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Relating high-velocity rock-friction experiments to coseismic slip in the presence of melts

2006
The dynamic strength (τ f ) of faults during coseismic slip is a major unknown in earthquake mechanics, though it has crucial influence on rupture properties, dynamic stress drop, radiated energy and heat produced during slip. In order to provide constraints on τ f , High-Velocity Rock Friction Experiments (HVRFE) are conducted on natural rocks with ...
DI TORO, GIULIO   +3 more
openaire   +2 more sources

Coseismic slip gradient at the western terminus of the 1920 Haiyuan Mw 7.9 earthquake

Journal of Structural Geology, 2021
Wenqian Yao   +2 more
exaly  

Nonlinear Response of Tunnels under Coseismic Displacement Induced by Strike-Slip Fault

International Journal of Geomechanics, 2022
Mi Zhao, Jingqi Huang
exaly  

Coseismic slip model for 2020 Ghotor earthquake based on InSAR DATA

Journal of Geomatics Science and Technology, 2023
Mahin Jafari   +2 more
openaire   +1 more source

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