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- W1993001572 abstract "An oceanic crustal model has been produced for the Nazca plate south of the Nazca Ridge prior to subduction into the Peru-Chile Trench at 18°S latitude. Consistent delays of thePn arrivals and a discontinuity in the tau-p curve indicate a low-velocity zone at the base of the crust. Observed upper mantle velocities are low; however, the mantle velocity increases with depth, at least to 20 km, to a value of 8.5 km/s. A possible petrological cause for the low-velocity zone is partially serpentinized peridotite; however, no clear refracted shear waves were observed to constrain this interpretation." @default.
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- W1993001572 date "1977-11-01" @default.
- W1993001572 modified "2023-09-27" @default.
- W1993001572 title "The structure of the oceanic crust off southern Peru determined from an ocean bottom seismometer" @default.
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- W1993001572 doi "https://doi.org/10.1016/0012-821x(77)90142-x" @default.
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