A
Annia K. Fayon
Researcher at University of Minnesota
Publications - 28
Citations - 903
Annia K. Fayon is an academic researcher from University of Minnesota. The author has contributed to research in topics: Thermochronology & Zircon. The author has an hindex of 14, co-authored 28 publications receiving 804 citations.
Papers
More filters
Journal ArticleDOI
Tectonic controls on metamorphism, partial melting, and intrusion: timing and duration of regional metamorphism and magmatism in the Niğde Massif, Turkey
TL;DR: In this article, an interval of melting and melting of orogenic middle crust followed by emplacement of a syn-extensional pluton during decompression and cooling are demonstrated for a metamorphic core complex in central Turkey.
Journal ArticleDOI
Metamorphism of the Central Anatolian Crystalline Complex, Turkey: influence of orogen‐normal collision vs. wrench‐dominated tectonics on P–T–t paths
TL;DR: The Central Anatolian Crystalline Complex (CACC) is a microcontinent in the Alpine-Himalayan belt as discussed by the authors, which consists of at least four tectonic blocks characterized by different P-T-t paths.
Journal ArticleDOI
Isothermal decompression, partial melting and exhumation of deep continental crust
TL;DR: In this article, the authors propose that gneiss domes are a signature of decompression and crustal melting, and are therefore fundamental structures for understanding the thermo-mechanical evolution of continental crust during orogeny.
Journal ArticleDOI
Timing of deformation and exhumation in the western Idaho shear zone, McCall, Idaho
TL;DR: The western Idaho shear zone is one of several Cretaceous high-strain zones in the Cordillera that are thought to have been associated with the northward translation and/or docking of terranes presently in British Columbia.
Journal ArticleDOI
Effects of plate convergence obliquity on timing and mechanisms of exhumation of a mid-crustal terrain, the Central Anatolian Crystalline Complex
TL;DR: Apatite fission track ages from the Central Anatolian Crystalline Complex (CACC), a microcontinent within the Turkish segment of the Alpine-Himalayan orogen, vary dramatically from north to south as mentioned in this paper.