High Temperature in the Upper Mantle Beneath Cape Verde as a Possible Cause for the Oceanic Lithosphere Rejuvenation Inferred from Rayleigh-Wave Phase-Velocity Measurements.

AuthID
 P-013-BD0
9
Author(s)
Carvalho, J
·
Bonadio, R
·
Lebedev, S
·
Custódio, S
·
Mata, J
·
Meier, T
·
Celli, N
Tipo de Documento
Unpublished
Year published
2020
Publicado
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