Influence of subglacial geology on the position of a West Antarctic ice stream from seismic observations
- 1 July 1998
- journal article
- Published by Springer Science and Business Media LLC in Nature
- Vol. 394 (6688), 62-65
- https://doi.org/10.1038/27889
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Stagnation of Ice Stream C, West Antarctica by water piracyGeophysical Research Letters, 1997
- Satellite imagery of the onset of streaming flow of ice streams C and D, West AntarcticaJournal of Geophysical Research: Oceans, 1996
- Ice Stream C, Antarctica, sticky spots detected by microearthquake monitoringAnnals of Glaciology, 1994
- A water-piracy hypothesis for the stagnation of Ice Stream C, AntarcticaAnnals of Glaciology, 1994
- Active volcanism beneath the West Antarctic ice sheet and implications for ice-sheet stabilityNature, 1993
- DEFORMATION OF TILL BENEATH ICE STREAM-B, WEST ANTARCTICANature, 1986
- Seismic measurements reveal a saturated porous layer beneath an active Antarctic ice streamNature, 1986
- The heat flow through oceanic and continental crust and the heat loss of the EarthReviews of Geophysics, 1980
- The West Antarctic Ice Sheet: Instability, disintegration, and initiation of Ice AgesReviews of Geophysics, 1975
- Ice Movement and Temperature Distribution in Glaciers and Ice SheetsJournal of Glaciology, 1955