Claire O. Harrigan
Bowdoin College, Brunswick, ME
Activity
2023
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40AR/39AR DATING AND PALEOMAGNETIC ANALYSES OF PSEUDOTACHYLYTE REVEAL A MINIMUM OF 2.97 MILLION YEARS OF LOW-ANGLE NORMAL FAULT SEISMICITY
T242 What’s in a Fault? Fault Structure, Deformation Mechanisms, and Why Fault Zones Matter to Society: In Honor of James P. Evans (Posters)Wednesday, 18 October 20238:00 AM - 5:30 PMHall B
2022
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GUIDING CAREER EXPLORATION AND PLANNING THROUGH A CAREER COURSE FOR UNDERGRADUATE GEOSCIENCE MAJORS
T53 Career Paths and Licensure: Program Strategies to Help Students Explore Career Pathways in the Earth SciencesSunday, 9 October 20221:30 PM - 5:30 PM603
2021
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TITANITE PETROCHRONOLOGY DATES SHEAR ZONE INITIATION TO BETWEEN 99 AND 96 MA IN THE WESTERN IDAHO SHEAR ZONE
127 D32. Recent Advances in Tectonics/Tectonophysics (Posters)Monday, 11 October 20212:30 PM - 6:30 PMExhibit Hall A
2019
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TITANITE U-PB PETROCHRONOLOGY REVEALS ~26 MILLION YEARS OF DEFORMATION IN A MID-CRUSTAL HIGH-TEMPERATURE SHEAR ZONE
T217 How Old, How Long, and How Fast: Establishing the Timing, Duration, and Rates of Mid- to Lower-Crustal DeformationTuesday, 24 September 20191:30 PM - 5:30 PMRoom 229B, North Building
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EPPUR SI MUOVE: MIOCENE PSEUDOTACHYLYTE VEINS PRESERVE A RECORD OF EARTHQUAKES >M5.5 ON LOW-ANGLE NORMAL FAULTS
T168 Fossil Magnetism and Paleopoles; Tectonics, Stratigraphy, Geochronology, and Geomorphology; Geoscience Challenges and Education: A Celebration of John Geissman’s CareerTuesday, 24 September 20198:00 AM - 12:00 PMRoom 229B, North Building
2017
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FINDING STRAIN LOCALIZATION AND DATING THE ONSET OF DEFORMATION IN THE WESTERN IDAHO SHEAR ZONE USING TITANITE U-PB GEOCHRONOLOGY AND CRYSTALLOGRAPHIC VORTICITY AXIS ANALYSIS
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
2016
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ZIRCON AND TITANITE PETROCHRONOLOGY OF DEFORMED AND NON-DEFORMED PAYETTE RIVER TONALITE NORTH OF MCCALL, ID: IMPLICATIONS FOR THE TIMING OF HIGH TEMPERATURE DEFORMATION IN THE WESTERN IDAHO SHEAR ZONE
34 Geologic Evolution of Accretion-Related Orogenic Belts and Associated Elements of the Central North American CordilleraThursday, 19 May 20161:00 PM - 3:00 PMHorizon/Aurora Rooms