Bringing Faults to the Lab: 3D Printing Natural Faults for Rock Friction Experiments
Julia Baumgarte, McGill University

Bridge Zones and Stress Amplification: How Rocks Start to Deform
He Feng, University of Maine

Exhumation of the Pelona-Orocopia-Rand and related schist
Alan Chapman, Macalester College

Ductile and Brittle Fault Rocks in the Upper and Lower Crust, Respectively.
Robert Wintsch, Indiana University-Bloomington

The anatomy of a shear zone: Evidence for constrictional deformation and crustal thickening within the Nevadan-age Condrey Mountain Shear Zone
Katie Gates, Texas Tech University

Three Proterozic metamorphic episodes and 1.70-1.67 Ga age of the Uncompahgre quartzite resolved by in-situ monazite and xenotime petrochronology, Needle Mountains, Colorado

Strain Localization Mechanisms and Damage Zone Microstructures Across the Brittle-Ductile Transition: A Case Study of the Kellyland Fault Zone
Walter (Bill) Sullivan, Colby College

Velocity influence on restraining bend evolution
Hanna Elston, University of Massachusetts-Amherst

A Global Compilation of Olivine and Orthopyroxene Crystallographic Preferred Orientations and Their Relationship to Deformation Conditions in the Lithospheric Mantle
Rachel Bernard, Amherst College

Paleostress Analysis of Normal faults and Early Cretaceous Sheet Intrusions in Northern New England: Evidence for a Dynamic Extensional Setting During the Early Cretaceous
Jennifer Cooper Boemmels, Southern Connecticut State University