Abstract
Steady-state creep-rates of polycrystalline ice were investigated as a function of temperature, grain-size, and inclusion concentration through uniaxial compression in the laboratory. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | l79-l94 |
| Journal | Journal of Glaciology |
| Volume | 24 |
| Issue number | 90 |
| DOIs | |
| State | Published - 1979 |
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