Synchronous partial melting, deformation, and magmatism: evidence from in an exhumed Proterozoic orogen

Jamie S. F. Levine, Appalachian State University, Department of Geological and Environmental Sciences, Boone, NC, United States and Sharon Mosher, Univ Texas, Austin, TX, United States
Back to: Partial Melting During High-Grade Metamorphism: Implications for Orogenic Systems I