Hybrid approach for seismic travel time tomography is proposed in the case of elliptical anisotropic media. A sequential scheme is presented that combines Simulating Annealing with Linearized Least Squares inversion: at first, Simulated Annealing is implemented to obtain a velocity model that can be used as initial guess for successive Linearized Least Square inversion; in the meantime Linear Traveltime Interpolation is diffusely used to trace raypaths and calculate traveltimes. The procedure was tested both for a synthetic model and a field study. Since the field study come from a previous study, uniquely solved by Linearized Least Squares inversion without suggestions for initial guess of the velocity model, we were interested in evaluati...
Copyright © 2008 Society of ExplorationGeophysicists. All rights reserved. Crosshole seismic tomogra...
International audienceWe present a new method of traveltime tomography. In this method, the travelti...
In the medium composed of parallel sedimentary layers, model of elliptic anisotropy is often better ...
Hybrid approach for seismic travel time tomography is proposed in the case of elliptical anisotropic...
The definitive version is available at www.blackwell-synergy.comWe have developed two, new non-linea...
Seismic wave speed and anisotropy provide essential constraints on the Earth’s internal velocity st...
A seismic traveltime inversion method is proposed for building smooth velocity models using travelti...
We present a new 2-D traveltime tomography method for the inversion of densely sampled seismic strea...
We present a hybrid method to produce a velocity model of the Earth’s crust using evolutionary and s...
This study is concerned with the computation of seismic first-arrival traveltimes in anisotropic med...
A velocity model is described in which we assume that velocity increases linearly with depth and var...
Wavefield travel time tomography is used for a variety of purposes in acoustics, geophysics and non-...
A back projection method of reconstruction is adapted to invert seismic travel time data for velocit...
The measured traveltimes of specular reflection events are inverted to obtain a low spatial frequenc...
In this paper, we propose a wave-equation-based travel-time seismic tomography method with a detaile...
Copyright © 2008 Society of ExplorationGeophysicists. All rights reserved. Crosshole seismic tomogra...
International audienceWe present a new method of traveltime tomography. In this method, the travelti...
In the medium composed of parallel sedimentary layers, model of elliptic anisotropy is often better ...
Hybrid approach for seismic travel time tomography is proposed in the case of elliptical anisotropic...
The definitive version is available at www.blackwell-synergy.comWe have developed two, new non-linea...
Seismic wave speed and anisotropy provide essential constraints on the Earth’s internal velocity st...
A seismic traveltime inversion method is proposed for building smooth velocity models using travelti...
We present a new 2-D traveltime tomography method for the inversion of densely sampled seismic strea...
We present a hybrid method to produce a velocity model of the Earth’s crust using evolutionary and s...
This study is concerned with the computation of seismic first-arrival traveltimes in anisotropic med...
A velocity model is described in which we assume that velocity increases linearly with depth and var...
Wavefield travel time tomography is used for a variety of purposes in acoustics, geophysics and non-...
A back projection method of reconstruction is adapted to invert seismic travel time data for velocit...
The measured traveltimes of specular reflection events are inverted to obtain a low spatial frequenc...
In this paper, we propose a wave-equation-based travel-time seismic tomography method with a detaile...
Copyright © 2008 Society of ExplorationGeophysicists. All rights reserved. Crosshole seismic tomogra...
International audienceWe present a new method of traveltime tomography. In this method, the travelti...
In the medium composed of parallel sedimentary layers, model of elliptic anisotropy is often better ...