Abstract
Mapping the spatial distribution of c-axis orientations in ice thin sections is not much more difficult than preparing c-axis scatter plots but can reveal additional information about procesess responsible for the observed fabric and texture of the ice. Distributions of angles between c-axes of neighbouring grains from the Byrd Station (West Antarctica) ice core suggest that polygonization causes average grain-size to stabilize below 400m depth. -Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 197-203 |
| Number of pages | 7 |
| Journal | Journal of Glaciology |
| Volume | 41 |
| Issue number | 137 |
| DOIs | |
| State | Published - 1995 |
All Science Journal Classification (ASJC) codes
- Earth-Surface Processes
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