Abstract
Deformation of chalcopyrite (CuFeS2) under low-grade metamorphic
conditions within fault zones in the Mt. Lyell area of western
Tasmania (Australia) has occurred dominantly by a dislocation flow
process. Elongate grain fabrics and well-developed crystallographic
preferred orientations have developed by { 112} (110)/(20l) dislocation
glide. However, the presence of recovered dislocation substructures
indicates that dislocation climb has also been important.
conditions within fault zones in the Mt. Lyell area of western
Tasmania (Australia) has occurred dominantly by a dislocation flow
process. Elongate grain fabrics and well-developed crystallographic
preferred orientations have developed by { 112} (110)/(20l) dislocation
glide. However, the presence of recovered dislocation substructures
indicates that dislocation climb has also been important.
| Original language | English |
|---|---|
| Pages (from-to) | 490-490 |
| Number of pages | 1 |
| Journal | Journal of Structural Geology |
| Volume | 7 |
| Issue number | 3-4 |
| DOIs | |
| Publication status | Published - 1985 |
| Externally published | Yes |