dc.date.accessioned | 2022-03-03T16:28:37Z | |
dc.date.available | 2022-03-03T16:28:37Z | |
dc.date.created | 2022-01-26T12:17:53Z | |
dc.date.issued | 2021 | |
dc.identifier.citation | Tek, Daniel E. McArthur, Adam D. Poyatos More, Miquel Colombera, Luca Patacci, Marco Craven, Benjamin McCaffrey, William D. . Relating seafloor geomorphology to subsurface architecture: How mass-transport deposits and knickpoint-zones build the stratigraphy of the deep-water Hikurangi Channel. Sedimentology. 2021, 68(7), 3141-3190 | |
dc.identifier.uri | http://hdl.handle.net/10852/91758 | |
dc.description.abstract | Monitoring of modern deep-water channels has revealed how migrating channel-floor features generate and remove stratigraphy, improving understanding of how channel morphologies relate to their deposits. Here, seafloor and subsurface data are reconciled through an integrated study of high-resolution bathymetry and three-dimensional seismic data imaging a ca 150 km stretch of the trench-axial Hikurangi Channel, offshore New Zealand. On the seafloor, terraced channel-walls bound a flat, wide, channel-floor, ornamented with three scales of features that increase then decrease in longitudinal gradient downstream, and widen downstream: cyclic-steps, knickpoints and knickpoint-zones (in increasing size). Mass-transport deposits derived from channel-wall collapse, are bordered by wide and flat reaches of channel-floor upstream and by knickpoint-zones (reaches containing multiple knickpoints) downstream. In the subsurface, recognition of ten seismofacies and five types of surface enables identification of four depositional elements: channel-fill, sheet or terrace, levée, and mass-transport deposits. Integration of subsurface and seafloor interpretations reveals that knickpoint-zones initiate on the downstream margins of channel-damming mass-transport deposits; they migrate and incise through the mass-transport deposits and weakly-confined deposits formed upstream, as the channel tends towards equilibrium. Downstream of a knickpoint-zone, a flat channel-floor is bounded by newly-formed terraces. Knickpoints migrate by eroding upstream and depositing downstream, generating filled concave-up (cross-sectional) surfaces in their wake. Within knickpoint-zones, knickpoint-generated surfaces are re-incised by subsequently-passing knickpoints to produce a composite bounding surface; this surface does not delineate the morphology of any palaeo-conduit. The Hikurangi Channel’s subsurface architecture records the localized erosional response to mass-transport deposit emplacement via knickpoint-zone migration, showcasing how transient seafloor features can build channelized stratigraphy. This model provides an additional mechanism to conventional models of channel deposit formation through ‘cut-and-fill’ over long stretches of channel. These findings may aid subsurface interpretation in systems lacking a contemporary self-analogue or with poor data coverage. | |
dc.language | EN | |
dc.publisher | Blackwell Science Ltd. | |
dc.rights | Attribution 4.0 International | |
dc.rights.uri | https://creativecommons.org/licenses/by/4.0/ | |
dc.title | Relating seafloor geomorphology to subsurface architecture: How mass-transport deposits and knickpoint-zones build the stratigraphy of the deep-water Hikurangi Channel | |
dc.type | Journal article | |
dc.creator.author | Tek, Daniel E. | |
dc.creator.author | McArthur, Adam D. | |
dc.creator.author | Poyatos More, Miquel | |
dc.creator.author | Colombera, Luca | |
dc.creator.author | Patacci, Marco | |
dc.creator.author | Craven, Benjamin | |
dc.creator.author | McCaffrey, William D. | |
cristin.unitcode | 185,15,22,0 | |
cristin.unitname | Institutt for geofag | |
cristin.ispublished | true | |
cristin.fulltext | original | |
cristin.qualitycode | 2 | |
dc.identifier.cristin | 1990360 | |
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=Sedimentology&rft.volume=68&rft.spage=3141&rft.date=2021 | |
dc.identifier.jtitle | Sedimentology | |
dc.identifier.volume | 68 | |
dc.identifier.issue | 7 | |
dc.identifier.startpage | 3141 | |
dc.identifier.endpage | 3190 | |
dc.identifier.doi | https://doi.org/10.1111/sed.12890 | |
dc.identifier.urn | URN:NBN:no-94348 | |
dc.type.document | Tidsskriftartikkel | |
dc.type.peerreviewed | Peer reviewed | |
dc.source.issn | 0037-0746 | |
dc.identifier.fulltext | Fulltext https://www.duo.uio.no/bitstream/handle/10852/91758/1/Sedimentology%2B-%2B2021%2B-%2BTek%2B-%2BRelating%2Bseafloor%2Bgeomorphology%2Bto%2Bsubsurface%2Barchitecture%2B%2BHow%2Bmass%25E2%2580%2590transport%2Bdeposits%2Band.pdf | |
dc.type.version | PublishedVersion | |