Wendy M. Barrow
Univ of Nevada - Las Vegas, Las Vegas, NV
Activity
2007
-
PALEOZOIC EVLOUTION OF THE CORDILLERAN CONVERGENT MARGIN: A VIEW FROM THE EASTERN KLAMATH MOUNTAINS
28 Origin and Accretionary Processes of Cordilleran Terranes: New Methods, Models and Challenges ISunday, 6 May 20078:00 AM - 12:00 PM
Date Unknown
-
LATE PALEOZOIC EXHUMATION OF SUBDUCTED OCEANIC CRUST BY EXTENSIONAL REACTIVATION OF A MID-PALEOZOIC SUBDUCTION MARGIN: CENTRAL METAMORPHIC TERRANE, KLAMATH MOUNTAINS, CALIFORNIA
171 Tectonics (Posters)
-
THE MID-PALEOZOIC TRINITY THRUST FAULT OF THE EASTERN KLAMATH MOUNTAINS, NORTHERN CALIFORNIA: REACTIVATED IN THE PERMIAN AS AN EXTENSIONAL STRUCTURE
T58 Whence the Mountains? New Developments in the Tectonic Evolution of Orogenic Belts: Celebrating the Dynamic Career of Raymond A. Price at the 50-Year Mark (Posters)