| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6440685 | Lithos | 2015 | 13 Pages |
Abstract
The rapid tectonic and temperature evolution of the Fosdick Mountains dome lends support to recently developed numerical models of crustal flow and cooling in orogenic crust undergoing extension/transtension, and accords with numerous studies of migmatite-cored gneiss domes in transcurrent settings.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
R.R. McFadden, C. Teyssier, C.S. Siddoway, M.A. Cosca, C.M. Fanning,