Shear velocity structure of the crust and upper mantle of Madagascar derived from surface wave tomography

Autor: G. I. Aleqabi, Patrick J. Shore, Gérard Rambolamanana, Michael E. Wysession, Douglas A. Wiens, Tsiriandrimanana Rakotondraibe, Andrew A. Nyblade, E. J. Rindraharisaona, M. J. Pratt, Guilhem Barruol, Fenitra Andriampenomanana, Robert D. Tucker
Přispěvatelé: Washington University in Saint Louis (WUSTL), Department of Geosciences, Pennsylvania State University (Penn State), Penn State System-Penn State System, Institut et Observatoire de Géophysique et Astronomie d'Antananarivo, Madagascar (IOGA), University of Maryland [College Park], University of Maryland System, Institut de Physique du Globe de Paris (IPGP), Centre National de la Recherche Scientifique (CNRS)-Université de La Réunion (UR)-Université Paris Diderot - Paris 7 (UPD7)-IPG PARIS-Institut national des sciences de l'Univers (INSU - CNRS), Laboratoire GéoSciences Réunion (LGSR), Université de La Réunion (UR)-Institut de Physique du Globe de Paris, GeoForschungsZentrum - Helmholtz-Zentrum Potsdam (GFZ), MACOMO project was provided by NSF award EAR-0838426DFG (Deutsche Forschungsgemeinschaft) grant SI1538/2-1, ANR-11-BS56-0013,RHUM-RUM,Imagerie mantellique du point chaud de La Réunion(2011), Washington University in St Louis
Rok vydání: 2017
Předmět:
Zdroj: Earth and Planetary Science Letters
Earth and Planetary Science Letters, Elsevier, 2017, 458, pp.405-417. ⟨10.1016/j.epsl.2016.10.041⟩
Earth And Planetary Science Letters (0012-821X) (Elsevier), 2017-01, Vol. 458, P. 405-417
ISSN: 0012-821X
DOI: 10.1016/j.epsl.2016.10.041
Popis: International audience; The crust and upper mantle of the Madagascar continental fragment remained largely unexplored until a series of recent broadband seismic experiments. An island-wide deployment of broadband seismic instruments has allowed the first study of phase velocity variations, derived from surface waves, across the entire island. Late Cenozoic alkaline intraplate volcanism has occurred in three separate regions of Madagascar (north, central and southwest), with the north and central volcanism active until
Databáze: OpenAIRE