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FROM TRAVELTIME TO COMPOSITION: A NEW INVERSION ALGORITH FOR SEIMIC AND GRAVITY DATA

Ivan Virshylo

First published: 2014-06-20https://doi.org/10.5593/sgem2014/b11/s5.060View metrics

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Title
FROM TRAVELTIME TO COMPOSITION: A NEW INVERSION ALGORITH FOR SEIMIC AND GRAVITY DATA
Authors
Ivan Virshylo
Proceedings
14th International Multidisciplinary Scientific GeoConference SGEM 2014, Science and Technologies in Geology, Exploration and Mining, Vol. 14, Book 1, Volume 1
Publisher
Stef92 Technology
Year
2014
Pages
Not available yet
ISSN
1314-2704
ISBN
Not available yet
Language
en
Publication type
Conference Paper
Proceedings volume
14th International Multidisciplinary Scientific GeoConference SGEM 2014, Science and Technologies in Geology, Exploration and Mining, Vol. 14, Book 1, Volume 1 · Issue Book 1, Volume 1
References9
  1. Woodward M.J. et al., A decade of tomography, Geophysics, USA, Vol. 73, issue 5, pp VE5–VE11, 2008

  2. Moser T.J., Shortest path calculations of seismic rays, Geophysics, USA, Vol. 56, issue 1, pp 59-67, 1991

  3. Lo T. and Inderwiesen P.L., Fundamentals of Seismic Tomography, Society of Exploration Geophysicists, USA, 187 p., 1994

  4. Chapman B., Jost G. and van der Pas R. Using OpenMP: portable shared memory parallel programming, USA, 353 p., 2008;

  5. Farber R. CUDA application design and development, USA, 315 p, 2011;

  6. Sanders J. and Kandrot E. CUDA by example: an introduction to general-purpose GPU programming, USA, 290 p, 2011;

  7. ] Lines L.R., Schultz A.K. and Treitel S. Cooperative inversion of geophysical data, Geophysics, Vol. 53, issue 1, pp 8-20, 1988

  8. Prodaivoda, G. T., Khoroshun, L. P., Nazarenko, L. V., & Vyzhva, S. A. (2000). Mathematical modeling of the azimuthal anisotropy in thermoelasic properties of the oceanic upper mantle. IzvestiyaPhysics of the Solid Earth, 36(5), 394–405 (in Russian).

  9. Stixrude, L., & Lithgow-Bertelloni, C. (2005). Thermodynamics of mantle minerals - I. Physical properties. Geophysical Journal International, 162(2), 610–632.

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