1887

Abstract

Summary

Over the last decade the acoustic 3-D full-waveform inversion technique has become almost a common tool for imaging geologically complex structures in marine, as well as in land settings. However, it has been speculated that excluding the elastic effect from the waveform modeling in some cases could have a big impact and potentially result in an erroneous image of the subsurface. To examine the contribution of the elastic effect, we conduct acoustic and elastic 3-D FWI on the 3-D seismic data, collected at the East Pacific Rise (EPR) 9°50’N, deep-water environment (minimum depth ~2500 m) with high compression velocity contrast at the seafloor. We first establish a strategy for inversion within the EPR setting, which suggest simultaneous multi-parameter inversion for the frequencies <7 Hz. Comparison of the results shows that the total misfit for the elastic case is reduced for ~10% more when compared to the acoustic, suggesting that the elastic effect is not negligible. Furthermore, the images of the upper-crust obtained using the two approaches differ significantly, not only in velocity amplitude, but also structurally, leading to different implications for crustal accretion processes, with the elastic approach leading to geologically more plausible solution.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201800686
2018-06-11
2024-04-26
Loading full text...

Full text loading...

References

  1. Arnulf, A.F., A.J.Harding, S.C.Singh, G.M.Kent, and W.Crawford
    (2014), Nature of upper crust beneath the Lucky Strike volcano using elastic full waveform inversion of streamer data, Geophys. J. Int., 196, 1471–1491.
    [Google Scholar]
  2. Christeson, G.L., J.V.Morgan, and M.R.Warner
    (2012), Shallow oceanic crust: Full waveform tomographic images of the seismic layer 2A/2B boundary, J. Geophys. Res., 117, B05101.
    [Google Scholar]
  3. DetrickR.S., P.Buhl, E.Vera, J.Mutter, J.Orcutt, J.Madsen & T.Brocher
    (1987), Multi-channel seismic imaging of a crustal magma chamber along the East Pacific Rise, Nature326, 35–41.
    [Google Scholar]
  4. Marjanovic, M., Fuji, N., Singh, S.C., Belahi, T., & Escartín, J.
    (2017). Seismic signatures of hydrothermal pathways along the East Pacific Rise between 9° 16’ and 9°56’N. Journal Geophys. Res. Solid Earth, 122.
    [Google Scholar]
  5. MilcikP., Plessix, R.-E., Maison, K., Goh, V
    (2014) Low-frequency denoising and deghosting marine full-waveform inversion, 76th EAGE Conference and Exhibition.
    [Google Scholar]
  6. Mutter, J.C., Carbotte, S.M., Nedimović, M.R., Canales, J.P., and H.D., Carton
    (2009), Seismic imaging in three dimensions on the East Pacific Rise, Eos Trans. AGO, 90(42), 374–375.
    [Google Scholar]
  7. Morgan, J., M.Warner, G.Arnoux, E.Hooft, D.Toomey, B.VanderBeek and WWilcock
    (2016), Next generation seismic experiments — II: wide-angle, multi-azimuth, 3-D, full-waveform inversion of sparse field data, Geophys. J. Int.204, 1342–1363.
    [Google Scholar]
  8. Pérez SolanoC.A., A.Stopin, R.E.Plessix
    , (2013) Synthetic study of elastic effect on acoustic full waveform inversion, 75th EAGE Conference and Exhibition.
    [Google Scholar]
  9. Plessix, R.E. & C.Perkins
    (2010). Full waveform inversion of a deep water ocean bottom seismometer dataset, First Break, vol. 28, pp. 71–78.
    [Google Scholar]
  10. PlessixR.E., P.Milcik, H.Rynja, A.Stopin, K.Maison & S.Abri
    (2013), Multiparameter full-waveform inversion: Marine and land examples, The Leading Edge, pp. 1030–1038.
    [Google Scholar]
  11. Tarantola, A.
    (1987) Inverse Problem Theory.Elsevier, Amsterdam.
    [Google Scholar]
  12. Warner, M.R., Morgan, J.V., Umpleby, A., Štekl, I. & Guasch, L.
    , (2012). Which physics for full wavefield inversion?, in 74th EAGE Conference and Exhibition incorporating EUROPEC2012, EAGE, Extended Abstracts,pp. 2994–2998.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201800686
Loading
/content/papers/10.3997/2214-4609.201800686
Loading

Data & Media loading...

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error