The use of parametric curves to define velocity models in seismic traveltime tomography is proposed. This approach provides increased flexibility in shaping the velocity models because it allows inversion for both velocity and grid point adjustments. The method is applied to a data set generated from a 1-D profile having sharp discontinuities. The results are compared with those obtained from other methods currently in use for traveltime tomography. It is found that large gradients and discontinuities can be retrieved with improved accuracy and that instabilities caused by non-optimal prior selection of the inversion grid can be avoided. The results appear to be robust when the sizes of both data and model space are reduced which makes the ...
Abstract. Spatial gradients of tomographic velocities are seldom used in interpretation of subsurfac...
A method is presented for deriving 1-D velocity depth models from earthquake bulletin data. The mod...
Seismic tomography is a well-established approach to invert smooth macro-velocity models from kinema...
To better assess quality of three-dimensional (3-D) tomographic images and to better define possible...
We present a new 2-D traveltime tomography method for the inversion of densely sampled seismic strea...
In conventional migration velocity analysis methods, a velocity model is estimated that results in f...
A seismic traveltime inversion method is proposed for building smooth velocity models using travelti...
We have developed an inversion formulation for velocity and attenuation structure using seismic attr...
The measured traveltimes of specular reflection events are inverted to obtain a low spatial frequenc...
We have developed an inversion formulation for velocity and attenuation structure using seismic attr...
A dense wide-angle data set is used to test a two-step procedure for the separate inversion of first...
Further development of the theory and practice of the method for solving the inverse problem of seis...
Geophysical Journal International, v. 151, n. 1, p. 264-278 [452], 2002International audienceWe have...
Walkaway vertical seismic profiling (WVSP) is known for its high level of credibility in obtaining t...
A back projection method of reconstruction is adapted to invert seismic travel time data for velocit...
Abstract. Spatial gradients of tomographic velocities are seldom used in interpretation of subsurfac...
A method is presented for deriving 1-D velocity depth models from earthquake bulletin data. The mod...
Seismic tomography is a well-established approach to invert smooth macro-velocity models from kinema...
To better assess quality of three-dimensional (3-D) tomographic images and to better define possible...
We present a new 2-D traveltime tomography method for the inversion of densely sampled seismic strea...
In conventional migration velocity analysis methods, a velocity model is estimated that results in f...
A seismic traveltime inversion method is proposed for building smooth velocity models using travelti...
We have developed an inversion formulation for velocity and attenuation structure using seismic attr...
The measured traveltimes of specular reflection events are inverted to obtain a low spatial frequenc...
We have developed an inversion formulation for velocity and attenuation structure using seismic attr...
A dense wide-angle data set is used to test a two-step procedure for the separate inversion of first...
Further development of the theory and practice of the method for solving the inverse problem of seis...
Geophysical Journal International, v. 151, n. 1, p. 264-278 [452], 2002International audienceWe have...
Walkaway vertical seismic profiling (WVSP) is known for its high level of credibility in obtaining t...
A back projection method of reconstruction is adapted to invert seismic travel time data for velocit...
Abstract. Spatial gradients of tomographic velocities are seldom used in interpretation of subsurfac...
A method is presented for deriving 1-D velocity depth models from earthquake bulletin data. The mod...
Seismic tomography is a well-established approach to invert smooth macro-velocity models from kinema...