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dc.contributor.authorSammarco, Carmelo
dc.contributor.authorCornwell, David G.
dc.contributor.authorRawlinson, Nicholas
dc.date.accessioned2018-09-18T23:06:56Z
dc.date.available2018-09-18T23:06:56Z
dc.date.issued2017-11-28
dc.identifier.citationSammarco , C , Cornwell , D G & Rawlinson , N 2017 , ' Ambient noise tomography reveals basalt and sub-basalt velocity structure beneath the Faroe Islands, North Atlantic ' Tectonophysics , vol. 721 , pp. 1-11 . DOI: 10.1016/j.tecto.2017.09.012en
dc.identifier.issn0040-1951
dc.identifier.otherPURE: 108692527
dc.identifier.otherPURE UUID: 9da9edea-1b1a-45fc-88e8-7f57437cd612
dc.identifier.otherScopus: 85034020833
dc.identifier.urihttp://hdl.handle.net/2164/11120
dc.descriptionThe Faroe Islands Passive Seismological Experiment (FIPSE) was funded by Sindri (contract C46-52-01) and formed a collaborative project between Dr. David Cornwell, Prof. Richard England (University of Leicester) and Prof. Graham Stuart (University of Leeds). Seismological equipment was loaned from the NERC geophysical equipment facility (GEF, loan 918), with field assistance from David Hawthorn and data processing assistance from Victoria Lane (SEIS-UK). We acknowledge the help, advice and support of Jarðfeingi, especially Thomas Varming, Uni Petersen, Bartal Højgaard, Romica Øster and Heri Ziska. Rannvá M. Arge and Magni Jøkladal are thanked for their assistance with fieldwork. Research undertaken in this article was supported by the Carnegie Trust for the Universities of Scotland, via a Collaborative Research Grant. Rosie Fletcher is thanked for her comments, which greatly improved the text.en
dc.format.extent11en
dc.language.isoeng
dc.relation.ispartofTectonophysicsen
dc.rights© 2017. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/en
dc.subjectSeismic tomographyen
dc.subjectAmbient seismic noiseen
dc.subjectNorth Atlanticen
dc.subjectCrustal structureen
dc.subjectQE Geologyen
dc.subject.lccQEen
dc.titleAmbient noise tomography reveals basalt and sub-basalt velocity structure beneath the Faroe Islands, North Atlanticen
dc.typeJournal articleen
dc.contributor.institutionUniversity of Aberdeen, Geology & Petroleum Geologyen
dc.contributor.institutionUniversity of Aberdeen, Energyen
dc.contributor.institutionUniversity of Aberdeen, Aberdeen Institute of Energyen
dc.description.statusPeer revieweden
dc.description.versionPostprinten
dc.identifier.doihttps://doi.org/10.1016/j.tecto.2017.09.012
dc.date.embargoedUntil19-09-20


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