| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5779569 | Earth and Planetary Science Letters | 2017 | 11 Pages |
Abstract
- Thermo-mechanical petrological models of continental collision and magmatism.
- Slab breakoff is commonly too deep to create magmatism.
- Dehydration of tip of detaching slab more likely to cause magmatism.
- Slab breakoff alone unlikely to explain post-collisional magmatism.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Rebecca Freeburn, Pierre Bouilhol, Ben Maunder, Valentina Magni, Jeroen van Hunen,