FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2142956211> ?p ?o ?g. }

• W2142956211 endingPage "54" @default.
• W2142956211 startingPage "33" @default.
• W2142956211 abstract "Abstract The presence of ice during the Late Cenozoic distinguishes the nature and rates of processes on high-latitude margins from those elsewhere. Ice sheets terminating in marine waters deliver icebergs, meltwater and debris to high-latitude seas. Sea ice influences ocean salinity structure and downslope water and sediment transfer, and also transports fine-grained sediments over long distances. These cryospheric processes have led to the development of a distinctive sedimentary architecture on modern high-latitude continental margins. Large submarine fans made up almost entirely of stacked debris flows are present around the Norwegian-Greenland Sea. Large slides are located in a variety of settings relative to rates of sediment delivery from Quaternary ice-sheet margins, but no large slides have been mapped on the East Greenland margin. However, extensive channel systems and sediment-wave fields are present in the Greenland Basin, probably related to intermittent downslope flow of dense water and turbidity currents. The extensive NE Greenland shelf was not innundated by ice-sheet advance during recent full-glacial conditions, allowing sea-ice and deep-water production during both interglacials and full-glacials. Changes in the nature and rate of sedimentation within the Greenland Basin should provide clues on the rate of dense-water production, with implications for thermohaline circulation in the North Atlantic. Other erosional and depositional features on the Norwegian-Greenland Sea margins include canyons and contourite drifts. High-relief tectonic features influence sediment reworking by turbidity currents at abyssal depths. A simple conceptual model for glacier-influenced marine sedimentation summarizes the role of cryospheric processes in high-latitude margin sedimentary environments." @default.
• W2142956211 created "2016-06-24" @default.
• W2142956211 creator A5000303897 @default.
• W2142956211 creator A5000615017 @default.
• W2142956211 creator A5029363373 @default.
• W2142956211 creator A5032664647 @default.
• W2142956211 creator A5069062834 @default.
• W2142956211 creator A5081009247 @default.
• W2142956211 date "2002-01-01" @default.
• W2142956211 modified "2023-09-26" @default.
• W2142956211 title "On the architecture of high-latitude continental margins: the influence of ice-sheet and sea-ice processes in the Polar North Atlantic" @default.
• W2142956211 cites W103337811 @default.
• W2142956211 cites W11148313 @default.
• W2142956211 cites W1528044173 @default.
• W2142956211 cites W1556223768 @default.
• W2142956211 cites W1558001919 @default.
• W2142956211 cites W1639268213 @default.
• W2142956211 cites W1875334564 @default.
• W2142956211 cites W1964388422 @default.
• W2142956211 cites W1968402863 @default.
• W2142956211 cites W1972985749 @default.
• W2142956211 cites W1973227610 @default.
• W2142956211 cites W1975637812 @default.
• W2142956211 cites W1976921052 @default.
• W2142956211 cites W1977293294 @default.
• W2142956211 cites W1978904543 @default.
• W2142956211 cites W1979352924 @default.
• W2142956211 cites W1981028614 @default.
• W2142956211 cites W1982471743 @default.
• W2142956211 cites W1983631589 @default.
• W2142956211 cites W1985167833 @default.
• W2142956211 cites W1989915921 @default.
• W2142956211 cites W1997690170 @default.
• W2142956211 cites W1998877509 @default.
• W2142956211 cites W2002356564 @default.
• W2142956211 cites W2003466627 @default.
• W2142956211 cites W2008429875 @default.
• W2142956211 cites W2010608057 @default.
• W2142956211 cites W2016440287 @default.
• W2142956211 cites W2017938799 @default.
• W2142956211 cites W2019979254 @default.
• W2142956211 cites W2021049577 @default.
• W2142956211 cites W2021296757 @default.
• W2142956211 cites W2023007775 @default.
• W2142956211 cites W2026838234 @default.
• W2142956211 cites W2027624641 @default.
• W2142956211 cites W2028946394 @default.
• W2142956211 cites W2029202682 @default.
• W2142956211 cites W2031564252 @default.
• W2142956211 cites W2032053405 @default.
• W2142956211 cites W2034639312 @default.
• W2142956211 cites W2034659250 @default.
• W2142956211 cites W2039771357 @default.
• W2142956211 cites W2043672520 @default.
• W2142956211 cites W2043987388 @default.
• W2142956211 cites W2048496723 @default.
• W2142956211 cites W2054953518 @default.
• W2142956211 cites W2055674526 @default.
• W2142956211 cites W2057406009 @default.
• W2142956211 cites W2059859557 @default.
• W2142956211 cites W2064076409 @default.
• W2142956211 cites W20641944 @default.
• W2142956211 cites W2066227436 @default.
• W2142956211 cites W2067923119 @default.
• W2142956211 cites W2068244057 @default.
• W2142956211 cites W2073045875 @default.
• W2142956211 cites W2073673183 @default.
• W2142956211 cites W2078076761 @default.
• W2142956211 cites W2079670946 @default.
• W2142956211 cites W2081452654 @default.
• W2142956211 cites W2081662319 @default.
• W2142956211 cites W2081832652 @default.
• W2142956211 cites W2084545552 @default.
• W2142956211 cites W2089366808 @default.
• W2142956211 cites W2089468565 @default.
• W2142956211 cites W2091645757 @default.
• W2142956211 cites W2092339430 @default.
• W2142956211 cites W2093874911 @default.
• W2142956211 cites W2094822062 @default.
• W2142956211 cites W2096072946 @default.
• W2142956211 cites W2097945396 @default.
• W2142956211 cites W2098786925 @default.
• W2142956211 cites W2107422206 @default.
• W2142956211 cites W2123416608 @default.
• W2142956211 cites W2127148136 @default.
• W2142956211 cites W2136232108 @default.
• W2142956211 cites W2143017711 @default.
• W2142956211 cites W2147239287 @default.
• W2142956211 cites W2149061491 @default.
• W2142956211 cites W2152770194 @default.
• W2142956211 cites W2157131198 @default.
• W2142956211 cites W2165917981 @default.
• W2142956211 cites W2344153379 @default.
• W2142956211 cites W2483167084 @default.
• W2142956211 cites W256631737 @default.
• W2142956211 cites W30301213 @default.
• W2142956211 cites W3178231311 @default.
• W2142956211 doi "https://doi.org/10.1144/gsl.sp.2002.203.01.03" @default.

• next