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dc.contributor.authorGambino, Salvatore
dc.contributor.authorBarreca, Giovanni
dc.contributor.authorGross, Felix
dc.contributor.authorMonaco, Carmelo
dc.contributor.authorGutscher, Marc-André
dc.contributor.authorAlsop, G. Ian
dc.date.accessioned2023-02-01T00:13:08Z
dc.date.available2023-02-01T00:13:08Z
dc.date.issued2022-02-01
dc.identifier202606541
dc.identifier720d701d-3584-4743-9698-e3c8ab957938
dc.identifier000710120800001
dc.identifier85117622666
dc.identifier.citationGambino , S , Barreca , G , Gross , F , Monaco , C , Gutscher , M-A & Alsop , G I 2022 , ' Assessing the rate of crustal extension by 2D sequential restoration analysis : A case study from the active portion of the Malta Escarpment ' , Basin Research , vol. 34 , no. 1 , pp. 321-341 . https://doi.org/10.1111/bre.12621en
dc.identifier.issn0950-091X
dc.identifier.otherRIS: urn:0334E9D8FC274356A234F80DDFC7C9FB
dc.identifier.otherSCOPUS: 85117622666
dc.identifier.urihttp://aura-test.abdn.ac.uk/handle/2164/19420
dc.descriptionACKNOWLEDGEMENTS The bathymetric data were extracted from Gutscher et al. (2017) and from EMODnet open dataset (http://www.emodnet-bathymetry.eu/). Digital topographic data are from the Japan Aerospace Exploration Agency (https://www.eorc.jaxa.jp). The authors also acknowledge the use of MOVE Software Suite granted by Petroleum Experts Limited (www.petex.com). This work is part of the S. Gambino's Ph.D. research project at the University of Catania. Bernard Mercier de Lepinay (GeoAzur, Université de Nice/CNRS), is also acknowledged for the CIRCEE-HR seismic data processing. Funding information: This work benefits from the finding from the University of Catania in the framework of the project “Multidisciplinary analysis of the deformation around active tectonic structures” (responsible G. Barreca) and partly from the MUSE 4D project - Overtime tectonic, dynamic and rheologic control on destructive multiple seismic events -Special Italian Faults & Earthquakes: from real 4D cases to models in the frame of PRIN 2017en
dc.format.extent21
dc.format.extent3216878
dc.language.isoeng
dc.relation.ispartofBasin Researchen
dc.subjectdeformation rateen
dc.subjectMalta Escarpmenten
dc.subjectseismic profileen
dc.subjectsequential restorationen
dc.subjectQE Geologyen
dc.subjectSupplementary Informationen
dc.subject.lccQEen
dc.titleAssessing the rate of crustal extension by 2D sequential restoration analysis : A case study from the active portion of the Malta Escarpmenten
dc.typeJournal articleen
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.description.statusPeer revieweden
dc.identifier.doihttps://doi.org/10.1111/bre.12621
dc.date.embargoedUntil2022-10-23
dc.identifier.vol34en
dc.identifier.iss1en


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