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Distinguishing tectonically-and gravity-driven synsedimentary deformation structures along the Apulian platform margin (Gargano Promontory, southern Italy)

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dc.contributor.authorKorneva, Irina
dc.contributor.authorTondi, Emanuele
dc.contributor.authorJablonska, Danica
dc.contributor.authorDi Celma, Claudio
dc.contributor.authorAlsop, Ian
dc.contributor.authorAgosta, Fabrizio
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.contributor.institutionUniversity of Aberdeen.Centre for Energy Transitionen
dc.date.accessioned2017-05-01T23:01:57Z
dc.date.available2017-05-01T23:01:57Z
dc.date.embargoedUntil2017-05-01
dc.date.issued2016-05
dc.descriptionAcknowledgements This work has been supported by Reservoir Characterisation Project (www.rechproject.com) and FAR Project 2014 "Characterisation and modelling of natural reservoirs of geofluids in fractured carbonate rocks", funded by the University of Camerino, coordinator Emanuele Tondi.en
dc.description.statusPeer revieweden
dc.format.extent13
dc.format.extent21185330
dc.identifier62106055
dc.identifier17c9c62a-373c-46a1-adc0-90489d5a92ac
dc.identifier84961644315
dc.identifier.citationKorneva, I, Tondi, E, Jablonska, D, Di Celma, C, Alsop, I & Agosta, F 2016, 'Distinguishing tectonically-and gravity-driven synsedimentary deformation structures along the Apulian platform margin (Gargano Promontory, southern Italy)', Marine and Petroleum Geology, vol. 73, pp. 479-491. https://doi.org/10.1016/j.marpetgeo.2015.12.009en
dc.identifier.doi10.1016/j.marpetgeo.2015.12.009
dc.identifier.issn0264-8172
dc.identifier.otherORCID: /0000-0003-4479-372X/work/161797412
dc.identifier.urihttp://hdl.handle.net/2164/8583
dc.identifier.vol73en
dc.language.isoeng
dc.relation.ispartofMarine and Petroleum Geologyen
dc.subjectApulian platformen
dc.subjectMaiolica formationen
dc.subjectsynsedimentary faultsen
dc.subjectslumpsen
dc.subjectmass-transport depositsen
dc.subjectQE Geologyen
dc.subject.lccQEen
dc.titleDistinguishing tectonically-and gravity-driven synsedimentary deformation structures along the Apulian platform margin (Gargano Promontory, southern Italy)en
dc.typeJournal articleen

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