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dc.contributor.authorSpychala, Yvonne T.
dc.contributor.authorRamaaker, Thymen A. B.
dc.contributor.authorEggenhuisen, Joris T.
dc.contributor.authorGrundvåg, Sten-Andreas
dc.contributor.authorPohl, Florian
dc.contributor.authorWróblewska, Sara
dc.date.accessioned2022-01-04T09:50:23Z
dc.date.available2022-01-04T09:50:23Z
dc.date.issued2021-09-09
dc.description.abstractThe grain-size distribution of sediment particles is an important aspect of the architecture of submarine fans and lobes. It governs depositional sand quality and reflects distribution of particulate organic carbon and pollutants. Documenting the grain-size distribution of these deep-marine sedimentary bodies can also offer us an insight into the flows that deposited them. Submarine lobes are commonly assumed to linearly fine from an apex, meaning there should be a proportional relationship between grain size and distance from the lobe apex. However, not much detailed quantitative work has been done to test this hypothesis. Exposure of a 5 km long dip-section of basin-floor lobes in Clinoform 12, Battfjellet Formation, Spitsbergen, enable the study of basinward grain-size evolution in lobe deposits. Furthermore, the dataset allows testing if there are any documentable grain-size differences between lobe sub-environments. For this purpose, the palaeogeography of Clinoform 12 was reconstructed and the youngest lobe, which was exposed in all collected logs, chosen to be evaluated for its grain-size trends. Photographed thin sections of 66 rock samples were analysed to obtain quantitative grain-size distributions. The results show that fining of lobe deposits occurs predominantly in the most proximal and most distal parts of the lobe, while the intermediate lobe, which is dominated by lobe off-axis deposits, is characterised by a relatively consistent grain-size range. Lobe subenvironments show statistically distinct grain-size distributions from lobe axis to lobe fringe. An explanation for these trends is the interplay of capacity and competence-driven deposition with the grain-size stratification of the flows. The outcomes of this study help to better understand the proximal to distal evolution of turbidity currents and their depositional patterns. They also provide important insights in reservoir potential of basin-floor fans at lobe scaleen_US
dc.identifier.citationSpychala, Ramaaker, Eggenhuisen, Grundvåg S.-A., Pohl, Wróblewska. Proximal to distal grain-size distribution of basin-floor lobes: A study from the Battfjellet Formation, Central Tertiary Basin, Svalbard. The Depositional Record. 2021:1-21en_US
dc.identifier.cristinIDFRIDAID 1944296
dc.identifier.doi10.1002/dep2.167
dc.identifier.issn2055-4877
dc.identifier.urihttps://hdl.handle.net/10037/23591
dc.language.isoengen_US
dc.publisherWileyen_US
dc.relation.journalThe Depositional Record
dc.relation.projectIDNorges forskningsråd: 228107en_US
dc.relation.projectIDinfo:eu-repo/grantAgreement/RCN/PETROSENTR/228107/Norway/Research Centre for Arctic Petroleum Exploration/ARCEx/en_US
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2021 The Author(s)en_US
dc.subjectVDP::Mathematics and natural science: 400::Geosciences: 450en_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Geofag: 450en_US
dc.titleProximal to distal grain-size distribution of basin-floor lobes: A study from the Battfjellet Formation, Central Tertiary Basin, Svalbarden_US
dc.type.versionpublishedVersionen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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