The original publication can be found at www.springerlink.com Copyright © 2005 Birkhauser Verlag, BaselIn this paper we present an approach for 3-D travel-time tomography, which works well in reconstructing high contrast velocity anomalies in both location and strength. It uses a revised ‘irregular’ approach to the shortest-path method as the ray tracer and a damped minimum norm, and constrained least-squares CG approach as the inversion solver. In ray tracing, the advantages of the revised ‘irregular’ over the ‘regular’ approach are that the secondary nodes introduced on the cell surfaces significantly improve accuracy of computed travel times, without dramatically increasing the total number of cells and nodes; the tri-linear velocity fun...
International audienceWe present a new 3-D travel-time tomography code (TOMO3D) for the modelling of...
The determination of a correct subsurface velocity model is of strategic importance for seismic imag...
The convergence of conventional reflection tomography is often uncer-tain when the starting velocity...
The use of 1D or pseudo- 3D ray tracing techniques in linearized tomographic problems leads to solut...
International audienceWe present a new method of traveltime tomography. In this method, the travelti...
The definitive version is available at www.blackwell-synergy.comWe have developed two, new non-linea...
Fermat's principle shows that a definite convex set of feasible slowness models -- depending on...
I performed traveltime tomography on a 3-D seismic refraction dateset collected at Hill Air Force Ba...
Traditional straight ray- and curved ray-based tomography algorithms need to perform ray tracing to ...
Some test studies were performed for comparison of two travel-time inversion schemes for tomographic...
An approximate inversion formula is proposed for the reconstruction of slowness anomalies in a known...
Conventional crosswell direct-arrival traveltime tomography solves for velocity in a 2-D slice of th...
77th Earth Science for Energy and Environment (EAGE) Conference & Exhibition 2015, 1-4 June 2015, Ma...
International audienceClassical 3-D refraction traveltime tomography algorithms may suffer from comp...
Seismic tomography is a well-established approach to invert smooth macro-velocity models from kinema...
International audienceWe present a new 3-D travel-time tomography code (TOMO3D) for the modelling of...
The determination of a correct subsurface velocity model is of strategic importance for seismic imag...
The convergence of conventional reflection tomography is often uncer-tain when the starting velocity...
The use of 1D or pseudo- 3D ray tracing techniques in linearized tomographic problems leads to solut...
International audienceWe present a new method of traveltime tomography. In this method, the travelti...
The definitive version is available at www.blackwell-synergy.comWe have developed two, new non-linea...
Fermat's principle shows that a definite convex set of feasible slowness models -- depending on...
I performed traveltime tomography on a 3-D seismic refraction dateset collected at Hill Air Force Ba...
Traditional straight ray- and curved ray-based tomography algorithms need to perform ray tracing to ...
Some test studies were performed for comparison of two travel-time inversion schemes for tomographic...
An approximate inversion formula is proposed for the reconstruction of slowness anomalies in a known...
Conventional crosswell direct-arrival traveltime tomography solves for velocity in a 2-D slice of th...
77th Earth Science for Energy and Environment (EAGE) Conference & Exhibition 2015, 1-4 June 2015, Ma...
International audienceClassical 3-D refraction traveltime tomography algorithms may suffer from comp...
Seismic tomography is a well-established approach to invert smooth macro-velocity models from kinema...
International audienceWe present a new 3-D travel-time tomography code (TOMO3D) for the modelling of...
The determination of a correct subsurface velocity model is of strategic importance for seismic imag...
The convergence of conventional reflection tomography is often uncer-tain when the starting velocity...