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F. Mancilla, E. Del Pezzo, D. Stich, J. Morales, J. Ibañez and F. Bianco QP and QS in the upper mantle beneath the Iberian peninsula from recordings of the very deep Granada earthquake of April 11, 2010 Geophysical Research Letters 39

Article first published online: 2 MAY 2012 | DOI: 10.1029/2012GL050947

Key Points

  • A rare, very deep earthquakes probes the upper-mantle beneath Iberia
  • Upper mantle attenuation is high between 0.25 Hz and 8 Hz
  • Scattering is the dominant mechanism, indicating strong heterogeneity

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