We apply a deconvolution approach to the problem of determining the input motion at the base of an instrumented borehole using only a pair of recordings, one at the borehole surface and the other at its bottom. To stabilize the bottom-tosurface spectral ratio, we apply an iterative regularization algorithm that allows us to constrain the solution to be positively defined and to have a finite time duration. Through the analysis of synthetic data, we show that the method is capable of retrieving reliable input motion, suppressing the effect of the negative interference generated by the downgoing waves. Results obtained by applying the methodology to weak earthquakes recorded at the Ataköy (Istanbul) vertical array are also presented and show ...
Receiver functions (RFs) are derived by deconvolution of the horizontal (radial or transverse) compo...
Receiver functions (RFs) are derived by deconvolution of the horizontal (radial or transverse) compo...
Seismic interferometry is a method to retrieve Green’s functions for sources (or receivers) where th...
We apply a deconvolution approach to the problem of determining the input motion at the base of an ...
Abstract We apply a deconvolution approach to the problem of determining the input motion at the bas...
We use seismic interferometry by deconvolution to estimate the travel time between two receivers loc...
We use seismic interferometry by deconvolution to estimate the travel time between two receivers loc...
The estimation of shear-wave velocity and attenuation in near-surface geology is of primary importan...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
In seismic imaging the aim is to obtain an image of the subsurface using reflection data. The reflec...
Seismic interferometry is a method to retrieve Green’s functions for sources (or receivers) where th...
Receiver functions (RFs) are derived by deconvolution of the horizontal (radial or transverse) compo...
Receiver functions (RFs) are derived by deconvolution of the horizontal (radial or transverse) compo...
Seismic interferometry is a method to retrieve Green’s functions for sources (or receivers) where th...
We apply a deconvolution approach to the problem of determining the input motion at the base of an ...
Abstract We apply a deconvolution approach to the problem of determining the input motion at the bas...
We use seismic interferometry by deconvolution to estimate the travel time between two receivers loc...
We use seismic interferometry by deconvolution to estimate the travel time between two receivers loc...
The estimation of shear-wave velocity and attenuation in near-surface geology is of primary importan...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
International audienceThe near-surface shear-wave attenuation characteristics of a site are crucial ...
In seismic imaging the aim is to obtain an image of the subsurface using reflection data. The reflec...
Seismic interferometry is a method to retrieve Green’s functions for sources (or receivers) where th...
Receiver functions (RFs) are derived by deconvolution of the horizontal (radial or transverse) compo...
Receiver functions (RFs) are derived by deconvolution of the horizontal (radial or transverse) compo...
Seismic interferometry is a method to retrieve Green’s functions for sources (or receivers) where th...