The use of 1D or pseudo- 3D ray tracing techniques in linearized tomographic problems leads to solutions for which it is difficult to assess the true resolution and error distribution. For this reason, we employ a revised 3D bending algorithm (Moser et al., 1992) and show that it can be used efficiently for a non-linear inversion in a stepwise scheme. Initial paths are determined from graph theory in order to avoid local minima in bending. The importance of 3D ray tracing in inversion studies and the limitations of the standard 1D approach are demonstrated through synthetic examples. The speed of the ray tracing and the simple scaling scheme allow for an implementation in large-scale tomographic problems
A dense wide-angle data set is used to test a two-step procedure for the separate inversion of first...
this paper is as follows. In section 2 we survey the mathematical models used in tomography. In sect...
We have developed a first-arrival traveltime inversion scheme that jointly solves for seismic veloci...
The use of 1D or pseudo- 3D ray tracing techniques in linearized tomographic problems leads to solut...
The original publication can be found at www.springerlink.com Copyright © 2005 Birkhauser Verlag, Ba...
International audienceWe present a new method of traveltime tomography. In this method, the travelti...
Fermat's principle shows that a definite convex set of feasible slowness models -- depending on...
Inversion of head wave arrival times for three-dimensional (3D) planar structure is formulated as a ...
The determination of a correct subsurface velocity model is of strategic importance for seismic imag...
Tiré à part de: Revue du CETHEDEC. Ondes et signal. - 1983, 76. Bulletin de liaison des Laboratoires...
International audienceClassical algorithms used for travel time tomography are not necessarily well-...
Traditional straight ray- and curved ray-based tomography algorithms need to perform ray tracing to ...
Abstract-In this paper, linearized tomography and the Herglotz-Wiechert inverse formulation are comp...
Seismic tomography is a well-established approach to invert smooth macro-velocity models from kinema...
The definitive version is available at www.blackwell-synergy.comWe have developed two, new non-linea...
A dense wide-angle data set is used to test a two-step procedure for the separate inversion of first...
this paper is as follows. In section 2 we survey the mathematical models used in tomography. In sect...
We have developed a first-arrival traveltime inversion scheme that jointly solves for seismic veloci...
The use of 1D or pseudo- 3D ray tracing techniques in linearized tomographic problems leads to solut...
The original publication can be found at www.springerlink.com Copyright © 2005 Birkhauser Verlag, Ba...
International audienceWe present a new method of traveltime tomography. In this method, the travelti...
Fermat's principle shows that a definite convex set of feasible slowness models -- depending on...
Inversion of head wave arrival times for three-dimensional (3D) planar structure is formulated as a ...
The determination of a correct subsurface velocity model is of strategic importance for seismic imag...
Tiré à part de: Revue du CETHEDEC. Ondes et signal. - 1983, 76. Bulletin de liaison des Laboratoires...
International audienceClassical algorithms used for travel time tomography are not necessarily well-...
Traditional straight ray- and curved ray-based tomography algorithms need to perform ray tracing to ...
Abstract-In this paper, linearized tomography and the Herglotz-Wiechert inverse formulation are comp...
Seismic tomography is a well-established approach to invert smooth macro-velocity models from kinema...
The definitive version is available at www.blackwell-synergy.comWe have developed two, new non-linea...
A dense wide-angle data set is used to test a two-step procedure for the separate inversion of first...
this paper is as follows. In section 2 we survey the mathematical models used in tomography. In sect...
We have developed a first-arrival traveltime inversion scheme that jointly solves for seismic veloci...