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N. Brantut

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Open access Jul 2026

Pore pressure change during nucleation and slip along experimental faults

In order to clarify the main controlling factors influencing fluid pressure changes in fault zones during the seismic cycle, we conducted laboratory rock friction experiments where fluid pressure was monitored in situ during sequences of quasi-static loading followed by dynamic slip events. The simulated fault was a 30...

N. Brantut, F. Passelegue, P. Dublanchet · 0 citations
Open access Jul 2026

Propagation of fluid-driven aseismic slip fronts under upper crustal conditions

Fracture mechanics models suggest that aseismic slip may either lag behind or outpace the fluid pressure front, depending on injection conditions and the fault’s initial stress state. However, direct experimental validation of these predictions has been lacking. Here, we report laboratory experiments on granite samples...

F. Passelègue, N. Brantut, H. Chauris et al. · 0 citations

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