Shallow Rupture Propagation of Pleistocene Earthquakes Along the Hurricane Fault, UT, Revealed by Hematite (U‐Th)/He Thermochronometry and Textures
Author:
Affiliation:
1. Department of Geosciences Utah State University Logan UT USA
2. Department of Geoscience University of Nevada, Las Vegas Las Vegas NV USA
Funder
National Science Foundation
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL094379
Reference66 articles.
1. Hydrothermal growth mechanism of α-Fe2O3 nanorods derived by near in situ analysis
2. Geometry of seismically active faults and crustal deformation within the Basin and Range-Colorado Plateau transition in Utah
3. Production of nanoparticles during experimental deformation of smectite and implications for seismic slip
4. Hematite fault rock thermochronometry and textures inform fault zone processes;Ault A. K.;Journal of Structural Geology,2020
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1. A closer look into slickensides: Deformation on and under fault surfaces;Journal of Structural Geology;2023-06
2. Hematite accommodated shallow, transient Pleistocene slow slip in the exhumed southern San Andreas fault system, California, USA;Geology;2022-10-20
3. Investigation of quartz luminescence properties in bedrock faults: Fault slip processes reduce trap depths, lifetimes, and sensitivity;Radiation Measurements;2022-07
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