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Toeplitz matrix
Seismic sparse-spike deconvolution via Toeplitz-sparse matrix factorization
A depiction of stationary convolution ( equation 1 ) as a Toeplitz matrix, ...
A fast reduced-rank interpolation method for prestack seismic volumes that depend on four spatial dimensions
Multidimensional simultaneous random plus erratic noise attenuation and interpolation for seismic data by joint low-rank and sparse inversion
The use of the conjugate-gradient algorithm in the computation of predictive deconvolution operators
Elimination of temporal dispersion from the finite-difference solutions of wave equations in elastic and anelastic models
Non-Gaussian reflectivity, entropy, and deconvolution
The product of the filters in Figures A-1 and A-2 , represented as matri...
A nonstationary sparse spike deconvolution with anelastic attenuation
Partitioned least-squares operator for large-scale geophysical inversion
Convolutional equivalent layer for gravity data processing
Automatic blind deconvolution with Toeplitz-structured sparse total least squares
Blind sparse-spike deconvolution with thin layers and structure
Convolutional equivalent layer for magnetic data processing
Illustration of nonstationary convolution as described by equation 9 . Lik...
Abstract The spectral estimation problem for a discrete-time series generated by a linear, time-invariant process can be formulated in terms of three models: autoregressive (AR), moving average (MA), and autoregressive-moving average (ARMA). Analysis procedures differ in each case, and specification errors arise due to application of the inappropriate algorithm. The AR and MA models lead respectively to the maximum entropy (MEM) and classical lag-window approaches. The ARMA model has much seismic interest because the unit impulse response of a horizontally stratified medium is expressible in this way. Since its feedback component has the minimum-delay property, an ARMA spectral estimation technique satisfying this requirement has particular seismic relevance. Such a spectral estimate results from the application of an iterative least-squares algorithm to selected gates of the observed time series. A sample set of synthetic time series serve to illustrate the degradation in the spectral estimate resulting from an incorrect specification of the model.