AttributesValues
rdf:type
Description
  • The objective of this study were Little Ice Age (LIA) to recent subglacial tills, glaciofluvial sediments of proglacial sandur, esker sediments and sediments of moraine-mound complexes of Horbyebreen polythermal valley glacier and LIA to recent sediments of lateral moraine, frontal moraine, ice-cored moraine and glaciofluvial sediments of proglacial sandur of Bertilbreen polythermal valley glacier. Fossil (probably early Holocene) subglacial and supraglacial tills and sediments of coarsegrained glaciomarginal delta of Bertilbreen have also been studied. The research focused on Old Red sandstone clasts, for which roundness, shape and striation presence have been investigated. The results from this research led to the proposal of new methodological approaches.
  • The objective of this study were Little Ice Age (LIA) to recent subglacial tills, glaciofluvial sediments of proglacial sandur, esker sediments and sediments of moraine-mound complexes of Horbyebreen polythermal valley glacier and LIA to recent sediments of lateral moraine, frontal moraine, ice-cored moraine and glaciofluvial sediments of proglacial sandur of Bertilbreen polythermal valley glacier. Fossil (probably early Holocene) subglacial and supraglacial tills and sediments of coarsegrained glaciomarginal delta of Bertilbreen have also been studied. The research focused on Old Red sandstone clasts, for which roundness, shape and striation presence have been investigated. The results from this research led to the proposal of new methodological approaches. (en)
Title
  • New methods to reconstruct clast transport history in different glacial sedimentary environments: Case study for Old Red sandstone clasts from polythermal Horbyebreen and Bertilbreen valley glaciers, Central Svalbard
  • New methods to reconstruct clast transport history in different glacial sedimentary environments: Case study for Old Red sandstone clasts from polythermal Horbyebreen and Bertilbreen valley glaciers, Central Svalbard (en)
skos:prefLabel
  • New methods to reconstruct clast transport history in different glacial sedimentary environments: Case study for Old Red sandstone clasts from polythermal Horbyebreen and Bertilbreen valley glaciers, Central Svalbard
  • New methods to reconstruct clast transport history in different glacial sedimentary environments: Case study for Old Red sandstone clasts from polythermal Horbyebreen and Bertilbreen valley glaciers, Central Svalbard (en)
skos:notation
  • RIV/00216224:14310/13:00077927!RIV15-MSM-14310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(EE2.3.30.0037), P(LM2010009), S, V
http://linked.open...iv/cisloPeriodika
  • 2
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 91629
http://linked.open...ai/riv/idVysledku
  • RIV/00216224:14310/13:00077927
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • clast striation; clast roundness; clast shape; Old Red sandstone clasts; glacial sedimentary environments; Svalbard (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [CB2462D8B3C1]
http://linked.open...i/riv/nazevZdroje
  • Czech Polar Reports
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 3
http://linked.open...iv/tvurceVysledku
  • Nývlt, Daniel
  • Procházková, Barbora
  • Flašar, Jan
  • Hanáček, Martin
  • Křenovská, Iva
  • Tóthová, Gabriela
  • Lehejček, Jiří
  • Mida, Peter
  • Stacke, Václav
  • Břežný, Michal
  • Uxa, Tomáš
issn
  • 1805-0689
number of pages
http://bibframe.org/vocab/doi
  • 10.5817/CPR2013-2-13
http://localhost/t...ganizacniJednotka
  • 14310
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