| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6441225 | Lithos | 2011 | 16 Pages |
Abstract
⺠Diffusion in garnet indicates different hanging wall cooling histories above a thrust. ⺠Peak T may not have been contemporaneous at different structural positions. ⺠Migmatitic amphibolite records partial retrograde re-equilibration. ⺠Cooling, then decompression matches 2-D thermal modeling.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Benjamin W. Hallett, Frank S. Spear,