Frictional and transport properties of faults zones in the Opalinus Clay formation

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Surface roughness ubiquitously prevails in natural faults across various length scales. Despite extensive studies highlighting the important role of fault geometry in the dynamics of tectonic earthquakes, whether and how fault roughness affects fluid-induc ...

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Opalinus Clay is a fine-grained sedimentary geomaterial with a mineral composition consisting mainly of silicates, carbonates and quartz. Due to its favourable barrier properties, this geomaterial has been selected as the host rock for the underground disp ...

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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 ...

Near-surface disposal of radioactive waste in shales is a promising option to safeguard the population and environment. However, natural faults intersecting these geological formations can potentially affect the long-term isolation of the repositories. Thi ...

The seismic history of the Mosha fault, the largest and most active fault of Eastern Tehran metropolis, and its relation to the Damavand active volcano, the highest mountain in the Middle East, is investigated. We deduce that the central Mosha, near the Da ...

Frictional and transport properties of faults zones in the Opalinus Clay formation

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Hydro-Mechanical Characterization of a Shale by Unusually High-Pressure Oedometric Tests

Thermo-hydro-mechanical analysis of the complete lifetime of the bentonite barrier in the FEBEX in-situ test

Fluid flow through microcracked and fractured granitic reservoirs

Shear strength and shear stiffness analysis of compacted Wyoming-type bentonite

Experimental and Numerical Investigation on Water Exchange of Opalinus Clay Samples

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Diffusion timescale conundrum in contact metamorphism: Oxygen isotope and trace element profiles in dolomite

Elongated hydraulic fracture emerging from layers of alternating fracture toughness

Influence of Viscous Lubricant on Nucleation and Propagation of Frictional Ruptures

Physical characterization of fault rocks within the Opalinus Clay formation

Long-term triggered seismicity on the Mosha fault by Damavand volcano, Iran: Implications on the seismic hazard of Tehran metropolis