Cameron A. Hughes
University of Tennessee, Knoxville, TN
Activity
2020
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EVIDENCE FOR METEORIC FLUID INFILTRATION INTO A YOUNG, ACTIVE MID-CRUSTAL SHEAR ZONE: δ2H OF MICA FISH FROM THE CORDILLERA BLANCA SHEAR ZONE, PERUVIAN ANDES
T238 Fluids in Faults—The Role of Fluid Activity, Fault-Rock Composition, and Alteration in the Earthquake CycleFriday, 30 October 202010:00 AM - 2:00 PMMeeting Rooms
2019
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MANTLE-TO-CRUST FLUID TRANSFER ABOVE THE PERUVIAN FLAT SLAB: INSIGHT FROM HELIUM ISOTOPES IN THERMAL SPRINGS OF THE PERUVIAN ANDES
T140 Present-Day and Ancient Flat-Slab Subduction in Rock Records, Geophysical Images, and Geodynamic ModelsMonday, 23 September 20191:30 PM - 5:30 PMRoom 132ABC, North Building
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HE AND CO2 FLUX FROM THE PERUVIAN FLAT SLAB ESTIMATED FROM HOT SPRING GEOCHEMISTRY
T50 Present-Day and Ancient Flat-Slab Subduction in Rock Records, Geophysical Images, and Geodynamic Models (Posters)Sunday, 22 September 20199:00 AM - 5:30 PMHall AB, North Building
2018
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CONDITIONS OF STRAIN LOCALIZATION ALONG THE CORDILLERA BLANCA SHEAR ZONE (CBSZ), PERU
13 Longstanding Problems and New Ideas About the Structure and Tectonic Evolution of the Southern Appalachians and Other Mountain Belts II: In Honor of the Career of Robert D. Hatcher Jr.Thursday, 12 April 20181:30 PM - 5:30 PMRoom 301 C
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RHEOLOGY, KINEMATICS, AND THERMAL CONDITIONS DURING SYN-CONVERGENT EXTENSION ON THE CORDILLERA BLANCA DETACHMENT, PERU
13 Longstanding Problems and New Ideas About the Structure and Tectonic Evolution of the Southern Appalachians and Other Mountain Belts II: In Honor of the Career of Robert D. Hatcher Jr.Thursday, 12 April 20181:30 PM - 5:30 PMRoom 301 C
2017
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DEFORMATION MECHANISMS RELATED TO STRAIN LOCALIZATION IN THE CORDILLERA BLANCA SHEAR ZONE (CBSZ), PERU
T386 Challenges in Tectonics: Beyond Steady State: New Developments in Understanding Strain Localization Processes and the Rheology of the Lithosphere (Posters)Wednesday, 25 October 20179:00 AM - 6:30 PMHalls 4EF
2015
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DEFORMATION DURING SYN-CONVERGENT EXTENSION ALONG THE CORDILLERA BLANCA SHEAR ZONE, PERU
T173 Strike Slip Fault Systems Transfer Stress Inboard from the Subduction Zone Margin Leading to Basin Subsidence and Orogensis, Are Conduits for Magmatism, and Are Responsible for Far-Traveled Terrane TranslationMonday, 2 November 20151:30 PM - 5:30 PMRoom 308