Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/16885
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dc.contributor.authorChávez, R. E.cat
dc.contributor.authorFlores-Márquez, E. L.cat
dc.contributor.authorSuriñach Cornet, Emmacat
dc.contributor.authorGalindo Zaldívar, Jesúscat
dc.contributor.authorRodríguez Fernández, Josécat
dc.contributor.authorMaldonado, Andréscat
dc.date.accessioned2011-03-08T09:35:08Z-
dc.date.available2011-03-08T09:35:08Z-
dc.date.issued2007-
dc.identifier.issn1695-6133-
dc.identifier.urihttp://hdl.handle.net/2445/16885-
dc.description.abstractThe Powell Basin is a small oceanic basin located at the NE end of the Antarctic Peninsula developed during the Early Miocene and mostly surrounded by the continental crusts of the South Orkney Microcontinent, South Scotia Ridge and Antarctic Peninsula margins. Gravity data from the SCAN 97 cruise obtained with the R/V Hespérides and data from the Global Gravity Grid and Sea Floor Topography (GGSFT) database (Sandwell and Smith, 1997) are used to determine the 3D geometry of the crustal-mantle interface (CMI) by numerical inversion methods. Water layer contribution and sedimentary effects were eliminated from the Free Air anomaly to obtain the total anomaly. Sedimentary effects were obtained from the analysis of existing and new SCAN 97 multichannel seismic profiles (MCS). The regional anomaly was obtained after spectral and filtering processes. The smooth 3D geometry of the crustal mantle interface obtained after inversion of the regional anomaly shows an increase in the thickness of the crust towards the continental margins and a NW-SE oriented axis of symmetry coinciding with the position of an older oceanic spreading axis. This interface shows a moderate uplift towards the western part and depicts two main uplifts to the northern and eastern sectors.eng
dc.format.extent13 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoengeng
dc.publisherUniversitat de Barcelona (UB). Institut de Ciències de la Terra Jaume Almera (ICTJA). Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDEA). Universitat Autonònoma de Barcelona (UAB). Consejo Superior de Investigaciones Científicas (CSIC)cat
dc.relation.isformatofReproducció del document publicat a http://www.geologica-acta.com/pdf/vol0504a06.pdfcat
dc.relation.ispartofGeologica Acta, 2007, vol. 5, núm. 4, p. 323-335-
dc.rightscc by-sa (c) Chávez et al., 2007-
dc.rights.urihttp://creativecommons.org/licenses/by-sa/3.0/es/*
dc.subject.classificationAntàrtidacat
dc.subject.classificationGeologia submarinacat
dc.subject.otherSubmarine geologyeng
dc.subject.otherAntarcticaeng
dc.titleCombined use of the GGSFT data base and on Board Marine Collected Data to Model the Moho Beneath the Powell Basin, Antarcticaeng
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.identifier.idgrec549783-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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