Normal thickness of the upper mantle transition zone in NE Brazil does not favour mantle plumes as origin for intraplate Cenozoic volcanism

We have investigated variations in transition zone thickness under the Borborema Province of NE Brazil by migrating and stacking teleseismic P-wave receiver functions at 32 seismic stations in the region. The Borborema Province represents the western portion of a larger Neoproterozoic mobile belt th...

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Veröffentlicht in:	Geophysical journal international 2014-11, Vol.199 (2), p.996-1005
Hauptverfasser:	Pinheiro, A. G., Julià, J.
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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