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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  

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

Coseismic slip and afterslip of the 2015 Mw 8.3 Illapel (Chile) earthquake determined from continuous GPS data

Geophysical Research Letters, 2016
Gonzalo Yanez   +2 more
exaly  

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