dc.contributor.author | Spychala, Yvonne T. | |
dc.contributor.author | Ramaaker, Thymen A. B. | |
dc.contributor.author | Eggenhuisen, Joris T. | |
dc.contributor.author | Grundvåg, Sten-Andreas | |
dc.contributor.author | Pohl, Florian | |
dc.contributor.author | Wróblewska, Sara | |
dc.date.accessioned | 2022-01-04T09:50:23Z | |
dc.date.available | 2022-01-04T09:50:23Z | |
dc.date.issued | 2021-09-09 | |
dc.description.abstract | The 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 scale | en_US |
dc.identifier.citation | Spychala, 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. 2021:1-21 | en_US |
dc.identifier.cristinID | FRIDAID 1944296 | |
dc.identifier.doi | 10.1002/dep2.167 | |
dc.identifier.issn | 2055-4877 | |
dc.identifier.uri | https://hdl.handle.net/10037/23591 | |
dc.language.iso | eng | en_US |
dc.publisher | Wiley | en_US |
dc.relation.journal | The Depositional Record | |
dc.relation.projectID | Norges forskningsråd: 228107 | en_US |
dc.relation.projectID | info:eu-repo/grantAgreement/RCN/PETROSENTR/228107/Norway/Research Centre for Arctic Petroleum Exploration/ARCEx/ | en_US |
dc.rights.accessRights | openAccess | en_US |
dc.rights.holder | Copyright 2021 The Author(s) | en_US |
dc.subject | VDP::Mathematics and natural science: 400::Geosciences: 450 | en_US |
dc.subject | VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 | en_US |
dc.title | Proximal to distal grain-size distribution of basin-floor lobes: A study from the Battfjellet Formation, Central Tertiary Basin, Svalbard | en_US |
dc.type.version | publishedVersion | en_US |
dc.type | Journal article | en_US |
dc.type | Tidsskriftartikkel | en_US |
dc.type | Peer reviewed | en_US |