Open AccessSeismic evidence for a sharp lithospheric base persisting to the lowermost mantle beneath the Caribbean
Author(s) -
Kito Tadashi,
Thomas Christine,
Rietbrock Andreas,
Garnero Edward J.,
Nippress Stuart E. J.,
Heath Andy E.
Publication year - 2008
Publication title -
geophysical journal international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0956-540X
DOI - 10.1111/j.1365-246x.2008.03880.x
Subject(s) - geology , mantle (geology) , core–mantle boundary , seismology , lithosphere , geophysics , crust , subduction , mantle convection , transition zone , discontinuity (linguistics) , seismogram , tectonics , mathematical analysis , mathematics
SUMMARY Broad‐band data from South American earthquakes recorded by Californian seismic networks are analysed using a newly developed seismic wave migration method—the slowness backazimuth weighted migration (SBWM). Using the SBWM, out‐of‐plane seismic P ‐wave reflections have been observed. The reflection locations extend throughout the Earth's lower mantle, down to the core–mantle boundary (CMB) and coincide with the edges of tomographically mapped high seismic velocities. Modelling using synthetic seismograms suggests that a narrow (10–15 km) low‐ or high‐velocity lamella with about 2 per cent velocity contrast can reproduce the observed reflected waveforms, but other explanations may exist. Considering the reflection locations and synthetic modelling, the observed out‐of‐plane energy is well explained by underside reflections off a sharp reflector at the base of the subducted lithosphere. We also detect weaker reflections corresponding to the tomographically mapped top of the slab, which may arise from the boundary between the Nazca plate and the overlying former basaltic oceanic crust. The joint interpretation of the waveform modelling and geodynamic considerations indicate mass flux of the former oceanic lithosphere and basaltic crust across the 660 km discontinuity, linking processes and structure at the top and bottom of the Earth's mantle, supporting the idea of whole mantle convection.