Origin and development of textures and fabrics in basal ice at Summit, Central Greenland
- 31 July 1994
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 125 (1-4) , 421-437
- https://doi.org/10.1016/0012-821x(94)90230-5
Abstract
No abstract availableKeywords
This publication has 25 references indexed in Scilit:
- Stable isotopes in the basal silty ice preserved in the Greenland Ice Sheet at summit; environmental implicationsGeophysical Research Letters, 1994
- Debris entrainment at the ice-bedrock interface in sub-freezing temperature conditions (Terre Adélie, Antarctica)Journal of Glaciology, 1993
- Flow-law hypotheses for ice-sheet modelingJournal of Glaciology, 1992
- Why ice-age ice is sometimes “soft”Cold Regions Science and Technology, 1991
- On the Special Rheological Properties of Ancient Microparticle-Laden Northern Hemisphere Ice as Derived from Bore-Hole and Core MeasurementsJournal of Glaciology, 1986
- Grain Growth in Polar Ice: II. ApplicationJournal of Glaciology, 1986
- Grain Growth in Polar Ice: I. TheoryJournal of Glaciology, 1986
- The Debris-Laden Ice at the Bottom of the Greenland Ice SheetJournal of Glaciology, 1979
- On the Origin of Stratified Debris in Ice Cores from the Bottom of the Antarctic Ice SheetJournal of Glaciology, 1979
- Ein Cluster-Verfahren zur richtungsstatistischen Analyse tektonischer DatenInternational Journal of Earth Sciences, 1978