Matches in SemOpenAlex for { <https://semopenalex.org/work/W2068909250> ?p ?o ?g. }
- W2068909250 endingPage "55" @default.
- W2068909250 startingPage "37" @default.
- W2068909250 abstract "The classical model of trough mouth fan (TMF) formation was developed in the Polar North Atlantic to explain large submarine fans situated in front of bathymetric troughs that extend across continental shelves to the shelf break. This model emphasizes the delivery of large volumes of subglacial sediment to the termini of ice streams flowing along troughs, and subsequent re-deposition of this glacigenic sediment down the continental slope via debris-flow processes. However, there is considerable variation in terms of the morphology and large-scale sediment architecture of continental slopes in front of palaeo-ice streams. This variability reflects differences in slope gradient, the relative contributions of meltwater sedimentation compared with debris-flow deposition, and sediment supply/geology of the adjacent continental shelf. TMF development is favoured under conditions of a low (<1°) slope gradient; a passive-margin tectonic setting; abundant, readily erodible sediments on the continental shelf - and thus associated high rates of sediment delivery to the shelf edge; and a wide continental shelf. The absence of large sediment fans on continental slopes in front of cross-shelf troughs should not, however, be taken to indicate the former absence of palaeo-ice streams in the geological record." @default.
- W2068909250 created "2016-06-24" @default.
- W2068909250 creator A5000303897 @default.
- W2068909250 creator A5029363373 @default.
- W2068909250 creator A5074481779 @default.
- W2068909250 creator A5081009247 @default.
- W2068909250 date "2003-03-01" @default.
- W2068909250 modified "2023-09-27" @default.
- W2068909250 title "Palaeo-ice streams, trough mouth fans and high-latitude continental slope sedimentation" @default.
- W2068909250 cites W1556373907 @default.
- W2068909250 cites W1558001919 @default.
- W2068909250 cites W1595395708 @default.
- W2068909250 cites W1601435429 @default.
- W2068909250 cites W1973000527 @default.
- W2068909250 cites W1973227610 @default.
- W2068909250 cites W1973668598 @default.
- W2068909250 cites W1974792344 @default.
- W2068909250 cites W1977393082 @default.
- W2068909250 cites W1978135243 @default.
- W2068909250 cites W1978904543 @default.
- W2068909250 cites W1979706861 @default.
- W2068909250 cites W1982980538 @default.
- W2068909250 cites W1989671436 @default.
- W2068909250 cites W1997690170 @default.
- W2068909250 cites W2005682478 @default.
- W2068909250 cites W2006091704 @default.
- W2068909250 cites W2016440287 @default.
- W2068909250 cites W2021959819 @default.
- W2068909250 cites W2025271308 @default.
- W2068909250 cites W2026838234 @default.
- W2068909250 cites W2027110890 @default.
- W2068909250 cites W2028109772 @default.
- W2068909250 cites W2028806816 @default.
- W2068909250 cites W2029202682 @default.
- W2068909250 cites W2029486441 @default.
- W2068909250 cites W2034074018 @default.
- W2068909250 cites W2034946003 @default.
- W2068909250 cites W2041005557 @default.
- W2068909250 cites W2043587023 @default.
- W2068909250 cites W2044974852 @default.
- W2068909250 cites W2047064059 @default.
- W2068909250 cites W2047970690 @default.
- W2068909250 cites W2047972453 @default.
- W2068909250 cites W2054953518 @default.
- W2068909250 cites W2057406009 @default.
- W2068909250 cites W2058005766 @default.
- W2068909250 cites W2058218337 @default.
- W2068909250 cites W2059136538 @default.
- W2068909250 cites W2067923119 @default.
- W2068909250 cites W2069169424 @default.
- W2068909250 cites W2069339378 @default.
- W2068909250 cites W2073045875 @default.
- W2068909250 cites W2078076761 @default.
- W2068909250 cites W2081662319 @default.
- W2068909250 cites W2082047738 @default.
- W2068909250 cites W2084545552 @default.
- W2068909250 cites W2089366808 @default.
- W2068909250 cites W2089468565 @default.
- W2068909250 cites W2092339430 @default.
- W2068909250 cites W2097945396 @default.
- W2068909250 cites W2098786925 @default.
- W2068909250 cites W2108751654 @default.
- W2068909250 cites W2113159671 @default.
- W2068909250 cites W2123416608 @default.
- W2068909250 cites W2142005755 @default.
- W2068909250 cites W2149061491 @default.
- W2068909250 cites W2162081980 @default.
- W2068909250 cites W2170988224 @default.
- W2068909250 cites W2344153379 @default.
- W2068909250 cites W2472552424 @default.
- W2068909250 cites W59269465 @default.
- W2068909250 doi "https://doi.org/10.1080/03009480310001858" @default.
- W2068909250 hasPublicationYear "2003" @default.
- W2068909250 type Work @default.
- W2068909250 sameAs 2068909250 @default.
- W2068909250 citedByCount "153" @default.
- W2068909250 countsByYear W20689092502012 @default.
- W2068909250 countsByYear W20689092502013 @default.
- W2068909250 countsByYear W20689092502014 @default.
- W2068909250 countsByYear W20689092502015 @default.
- W2068909250 countsByYear W20689092502016 @default.
- W2068909250 countsByYear W20689092502017 @default.
- W2068909250 countsByYear W20689092502018 @default.
- W2068909250 countsByYear W20689092502019 @default.
- W2068909250 countsByYear W20689092502020 @default.
- W2068909250 countsByYear W20689092502021 @default.
- W2068909250 countsByYear W20689092502022 @default.
- W2068909250 countsByYear W20689092502023 @default.
- W2068909250 crossrefType "journal-article" @default.
- W2068909250 hasAuthorship W2068909250A5000303897 @default.
- W2068909250 hasAuthorship W2068909250A5029363373 @default.
- W2068909250 hasAuthorship W2068909250A5074481779 @default.
- W2068909250 hasAuthorship W2068909250A5081009247 @default.
- W2068909250 hasConcept C100834320 @default.
- W2068909250 hasConcept C111368507 @default.
- W2068909250 hasConcept C114793014 @default.
- W2068909250 hasConcept C127313418 @default.
- W2068909250 hasConcept C139719470 @default.