Matches in SemOpenAlex for { <https://semopenalex.org/work/W1978274008> ?p ?o ?g. }
- W1978274008 endingPage "1129" @default.
- W1978274008 startingPage "1111" @default.
- W1978274008 abstract "In this paper new and previously published data on the Pleistocene glacial impact on the NW European margin from Ireland to Svalbard (between c. 48°N–80°N) are compiled. The morphology of the glaciated part of the European margin strongly reflects repeated occurrence of fast-moving ice streams, creating numerous glacial troughs/channels that are separated by shallow bank areas. End-moraines have been identified at several locations on the shelf, suggesting shelf-edge glaciation along the major part of the margin during the Last Glacial Maximum. Deposition of stacked units of glacigenic debris flows on the continental slope form fans at a number of locations from 55°N and northwards, whereas the margin to the south of this is characterised by the presence of submarine canyons. Glaciation curves, based primarily on information from the glacial fed fan systems, that depict the Pleistocene trends in extent of glaciations along the margin have been compiled. These curves suggest that extensive shelf glaciations started around Svalbard at 1.6–1.3 Ma, while repeated periods of shelf-edge glaciations on the UK margin started with MIS 12 (c. 0.45 Ma). The available evidence for MIS 2 suggest that shelf-edge glaciation for the whole margin was reached between c. 28 and 22 14C ka BP and maximum positions after this were more limited in some regions (North Sea and Lofoten). The last glacial advance on the margin has been dated to 15–13.5 14C ka BP, and by c. 13 14C ka BP the shelf areas were completely deglaciated. The Younger Dryas (Loch Lomond) advance reached the coastal areas in only a few regions." @default.
- W1978274008 created "2016-06-24" @default.
- W1978274008 creator A5024590900 @default.
- W1978274008 creator A5045420367 @default.
- W1978274008 creator A5048097438 @default.
- W1978274008 creator A5057363667 @default.
- W1978274008 creator A5060385090 @default.
- W1978274008 creator A5060615194 @default.
- W1978274008 creator A5069683261 @default.
- W1978274008 creator A5073261865 @default.
- W1978274008 creator A5083762411 @default.
- W1978274008 date "2005-11-01" @default.
- W1978274008 modified "2023-10-18" @default.
- W1978274008 title "Pleistocene glacial history of the NW European continental margin" @default.
- W1978274008 cites W127813593 @default.
- W1978274008 cites W1528044173 @default.
- W1978274008 cites W1567293375 @default.
- W1978274008 cites W1968360785 @default.
- W1978274008 cites W1969367513 @default.
- W1978274008 cites W1970957904 @default.
- W1978274008 cites W1971016183 @default.
- W1978274008 cites W1973012465 @default.
- W1978274008 cites W1974792344 @default.
- W1978274008 cites W1977948539 @default.
- W1978274008 cites W1978904543 @default.
- W1978274008 cites W1979887963 @default.
- W1978274008 cites W1980043759 @default.
- W1978274008 cites W1981613439 @default.
- W1978274008 cites W1981730693 @default.
- W1978274008 cites W1982369207 @default.
- W1978274008 cites W1985813939 @default.
- W1978274008 cites W1986810489 @default.
- W1978274008 cites W1988277361 @default.
- W1978274008 cites W1989915921 @default.
- W1978274008 cites W1990468006 @default.
- W1978274008 cites W1990776325 @default.
- W1978274008 cites W1992590047 @default.
- W1978274008 cites W1994214988 @default.
- W1978274008 cites W1995487081 @default.
- W1978274008 cites W1995715226 @default.
- W1978274008 cites W2000084287 @default.
- W1978274008 cites W2002069692 @default.
- W1978274008 cites W2002356564 @default.
- W1978274008 cites W2002976815 @default.
- W1978274008 cites W2002984609 @default.
- W1978274008 cites W2003300047 @default.
- W1978274008 cites W2004413882 @default.
- W1978274008 cites W2006557606 @default.
- W1978274008 cites W2007577561 @default.
- W1978274008 cites W2008429875 @default.
- W1978274008 cites W2011440332 @default.
- W1978274008 cites W2015107149 @default.
- W1978274008 cites W2015250886 @default.
- W1978274008 cites W2026840429 @default.
- W1978274008 cites W2028109772 @default.
- W1978274008 cites W2028390326 @default.
- W1978274008 cites W2028413048 @default.
- W1978274008 cites W2034639312 @default.
- W1978274008 cites W2037330253 @default.
- W1978274008 cites W2039120572 @default.
- W1978274008 cites W2041188833 @default.
- W1978274008 cites W2043070682 @default.
- W1978274008 cites W2044974852 @default.
- W1978274008 cites W2045967691 @default.
- W1978274008 cites W2046913473 @default.
- W1978274008 cites W2047261493 @default.
- W1978274008 cites W2047972453 @default.
- W1978274008 cites W2050336730 @default.
- W1978274008 cites W2051426483 @default.
- W1978274008 cites W2053318141 @default.
- W1978274008 cites W2053727446 @default.
- W1978274008 cites W2054760671 @default.
- W1978274008 cites W2054953518 @default.
- W1978274008 cites W2056720591 @default.
- W1978274008 cites W2056797720 @default.
- W1978274008 cites W2057526784 @default.
- W1978274008 cites W2059413201 @default.
- W1978274008 cites W2068165906 @default.
- W1978274008 cites W2068668124 @default.
- W1978274008 cites W2068909250 @default.
- W1978274008 cites W2069339378 @default.
- W1978274008 cites W2071659606 @default.
- W1978274008 cites W2071807884 @default.
- W1978274008 cites W2076488317 @default.
- W1978274008 cites W2079670946 @default.
- W1978274008 cites W2081452654 @default.
- W1978274008 cites W2081832652 @default.
- W1978274008 cites W2083622717 @default.
- W1978274008 cites W2084086407 @default.
- W1978274008 cites W2084711994 @default.
- W1978274008 cites W2085249241 @default.
- W1978274008 cites W2089366808 @default.
- W1978274008 cites W2089468565 @default.
- W1978274008 cites W2090412888 @default.
- W1978274008 cites W2090682838 @default.
- W1978274008 cites W2090694986 @default.
- W1978274008 cites W2092339430 @default.
- W1978274008 cites W2093437232 @default.