Time‐dependent heat budget of a thrust from geological records and numerical experiments
Journal of Geophysical Research: Solid Earth, 2020•Wiley Online Library
Key Points Thermometric quantification betweenfaulted and undeformed rocks are
compared with numerically calculated shearheating during thrusting Distributed cataclastic
flow of alarge shallow thrust (5‐7 km depht) produces a persistent temperature incrementof
few tens of degrees Higher and more localized temperature increase (50‐150 degrees)
requires seismic slip
compared with numerically calculated shearheating during thrusting Distributed cataclastic
flow of alarge shallow thrust (5‐7 km depht) produces a persistent temperature incrementof
few tens of degrees Higher and more localized temperature increase (50‐150 degrees)
requires seismic slip
Key Points
- Thermometric quantification betweenfaulted and undeformed rocks are compared with numerically calculated shearheating during thrusting
- Distributed cataclastic flow of alarge shallow thrust (5‐7 km depht) produces a persistent temperature incrementof few tens of degrees
- Higher and more localized temperature increase(50‐150 degrees) requires seismic slip
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