Seismic measurements reveal a saturated porous layer beneath an active Antarctic ice stream
- 1 July 1986
- journal article
- letter
- Published by Springer Science and Business Media LLC in Nature
- Vol. 322 (6074), 54-57
- https://doi.org/10.1038/322054a0
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- DEFORMATION OF TILL BENEATH ICE STREAM-B, WEST ANTARCTICANature, 1986
- Glacier Surge Mechanism: 1982-1983 Surge of Variegated Glacier, AlaskaScience, 1985
- The Importance of Pressurized Subglacial Water in Separation and Sliding at the Glacier BedJournal of Glaciology, 1983
- The Uplift of Unteraargletscher at the Beginning of the Melt Season—A Consequence of Water Storage at the Bed?Journal of Glaciology, 1983
- THE INFLUENCE OF PERMEABILITY ON COMPRESSIONAL WAVE VELOCITY IN MARINE SEDIMENTS*Geophysical Prospecting, 1982
- Subglacial Water flow Under Ice Streams and West Antarctic Ice-Sheet StabilityAnnals of Glaciology, 1982
- SOIL CONSOLIDATION BEHAVIOR ASSESSED BY SEISMIC VELOCITY MEASUREMENTS*Geophysical Prospecting, 1981
- The Effect of the Subglacial Water Pressure on the Sliding Velocity of a Glacier in an Idealized Numerical ModelJournal of Glaciology, 1981
- SOME ASPECTS OF ELASTIC WAVE PROPAGATION IN FLUID‐SATURATED POROUS SOLIDSGeophysics, 1961
- Theory of Propagation of Elastic Waves in a Fluid-Saturated Porous Solid. I. Low-Frequency RangeThe Journal of the Acoustical Society of America, 1956