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dc.contributor.authorPohl, F
dc.contributor.authorEggenhuisen, JT
dc.contributor.authorde Leeuw, J
dc.contributor.authorCartigny, MJB
dc.contributor.authorBrooks, HL
dc.contributor.authorSpychala, YT
dc.date.accessioned2022-10-24T14:56:38Z
dc.date.available2022-10-24T14:56:38Z
dc.date.issued2022-09-29
dc.identifier.issn1469-5081
dc.identifier.issn1469-5081
dc.identifier.otherPII S0016756822000693
dc.identifier.urihttp://hdl.handle.net/10026.1/19748
dc.description.abstract

<jats:title>Abstract</jats:title> <jats:p>Turbidity currents commonly bypass sediment in submarine channels on the continental slope, and deposit sediment lobes farther down-dip on the flat and unconfined abyssal plain. Seafloor and outcrop data have shown that the transition from bypass to deposition usually occurs over complex zones referred to as channel–lobe transition zones (CLTZs). Recognition of these zones in cores and outcrop remains challenging due to a lack of characteristic sedimentary facies and structures. This paper focuses on Unit E of the Permian Fort Brown Formation in the Karoo Basin, South Africa, in the Slagtersfontein outcrop complex, which has previously been interpreted as a CLTZ. This study integrates thin-section micrographs, sedimentary facies, bed-set and stratigraphic architecture, and palaeoflow directions to achieve a multiscale analysis of CLTZ features. A novel process-based facies scheme is developed to evaluate deposits in terms of the depositional or erosional tendencies of the flows that formed them. This scheme allows bypass to be distinguished from depositional zones by the spatial distribution of certain sediment facies. Areas of net sediment bypass were predominantly marked by erosive sediment facies and a larger variability in palaeoflow direction while depositional areas showed a lower variability in palaeoflow directions. Metre-scale structures in the bypass-dominated area reveal seafloor erosion and scour formation. Field relations suggest the presence of a ∼500 m long mega-scour in the CLTZ. The characteristic structures documented here are applicable for identifying CLTZs in sparse datasets such as outcrops with limited palaeogeographical context and sediment cores obtained from subsurface systems.</jats:p>

dc.format.extent107-126
dc.languageen
dc.language.isoen
dc.publisherCambridge University Press
dc.subjectturbidity current
dc.subjectdeep marine
dc.subjectsediment bypass
dc.subjectsediment facies
dc.subjectscour fields
dc.titleReconstructing sedimentary processes in a Permian channel–lobe transition zone: an outcrop study in the Karoo Basin, South Africa
dc.typejournal-article
dc.typeArticle
plymouth.author-urlhttps://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000861632100001&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=11bb513d99f797142bcfeffcc58ea008
plymouth.issue1
plymouth.volume160
plymouth.publisher-urlhttp://dx.doi.org/10.1017/s0016756822000693
plymouth.publication-statusPublished
plymouth.journalGeological Magazine
dc.identifier.doi10.1017/s0016756822000693
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Biological and Marine Sciences
plymouth.organisational-group/Plymouth/Users by role
plymouth.organisational-group/Plymouth/Users by role/Academics
dcterms.dateAccepted2022-06-20
dc.rights.embargodate2022-10-25
dc.identifier.eissn1469-5081
dc.rights.embargoperiodNot known
rioxxterms.versionofrecord10.1017/s0016756822000693
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/all-rights-reserved
rioxxterms.typeJournal Article/Review


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