Mapping earthquake temperature rise along faults to understand fault structure and mechanics
Recent advances in the use of thermal proxies provide a window into how faults slip during earthquakes. Faults have a similar large-scale structure with a fault core, where earthquakes nucleate, and a surrounding damage zone, but complexities in fault zone architecture and rheology influence earthqu...
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| Language: | English |
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2021
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| Online Access: | https://doi.org/10.7916/d8-0nzw-z090 |