FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2321886574> ?p ?o ?g. }

• W2321886574 endingPage "134" @default.
• W2321886574 startingPage "131" @default.
• W2321886574 abstract "Research Article| February 01, 2013 Variable history of Quaternary ice-sheet advance across the Beaufort Sea margin, Arctic Ocean C.L. Batchelor; C.L. Batchelor 1Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK Search for other works by this author on: GSW Google Scholar J.A. Dowdeswell; J.A. Dowdeswell 1Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK Search for other works by this author on: GSW Google Scholar J.T. Pietras J.T. Pietras 2BP Exploration Operating Company Limited, 240 4th Avenue SW, Calgary, Alberta T2P 2H8, Canada Search for other works by this author on: GSW Google Scholar Author and Article Information C.L. Batchelor 1Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK J.A. Dowdeswell 1Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK J.T. Pietras 2BP Exploration Operating Company Limited, 240 4th Avenue SW, Calgary, Alberta T2P 2H8, Canada Publisher: Geological Society of America Received: 24 May 2012 Revision Received: 21 Aug 2012 Accepted: 22 Aug 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2013) 41 (2): 131–134. https://doi.org/10.1130/G33669.1 Article history Received: 24 May 2012 Revision Received: 21 Aug 2012 Accepted: 22 Aug 2012 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 C.L. Batchelor, J.A. Dowdeswell, J.T. Pietras; Variable history of Quaternary ice-sheet advance across the Beaufort Sea margin, Arctic Ocean. Geology 2013;; 41 (2): 131–134. doi: https://doi.org/10.1130/G33669.1 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 seismic stratigraphy and architecture of the Beaufort Sea shelf and slope are investigated using a comprehensive grid of high-resolution two-dimensional seismic reflection data. Three cross-shelf troughs, representing locations of former ice streams draining a 1000-km-long section of the Laurentide Ice Sheet (LIS) are examined: the Mackenzie, Amundsen Gulf, and M’Clure Strait systems. Dynamics of these paleo-ice streams influenced ice-sheet configuration and may have forced abrupt climatic change through delivery of ice and freshwater to the Arctic Ocean. A comprehensive understanding of their geometry and dynamics is crucial for constraining numerical models of the LIS. Evidence for two Quaternary ice advances to the shelf break is interpreted from the Mackenzie Trough. By contrast, seismic stratigraphy of the Amundsen Gulf Trough, 400 km east of the Mackenzie Trough, records at least nine Quaternary ice advances. Here, the outer shelf consists of stacked till sheets, extending to the shelf break and forming a trough-mouth fan. The contrasting glacial histories of these neighboring ice streams are explained by their positions within the LIS; the Mackenzie Trough ice stream was situated at the extreme northwest ice-sheet margin, whereas the Amundsen Gulf ice stream had a more central location and larger drainage basin, supplying significant quantities of ice and sediment to the Arctic Ocean through much of the Quaternary. The M’Clure Strait Trough probably possesses a similar architecture to the Amundsen Gulf Trough, and an even larger trough-mouth fan. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2321886574 created "2016-06-24" @default.
• W2321886574 creator A5000303897 @default.
• W2321886574 creator A5006827140 @default.
• W2321886574 creator A5086825747 @default.
• W2321886574 date "2012-11-13" @default.
• W2321886574 modified "2023-10-17" @default.
• W2321886574 title "Variable history of Quaternary ice-sheet advance across the Beaufort Sea margin, Arctic Ocean" @default.
• W2321886574 cites W1569453219 @default.
• W2321886574 cites W1809829952 @default.
• W2321886574 cites W1968212627 @default.
• W2321886574 cites W2048104745 @default.
• W2321886574 cites W2061587877 @default.
• W2321886574 cites W2081662319 @default.
• W2321886574 cites W2103796175 @default.
• W2321886574 cites W2118816873 @default.
• W2321886574 cites W2123860995 @default.
• W2321886574 cites W2139743662 @default.
• W2321886574 cites W2150480637 @default.
• W2321886574 doi "https://doi.org/10.1130/g33669.1" @default.
• W2321886574 hasPublicationYear "2012" @default.
• W2321886574 type Work @default.
• W2321886574 sameAs 2321886574 @default.
• W2321886574 citedByCount "24" @default.
• W2321886574 countsByYear W23218865742013 @default.
• W2321886574 countsByYear W23218865742014 @default.
• W2321886574 countsByYear W23218865742015 @default.
• W2321886574 countsByYear W23218865742016 @default.
• W2321886574 countsByYear W23218865742017 @default.
• W2321886574 countsByYear W23218865742018 @default.
• W2321886574 countsByYear W23218865742019 @default.
• W2321886574 countsByYear W23218865742021 @default.
• W2321886574 countsByYear W23218865742022 @default.
• W2321886574 crossrefType "journal-article" @default.
• W2321886574 hasAuthorship W2321886574A5000303897 @default.
• W2321886574 hasAuthorship W2321886574A5006827140 @default.
• W2321886574 hasAuthorship W2321886574A5086825747 @default.
• W2321886574 hasConcept C111368507 @default.
• W2321886574 hasConcept C127313418 @default.
• W2321886574 hasConcept C161191863 @default.
• W2321886574 hasConcept C2778805511 @default.
• W2321886574 hasConcept C28115305 @default.
• W2321886574 hasConcept C41008148 @default.
• W2321886574 hasConcept C518008717 @default.
• W2321886574 hasConceptScore W2321886574C111368507 @default.
• W2321886574 hasConceptScore W2321886574C127313418 @default.
• W2321886574 hasConceptScore W2321886574C161191863 @default.
• W2321886574 hasConceptScore W2321886574C2778805511 @default.
• W2321886574 hasConceptScore W2321886574C28115305 @default.
• W2321886574 hasConceptScore W2321886574C41008148 @default.
• W2321886574 hasConceptScore W2321886574C518008717 @default.
• W2321886574 hasIssue "2" @default.
• W2321886574 hasLocation W23218865741 @default.
• W2321886574 hasOpenAccess W2321886574 @default.
• W2321886574 hasPrimaryLocation W23218865741 @default.
• W2321886574 hasRelatedWork W1522185562 @default.
• W2321886574 hasRelatedWork W1931798023 @default.
• W2321886574 hasRelatedWork W1986737027 @default.
• W2321886574 hasRelatedWork W1993519049 @default.
• W2321886574 hasRelatedWork W2102821267 @default.
• W2321886574 hasRelatedWork W2168644405 @default.
• W2321886574 hasRelatedWork W2383038422 @default.
• W2321886574 hasRelatedWork W3205642098 @default.
• W2321886574 hasRelatedWork W4232707782 @default.
• W2321886574 hasRelatedWork W989506215 @default.
• W2321886574 hasVolume "41" @default.
• W2321886574 isParatext "false" @default.
• W2321886574 isRetracted "false" @default.
• W2321886574 magId "2321886574" @default.
• W2321886574 workType "article" @default.