dc.date.accessioned | 2020-05-24T17:59:31Z | |
dc.date.available | 2020-05-24T17:59:31Z | |
dc.date.created | 2020-01-16T14:14:07Z | |
dc.date.issued | 2019 | |
dc.identifier.citation | Faleide, Thea Sveva Midtkandal, Ivar Planke, Sverre Corseri, Romain Faleide, Jan Inge Serck, Christopher Sæbø Nystuen, Johan Petter . Characterisation and development of Early Cretaceous shelf platform deposition and faulting in the Hoop area, southwestern Barents Sea—constrained by high-resolution seismic data. Norwegian Journal of Geology. 2019, 99(3), 1-20 | |
dc.identifier.uri | http://hdl.handle.net/10852/76190 | |
dc.description.abstract | Regional Early Cretaceous uplift of the northern Barents Sea associated with the High Arctic Large Igneous Province (HALIP) caused the development of the fluvial to open-marine depositional system, terminating in the southwestern Barents Sea. This study has established a new temporal and spatial evolution of the Lower Cretaceous deposits in the Hoop area, in particular the location and age of the intrashelf platform lobe front and subsequent block-faulting. A composite high-resolution 3D and 2.5D P-Cable and conventional 3D seismic dataset image the strata and cross-cutting faults in the Hoop area. The P-Cable data typically have a resolution of 3–7 m in the shallow subsurface, up to four times better than the conventional seismic data, contributing to a new and better mapping hence understanding of the Lower Cretaceous strata and faults. Seismic horizon and facies mapping reveal large-scale clinoforms, with present-day heights of 150–200 m and dips of 0.65–1.13°. The highresolution data furthermore display complex stratigraphic and structural features, such as small-scale clinoforms and numerous faults. The shelf platform succession is block-faulted, and the main Early Cretaceous fault activity thus postdates the arrival of the delta and platform sediments from the northwest. Detailed seismo-stratigraphic ties to the 7324/2–1 (Apollo) and 7325/1–1 (Atlantis) wells, and ties to the adjacent Fingerdjupet Subbasin, document a Barremian age for the shelf platform deposits and an Aptian?–early Albian age for the main faulting event. The faulting was likely initiated in the Aptian, but a hiatus or condensed section above the Barremian strata makes it difficult to constrain the onset of deformation in the Hoop area. | |
dc.language | EN | |
dc.rights | Attribution 4.0 International | |
dc.rights.uri | https://creativecommons.org/licenses/by/4.0/ | |
dc.title | Characterisation and development of Early Cretaceous shelf platform deposition and faulting in the Hoop area, southwestern Barents Sea—constrained by high-resolution seismic data | |
dc.type | Journal article | |
dc.creator.author | Faleide, Thea Sveva | |
dc.creator.author | Midtkandal, Ivar | |
dc.creator.author | Planke, Sverre | |
dc.creator.author | Corseri, Romain | |
dc.creator.author | Faleide, Jan Inge | |
dc.creator.author | Serck, Christopher Sæbø | |
dc.creator.author | Nystuen, Johan Petter | |
cristin.unitcode | 185,15,22,50 | |
cristin.unitname | Seksjon for geologi og geofysikk | |
cristin.ispublished | true | |
cristin.fulltext | original | |
cristin.qualitycode | 1 | |
dc.identifier.cristin | 1774956 | |
dc.identifier.bibliographiccitation | info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Norwegian Journal of Geology&rft.volume=99&rft.spage=1&rft.date=2019 | |
dc.identifier.jtitle | Norwegian Journal of Geology | |
dc.identifier.volume | 99 | |
dc.identifier.issue | 3 | |
dc.identifier.startpage | 1 | |
dc.identifier.endpage | 20 | |
dc.identifier.doi | https://doi.org/10.17850/njg99-3-7 | |
dc.identifier.urn | URN:NBN:no-79304 | |
dc.type.document | Tidsskriftartikkel | |
dc.type.peerreviewed | Peer reviewed | |
dc.source.issn | 2387-5844 | |
dc.identifier.fulltext | Fulltext https://www.duo.uio.no/bitstream/handle/10852/76190/1/NJG_Vol99_Nr3_Faleide_etal.pdf | |
dc.type.version | PublishedVersion | |
dc.relation.project | NFR/223272 | |