Emily A. Haugen
Utah State University, Logan, UT
Activity
2016
-
IS THE TRINITY OPHIOLITE A PIECE OF HYPEREXTENDED CONTINENTAL MARGIN?
T293 Earth History in the Broadest Context—Ophiolites, Global Tectonics, and Public Awareness of Earth Science I: Celebrating the Contributions of Eldridge MooresWednesday, 28 September 20168:00 AM - 12:00 PMRoom 203
-
GEOCHEMICAL MODELING OF BONINITE AND FAB FROM IODP EXPEDITION 352, IZU-BONIN FOREARC
T205 Records of Subduction Initiation in Modern and Ancient SettingsTuesday, 27 September 20168:00 AM - 12:00 PMMile High Ballroom 2C
-
CHEMOSTRATIGRAPHY OF SUBDUCTION INITIATION: IODP EXPEDITION 352 BONINITE AND FAB
T205 Records of Subduction Initiation in Modern and Ancient SettingsTuesday, 27 September 20168:00 AM - 12:00 PMMile High Ballroom 2C
2015
-
NEW AGES AND TECTONIC HISTORY FOR THE TRINITY TERRANE, A POLYGENETIC OPHIOLITIC COMPLEX, KLAMATH MOUNTAINS, CALIFORNIA
18 Terrane Accretion and Translation in the CordilleraWednesday, 13 May 20158:00 AM - 12:00 PMRoom 116
2014
-
AGE AND ORIGIN OF LEUCOCRATIC ROCKS OF THE NEOPROTEROZOIC TRINITY OPHIOLITE, KLAMATH MOUNTAINS, CALIFORNIA
T209 Ridge to Trench Evolution of Oceanic Lithosphere and Its Accretion Tectonics in the Pacific Rim (Past and Present) (Posters)Tuesday, 21 October 20149:00 AM - 6:30 PMExhibition Hall C
-
POSSIBLE DETACHMENT FAULT PRESERVED IN THE NEOPROTEROZOIC TRINITY OPHIOLITE, KLAMATH MOUNTAINS, CALIFORNIA
T209 Ridge to Trench Evolution of Oceanic Lithosphere and Its Accretion Tectonics in the Pacific Rim (Past and Present) (Posters)Tuesday, 21 October 20149:00 AM - 6:30 PMExhibition Hall C