FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2520993003> ?p ?o ?g. }

• W2520993003 endingPage "87" @default.
• W2520993003 startingPage "72" @default.
• W2520993003 abstract "The fore-mountain areas of southern Poland are locally composed of the coarse-grained sediments of alluvial fans, which created unusual conditions under the advancing Scandinavian Ice Sheet during the Elsterian glaciation. This highly permeable substratum potentially enabled rapid outflow of meltwater from the ice sheet base, thereby reducing the water pressure and strongly influencing the ice sheet dynamics. The subglacial conditions and the relationship between the ice sheet behaviour and its coarse-grained substratum were studied at the foreland of the western Carpathian Mountains. The sedimentological and structural analysis of the till and related sediments that were deposited above the alluvial gravel of the fore-mountain fans are presented. The study indicates that despite the high permeability of the coarse-grained substratum, it did not slow the ice sheet movement. Conversely, the ice sheet moved mainly due to basal slip and locally shallow deformations. This was a consequence of very high basal water pressure, which resulted largely from the presence of permafrost that restricted subglacial groundwater outflow. In addition, the ice sheet substratum was inclined opposite to the direction of its movement, increasing the pressure of the subglacial water. Numerous subhorizontal sandy laminae within the till indicate that the meltwater from the ice sheet base was drained by a water film along the ice/bed interface. The water escape structures within the till and subtill sediments indicate the occasional instability of the ice sheet hydrological system and suggest that the meltwater was periodically stored in the ice sheet base. Temporal changes occurring in the ice sheet hydrological system might indicate variations in the ice sheet behaviour; i.e. phases of relatively fast ice flow and phases of ice stagnation. The latter were probably correlated with the freezing of the ice margin to its base. The study shows how the coarse-grained substratum could potentially influence ice sheet behaviour and provides a broader look on the factors controlling the dynamics of the Pleistocene ice sheets, which soft-sediment substrata in many areas were texturally varied." @default.
• W2520993003 created "2016-09-23" @default.
• W2520993003 creator A5039071642 @default.
• W2520993003 date "2016-11-01" @default.
• W2520993003 modified "2023-10-18" @default.
• W2520993003 title "Subglacial conditions and Scandinavian Ice Sheet dynamics at the coarse-grained substratum of the fore-mountain area of southern Poland" @default.
• W2520993003 cites W121244430 @default.
• W2520993003 cites W132347153 @default.
• W2520993003 cites W1522186808 @default.
• W2520993003 cites W1556203767 @default.
• W2520993003 cites W1600515466 @default.
• W2520993003 cites W1612762442 @default.
• W2520993003 cites W1619617882 @default.
• W2520993003 cites W1630188976 @default.
• W2520993003 cites W1660495403 @default.
• W2520993003 cites W1870533145 @default.
• W2520993003 cites W1883154844 @default.
• W2520993003 cites W1904042138 @default.
• W2520993003 cites W1970597197 @default.
• W2520993003 cites W1974326113 @default.
• W2520993003 cites W1976675890 @default.
• W2520993003 cites W1977786326 @default.
• W2520993003 cites W1979006925 @default.
• W2520993003 cites W1980365882 @default.
• W2520993003 cites W1981604370 @default.
• W2520993003 cites W1983792157 @default.
• W2520993003 cites W1984452272 @default.
• W2520993003 cites W1988527752 @default.
• W2520993003 cites W1994271374 @default.
• W2520993003 cites W1997520134 @default.
• W2520993003 cites W1999702711 @default.
• W2520993003 cites W2003874045 @default.
• W2520993003 cites W2007533608 @default.
• W2520993003 cites W2011695108 @default.
• W2520993003 cites W2013682417 @default.
• W2520993003 cites W2015424851 @default.
• W2520993003 cites W2017514145 @default.
• W2520993003 cites W2021525755 @default.
• W2520993003 cites W2033886099 @default.
• W2520993003 cites W2035313077 @default.
• W2520993003 cites W2040498090 @default.
• W2520993003 cites W2042374358 @default.
• W2520993003 cites W2044219104 @default.
• W2520993003 cites W2044583965 @default.
• W2520993003 cites W2051124928 @default.
• W2520993003 cites W2051675253 @default.
• W2520993003 cites W2052231919 @default.
• W2520993003 cites W2052864504 @default.
• W2520993003 cites W2053475447 @default.
• W2520993003 cites W2053504232 @default.
• W2520993003 cites W2057737727 @default.
• W2520993003 cites W2058218337 @default.
• W2520993003 cites W2059473970 @default.
• W2520993003 cites W2063325308 @default.
• W2520993003 cites W2067811381 @default.
• W2520993003 cites W2069017248 @default.
• W2520993003 cites W2069816847 @default.
• W2520993003 cites W2071896927 @default.
• W2520993003 cites W2074836634 @default.
• W2520993003 cites W2075081175 @default.
• W2520993003 cites W2078246871 @default.
• W2520993003 cites W2078847369 @default.
• W2520993003 cites W2078856206 @default.
• W2520993003 cites W2080026324 @default.
• W2520993003 cites W2089905167 @default.
• W2520993003 cites W2090278680 @default.
• W2520993003 cites W2099614110 @default.
• W2520993003 cites W2101933158 @default.
• W2520993003 cites W2105314640 @default.
• W2520993003 cites W2123638428 @default.
• W2520993003 cites W2124832369 @default.
• W2520993003 cites W2130971273 @default.
• W2520993003 cites W2141736893 @default.
• W2520993003 cites W2145171295 @default.
• W2520993003 cites W2159712690 @default.
• W2520993003 cites W222785670 @default.
• W2520993003 cites W2328415063 @default.
• W2520993003 cites W4236983686 @default.
• W2520993003 cites W4237639194 @default.
• W2520993003 cites W4250867144 @default.
• W2520993003 cites W44903260 @default.
• W2520993003 cites W783424952 @default.
• W2520993003 doi "https://doi.org/10.1016/j.quascirev.2016.09.002" @default.
• W2520993003 hasPublicationYear "2016" @default.
• W2520993003 type Work @default.
• W2520993003 sameAs 2520993003 @default.
• W2520993003 citedByCount "11" @default.
• W2520993003 countsByYear W25209930032017 @default.
• W2520993003 countsByYear W25209930032018 @default.
• W2520993003 countsByYear W25209930032019 @default.
• W2520993003 countsByYear W25209930032020 @default.
• W2520993003 countsByYear W25209930032021 @default.
• W2520993003 countsByYear W25209930032022 @default.
• W2520993003 crossrefType "journal-article" @default.
• W2520993003 hasAuthorship W2520993003A5039071642 @default.
• W2520993003 hasConcept C100834320 @default.
• W2520993003 hasConcept C111368507 @default.
• W2520993003 hasConcept C114793014 @default.

• next