)褶积的结果。-Synthetic seismogram is sonic or vertical seismic profile data after conversion into synthetic seismograms (seismic trace) the production of synthetic se
predictive
- 地震反褶积运算,主要是对地震的成像波形进行滤波处理和对一些运算进行整理-Seismic deconvolution
predictive
- 地表一致性反褶积就是用预测的方法进行反褶积-Surface consistent deconvolution method is to use predictive deconvolution
spiking
- 脉冲反褶积时期望输出零延迟的尖脉冲的最小平方反褶积方法-Output zero latency spikes least squares deconvolution method expects pulse deconvolution
sparse_decon
- 稀疏脉冲反褶积是一种从地震记录中估计振幅和位置的反演方法。-Sparse deconvolution is a pulse inversion method estimates the amplitude and position seismic records.
kolmog
- 最小平方反褶积是把地震子波压缩成尖脉冲,从而使地震记录能够直接反映地下反射系数序列-Least squares deconvolution of seismic waves are compressed into spikes, which can directly reflect the seismic record subsurface reflection coefficient series
ls_inv_filter
- 子波整形反褶积是通过所设计的整形滤波器对地震子波,使其成为所期望的形状。-Shaping wavelet deconvolution by shaping filter designed for seismic waves, making it the desired shape.
zheji
- 用子波与反射系数进行褶积来模拟地震波的传播。-Convolution performed to simulate seismic wave propagation using wavelet and reflection coefficient.
7
- 验证时间域的循环褶积对应的是频率域的乘积;线性褶积则不然-Cycle time convolution corresponding authentication domain is the product of the frequency domain otherwise the linear convolution