FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2132657985> ?p ?o ?g. }

• W2132657985 endingPage "110" @default.
• W2132657985 startingPage "107" @default.
• W2132657985 abstract "Research Article| February 01, 2010 Late Pliocene–Pleistocene development of the Barents Sea Ice Sheet Jan Sverre Laberg; Jan Sverre Laberg * 1Department of Geology, University of Tromsø, N-9037 Tromsø, Norway *E-mail: jan.laberg@uit.no. Search for other works by this author on: GSW Google Scholar Karin Andreassen; Karin Andreassen 1Department of Geology, University of Tromsø, N-9037 Tromsø, Norway Search for other works by this author on: GSW Google Scholar Jochen Knies; Jochen Knies 2Geological Survey of Norway, N-7491 Trondheim, Norway Search for other works by this author on: GSW Google Scholar Tore O. Vorren; Tore O. Vorren 1Department of Geology, University of Tromsø, N-9037 Tromsø, Norway Search for other works by this author on: GSW Google Scholar Monica Winsborrow Monica Winsborrow 1Department of Geology, University of Tromsø, N-9037 Tromsø, Norway Search for other works by this author on: GSW Google Scholar Geology (2010) 38 (2): 107–110. https://doi.org/10.1130/G30193.1 Article history received: 03 Mar 2009 rev-recd: 14 Aug 2009 accepted: 18 Aug 2009 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Jan Sverre Laberg, Karin Andreassen, Jochen Knies, Tore O. Vorren, Monica Winsborrow; Late Pliocene–Pleistocene development of the Barents Sea Ice Sheet. Geology 2010;; 38 (2): 107–110. doi: https://doi.org/10.1130/G30193.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The late Pliocene–Pleistocene paleoenvironment has been reconstructed based on three-dimensional seismic data from the southwestern Barents Sea continental margin. During the late Pliocene–early Pleistocene, continental slope sediments were predominantly deposited from meltwater overflows and underflows. The seismic stratigraphy of the early–middle Pleistocene shows both glaciomarine sediment input from channelized meltwater discharge and the first indications of large debris-flow deposits on the continental slope, originating from input of subglacial deformation till eroded and transported by ice streams. During the middle–late Pleistocene, large debris flows dominated the slope succession. From the above results we infer the following evolution in the Barents Sea: (1) a temperate Barents Sea Ice Sheet with channelized meltwater flow developed during the late Pliocene–early Pleistocene; (2) alternating glacial periods of ice with channelized meltwater flow and the first periods of ice, including ice streams, characterized the early and middle Pleistocene; and (3) more polar ice conditions and a Barents Sea Ice Sheet that mainly included large ice streams, with little or no channelized meltwater flow, occurred in the middle and late Pleistocene. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2132657985 created "2016-06-24" @default.
• W2132657985 creator A5035624665 @default.
• W2132657985 creator A5038582799 @default.
• W2132657985 creator A5064116598 @default.
• W2132657985 creator A5068239197 @default.
• W2132657985 creator A5069683261 @default.
• W2132657985 date "2010-02-01" @default.
• W2132657985 modified "2023-09-27" @default.
• W2132657985 title "Late Pliocene-Pleistocene development of the Barents Sea Ice Sheet" @default.
• W2132657985 cites W1977210405 @default.
• W2132657985 cites W1982980538 @default.
• W2132657985 cites W1989915921 @default.
• W2132657985 cites W1992491233 @default.
• W2132657985 cites W1992590047 @default.
• W2132657985 cites W2002356564 @default.
• W2132657985 cites W2033870424 @default.
• W2132657985 cites W2037783183 @default.
• W2132657985 cites W2049611787 @default.
• W2132657985 cites W2059136538 @default.
• W2132657985 cites W2064002524 @default.
• W2132657985 cites W2069339378 @default.
• W2132657985 cites W2071807884 @default.
• W2132657985 cites W2072140164 @default.
• W2132657985 cites W2081662319 @default.
• W2132657985 cites W2083953706 @default.
• W2132657985 cites W2085718280 @default.
• W2132657985 cites W2089468565 @default.
• W2132657985 cites W2107442661 @default.
• W2132657985 cites W4236408527 @default.
• W2132657985 doi "https://doi.org/10.1130/g30193.1" @default.
• W2132657985 hasPublicationYear "2010" @default.
• W2132657985 type Work @default.
• W2132657985 sameAs 2132657985 @default.
• W2132657985 citedByCount "73" @default.
• W2132657985 countsByYear W21326579852012 @default.
• W2132657985 countsByYear W21326579852013 @default.
• W2132657985 countsByYear W21326579852014 @default.
• W2132657985 countsByYear W21326579852015 @default.
• W2132657985 countsByYear W21326579852016 @default.
• W2132657985 countsByYear W21326579852017 @default.
• W2132657985 countsByYear W21326579852018 @default.
• W2132657985 countsByYear W21326579852019 @default.
• W2132657985 countsByYear W21326579852020 @default.
• W2132657985 countsByYear W21326579852021 @default.
• W2132657985 countsByYear W21326579852022 @default.
• W2132657985 countsByYear W21326579852023 @default.
• W2132657985 crossrefType "journal-article" @default.
• W2132657985 hasAuthorship W2132657985A5035624665 @default.
• W2132657985 hasAuthorship W2132657985A5038582799 @default.
• W2132657985 hasAuthorship W2132657985A5064116598 @default.
• W2132657985 hasAuthorship W2132657985A5068239197 @default.
• W2132657985 hasAuthorship W2132657985A5069683261 @default.
• W2132657985 hasConcept C127313418 @default.
• W2132657985 hasConcept C151730666 @default.
• W2132657985 hasConcept C161191863 @default.
• W2132657985 hasConcept C199360897 @default.
• W2132657985 hasConcept C2778447006 @default.
• W2132657985 hasConcept C2778805511 @default.
• W2132657985 hasConcept C41008148 @default.
• W2132657985 hasConcept C53570757 @default.
• W2132657985 hasConceptScore W2132657985C127313418 @default.
• W2132657985 hasConceptScore W2132657985C151730666 @default.
• W2132657985 hasConceptScore W2132657985C161191863 @default.
• W2132657985 hasConceptScore W2132657985C199360897 @default.
• W2132657985 hasConceptScore W2132657985C2778447006 @default.
• W2132657985 hasConceptScore W2132657985C2778805511 @default.
• W2132657985 hasConceptScore W2132657985C41008148 @default.
• W2132657985 hasConceptScore W2132657985C53570757 @default.
• W2132657985 hasIssue "2" @default.
• W2132657985 hasLocation W21326579851 @default.
• W2132657985 hasOpenAccess W2132657985 @default.
• W2132657985 hasPrimaryLocation W21326579851 @default.
• W2132657985 hasRelatedWork W1735551483 @default.
• W2132657985 hasRelatedWork W1973699888 @default.
• W2132657985 hasRelatedWork W2015230985 @default.
• W2132657985 hasRelatedWork W2017786959 @default.
• W2132657985 hasRelatedWork W2079317421 @default.
• W2132657985 hasRelatedWork W2080374959 @default.
• W2132657985 hasRelatedWork W2083267600 @default.
• W2132657985 hasRelatedWork W2262727046 @default.
• W2132657985 hasRelatedWork W2299434101 @default.
• W2132657985 hasRelatedWork W4254011760 @default.
• W2132657985 hasVolume "38" @default.
• W2132657985 isParatext "false" @default.
• W2132657985 isRetracted "false" @default.
• W2132657985 magId "2132657985" @default.
• W2132657985 workType "article" @default.