T386 Challenges in Tectonics: Beyond Steady State: New Developments in Understanding Strain Localization Processes and the Rheology of the Lithosphere (Posters)
Wednesday, 25 October 2017
9:00 AM - 6:30 PM
Halls 4EF
DEFORMATION MECHANISMS RELATED TO STRAIN LOCALIZATION IN THE CORDILLERA BLANCA SHEAR ZONE (CBSZ), PERU
Paper number: T386-10
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
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Micah JessupUniversity of Tennessee, Knoxville, TN
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Colin ShawMontana State University, Bozeman, MT
Abstract
A general relationship of increasing differential stress with decreasing temperature is observed, with recorded stresses ranging from ~15 to ~90 MPa and temperatures from <280 °C to > 600°C. Quartz CPOs dominantly record prism <a> slip with varying contributions of rhomb <a> or basal <a> slip. Two samples record prism [c] slip. Temperatures recorded by asymmetric strain-induced myrmekite are consistent with those suggested by CPOs. Quartz bulging recrystallization and cataclastic microstructures record low temperature and/or high strain-rate ductile and brittle deformation. In summary, our results show evidence for dominantly moderate- to high-temperature deformation as well as lower temperature and/or high strain-rate ductile deformation and brittle processes in the CBSZ.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-307203
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