Abstract
Seismic experiments conducted on ice stream B, part of the marine ice sheet of West Antarctica, show a meters-thick layer immediately beneath the 1000-m thick ice. Very low wave speeds imply that the material in the layer is highly porous and is saturated with water at a high pore pressure. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 8903-8911 |
| Number of pages | 9 |
| Journal | Journal of Geophysical Research |
| Volume | 92 |
| Issue number | B9 |
| DOIs | |
| State | Published - 1987 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
-
SDG 14 Life Below Water
All Science Journal Classification (ASJC) codes
- Condensed Matter Physics
- Materials Chemistry
- Polymers and Plastics
- Physical and Theoretical Chemistry
Fingerprint
Dive into the research topics of 'Till beneath ice stream B. 1. Properties derived from seismic travel times'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver