Normal thickness of the upper mantle transition zone in NE Brazil does not favour mantle plumes as origin for intraplate Cenozoic volcanism
about
Spatial and temporal uplift history of South America from calibrated drainage analysisRayleigh-Wave, Group-Velocity Tomography of the Borborema Province, NE Brazil, from Ambient Seismic NoiseCrustal structure of the eastern Borborema Province, NE Brazil, from the joint inversion of receiver functions and surface wave dispersion: Implications for plateau uplift
P2860
Normal thickness of the upper mantle transition zone in NE Brazil does not favour mantle plumes as origin for intraplate Cenozoic volcanism
description
article
@en
im September 2014 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована у вересні 2014
@uk
name
Normal thickness of the upper ...... intraplate Cenozoic volcanism
@en
Normal thickness of the upper ...... intraplate Cenozoic volcanism
@nl
type
label
Normal thickness of the upper ...... intraplate Cenozoic volcanism
@en
Normal thickness of the upper ...... intraplate Cenozoic volcanism
@nl
prefLabel
Normal thickness of the upper ...... intraplate Cenozoic volcanism
@en
Normal thickness of the upper ...... intraplate Cenozoic volcanism
@nl
P2860
P356
P1476
Normal thickness of the upper ...... intraplate Cenozoic volcanism
@en
P2093
A. G. Pinheiro
P2860
P304
P356
10.1093/GJI/GGU281
P50
P577
2014-09-10T00:00:00Z