Computer Science – Sound
Scientist
Computer Science
Sound
Scientist
The Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, 10110 Burnet Rd., Bldg. 196, Austin, TX 78758, USA
R2200
Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, TX, USA for Geophysics, Jackson School of Geosciences, The University of Texas at Austin, Austin, TX, USA
Institute for Geophysics, John A. and Catherine G. Jackson School of Geosciences, 4412 Spicewood Springs Road, Bldg. 600, Austin, TX 78759, USA Univ., Austin
John A. and Katherine G. Jackson, School of Geosciences, University of Texas at Austin, Austin, Texas, USA
Institute for Geophysics, Jackson School of Geosciences, The university of Texas at Austin, TX, USA Institute for Geophysics, John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, 10100 Burnet Road, R2200 Austin, TX 78758, USA for Geophysics, University of Texas at Austin, Austin, Texas, USA
The Institute for Geophysics, John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, R2200 Austin, TX 78758, USA
Institution for Geophysics, University of Texas at Austin, Austin 78758, USA
Institute for Geophysics, Jackson School of Geosciences, 4412 Spicewood Springs Road, Austin, TX 78759, USA Institute for Computational Engineering and Sciences, The University of Texas at Austin, 1 University Station C0200 Austin, TX 78712, USA ; The Institute for Geophysics, John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, 10100 Burnet Road, R2200 Austin, TX 78758, USA
Institute for Geophysics, The University of Texas at Austin, Austin, TX 78759-8500 USA
2-D migration velocity estimation using a genetic algorithm
A hybrid scheme for seismic modelling based on Galerkin method
A new MCMC algorithm for seismic waveform inversion and corresponding uncertainty analysis
A possible mechanism for the spatial distribution of seismicity in northern Gulf of Mexico
A reflectivity method for laterally varying media: homogeneous layers with curved interfaces
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