Observation of near-podal P'P' precursors: Evidence for back scattering from the 150-220 km zone in the Earth's upper mantle

Physics

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Physical Properties Of Rocks: Wave Attenuation, Seismology: Body Waves, Seismology: Core (1212, 1213, 8124), Seismology: Mantle (1212, 1213, 8124), Tectonophysics: Earth'S Interior: Composition And State (1212, 7207, 7208, 8105)

Scientific paper

P'P' (PKPPKP) are P waves that travel from a hypocenter through the Earth's core, reflect from the free surface and travel back through the core to a recording station on the surface. Here we report the observations of hitherto unobserved near-podal P'P' waves (at epicentral distance <10°) and very prominent precursors preceding the main energy by as much as 60 s. We interpret these precursors as a back-scattered energy from horizontally connected small-scale heterogeneity in the upper mantle beneath the oceans in a zone between 150 and 220 km depth beneath the Earth's surface. From these observations, we identify a frequency dependence of attenuation quality factor Q in the lithosphere through forward modeling of the observed amplitude spectra of the main and back-scattered P'P' waves.

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