Effect of fluid viscosity on fault reactivation and co‐seismic weakening

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Fluids are pervasive in the Earth's crust and saturate fractures and faults. The combination of fluids and gouge layers developing along faults can generate fluids of different viscosities. Such viscous fluids were found to influence the reactivation, fric ...

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Effect of fluid viscosity on fault reactivation and co‐seismic weakening

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