FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2588416771> ?p ?o ?g. }

• W2588416771 endingPage "84" @default.
• W2588416771 startingPage "67" @default.
• W2588416771 abstract "Multibeam imagery and 3.5 kHz sub-bottom profiles acquired from CCGS Amundsen between 2003 and 2013 by ArcticNet and the Ocean Mapping Group at the University of New Brunswick provide information on seafloor features, geology, bathymetry and morphology in eastern Parry Channel and the adjoining large channels in the Canadian Arctic Archipelago. Together these include Peel Sound, Barrow Strait, Lancaster Sound, Wellington Channel, Prince Regent Inlet, Admiralty Inlet and Navy Board Inlet. Those data are in part complemented by high resolution single channel seismic reflection profiles acquired by the Geological Survey of Canada in the 1970s and 1980s and by sediment cores that provide chronological and depositional information. The occurrence and pattern of streamlined mega-scale ridge and groove lineations (MSGLs) indicate that these waterways were occupied by glacial ice streams in the past. Chronological information from marine and adjoining terrestrial areas suggests a long history of glacial events ranging in time from Early Pleistocene to Late Wisconsinan. Seafloor morphology and MSGL trends together with terrestrial ice flow patterns indicate that ice streams flowed into Barrow Strait from Peel Sound and Wellington Channel, and ice streams in Prince Regent, Admiralty and Navy Board inlets flowed northward into and eastward along Lancaster Sound. Recession of the ice stream westward along Parry Channel occurred ∼16 cal ka BP to 10.8 cal ka BP. Thick ice-contact sediments deposited by a late ice advance from Prince Regent Inlet constitute the seabed across a large area of western Lancaster Sound. Timing for that late ice advance appears to be bracketed between the 11.5 cal ka BP lift-off of the eastern Parry ice stream north of Prince Leopold Island and the ∼10.0 cal ka BP deglaciation of Prince Regent Inlet. Seafloor morphology and lineation trends suggest that ice delivered by the ice stream in Peel Sound was the westernmost tributary to the ice stream occupying Lancaster Sound during the late Wisconsinan glaciation. Bathymetric data and MSGLs indicate that the ice stream emanating from M'Clintock Channel flowed westward." @default.
• W2588416771 created "2017-02-24" @default.
• W2588416771 creator A5016586864 @default.
• W2588416771 creator A5031329659 @default.
• W2588416771 creator A5033366237 @default.
• W2588416771 creator A5037528768 @default.
• W2588416771 creator A5065640142 @default.
• W2588416771 creator A5066549496 @default.
• W2588416771 creator A5067467983 @default.
• W2588416771 creator A5080389444 @default.
• W2588416771 date "2017-03-01" @default.
• W2588416771 modified "2023-10-01" @default.
• W2588416771 title "Seafloor features delineate Late Wisconsinan ice stream configurations in eastern Parry Channel, Canadian Arctic Archipelago" @default.
• W2588416771 cites W1539894267 @default.
• W2588416771 cites W1853956339 @default.
• W2588416771 cites W1875334564 @default.
• W2588416771 cites W1879500246 @default.
• W2588416771 cites W1966429477 @default.
• W2588416771 cites W1968212627 @default.
• W2588416771 cites W1974155472 @default.
• W2588416771 cites W1975084362 @default.
• W2588416771 cites W1982565035 @default.
• W2588416771 cites W1982731139 @default.
• W2588416771 cites W1994730927 @default.
• W2588416771 cites W1999995634 @default.
• W2588416771 cites W2002789432 @default.
• W2588416771 cites W2005805597 @default.
• W2588416771 cites W2007310526 @default.
• W2588416771 cites W2009672870 @default.
• W2588416771 cites W2010966927 @default.
• W2588416771 cites W2013063174 @default.
• W2588416771 cites W2015211281 @default.
• W2588416771 cites W2022467063 @default.
• W2588416771 cites W2024958943 @default.
• W2588416771 cites W2030543908 @default.
• W2588416771 cites W2034033482 @default.
• W2588416771 cites W2038793362 @default.
• W2588416771 cites W2041809164 @default.
• W2588416771 cites W2046936370 @default.
• W2588416771 cites W2055214948 @default.
• W2588416771 cites W2068243085 @default.
• W2588416771 cites W2073290345 @default.
• W2588416771 cites W2074741021 @default.
• W2588416771 cites W2077453864 @default.
• W2588416771 cites W2082241947 @default.
• W2588416771 cites W2101538350 @default.
• W2588416771 cites W2105220545 @default.
• W2588416771 cites W2105688848 @default.
• W2588416771 cites W2112594191 @default.
• W2588416771 cites W2113159671 @default.
• W2588416771 cites W2122712105 @default.
• W2588416771 cites W2123118124 @default.
• W2588416771 cites W2123416608 @default.
• W2588416771 cites W2123481773 @default.
• W2588416771 cites W2132040233 @default.
• W2588416771 cites W2139743662 @default.
• W2588416771 cites W2149061491 @default.
• W2588416771 cites W32331197 @default.
• W2588416771 doi "https://doi.org/10.1016/j.quascirev.2017.02.001" @default.
• W2588416771 hasPublicationYear "2017" @default.
• W2588416771 type Work @default.
• W2588416771 sameAs 2588416771 @default.
• W2588416771 citedByCount "10" @default.
• W2588416771 countsByYear W25884167712017 @default.
• W2588416771 countsByYear W25884167712018 @default.
• W2588416771 countsByYear W25884167712019 @default.
• W2588416771 countsByYear W25884167712020 @default.
• W2588416771 countsByYear W25884167712021 @default.
• W2588416771 countsByYear W25884167712022 @default.
• W2588416771 countsByYear W25884167712023 @default.
• W2588416771 crossrefType "journal-article" @default.
• W2588416771 hasAuthorship W2588416771A5016586864 @default.
• W2588416771 hasAuthorship W2588416771A5031329659 @default.
• W2588416771 hasAuthorship W2588416771A5033366237 @default.
• W2588416771 hasAuthorship W2588416771A5037528768 @default.
• W2588416771 hasAuthorship W2588416771A5065640142 @default.
• W2588416771 hasAuthorship W2588416771A5066549496 @default.
• W2588416771 hasAuthorship W2588416771A5067467983 @default.
• W2588416771 hasAuthorship W2588416771A5080389444 @default.
• W2588416771 hasConcept C111368507 @default.
• W2588416771 hasConcept C117485682 @default.
• W2588416771 hasConcept C123750103 @default.
• W2588416771 hasConcept C12481700 @default.
• W2588416771 hasConcept C127313418 @default.
• W2588416771 hasConcept C136894858 @default.
• W2588416771 hasConcept C151730666 @default.
• W2588416771 hasConcept C197435368 @default.
• W2588416771 hasConcept C201289731 @default.
• W2588416771 hasConcept C203718221 @default.
• W2588416771 hasConcept C204207459 @default.
• W2588416771 hasConcept C518008717 @default.
• W2588416771 hasConcept C81820708 @default.
• W2588416771 hasConceptScore W2588416771C111368507 @default.
• W2588416771 hasConceptScore W2588416771C117485682 @default.
• W2588416771 hasConceptScore W2588416771C123750103 @default.
• W2588416771 hasConceptScore W2588416771C12481700 @default.
• W2588416771 hasConceptScore W2588416771C127313418 @default.
• W2588416771 hasConceptScore W2588416771C136894858 @default.

• next