Titlebook: Rock Physics and Natural Hazards; Sergio Vinciguerra,Yves Bernabé Book 2009 Birkhäuser Basel 2009 Earthquake.fault.mechanical properties o

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Rosolino Cirrincione,Eugenio Fazio,Patrizia Fiannacca,Gaetano Ortolano,Rosalda Punturo

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Jeremie Dautriat,Nicolas Gland,Jean Guelard,Alexandre Dimanov,Jean L. Raphanel

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Microstructural Investigation of Naturally Deformed Leucogneiss from an Alpine Shear Zone (Southernled a correlation between finite strain and textural features: As strain increases, the matrix develops at the expense of the clast counterpart, which is instead progressively reduced in both size and amount.

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2504-3625 of research in this area: laboratory experiments, theoretica.Natural hazards events such as earthquakes or volcanic eruptions involve activation of coupled thermo-hydro-chemo-mechanical processes in rocks. ..The present book assembles unpublished contributions to the 7th Euro-Conference on Rock Phys

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What Does Control Earthquake Ruptures and Dynamic Faulting? A Review of Different Competing Mechaniisms, potentially concurrent and interacting. Recent laboratory experiments and geological field observations of natural faults revealed the presence, and sometime the coexistence, of thermally activated processes (such as thermal pressurization of pore fluids, melting of gouge and rocks, material p

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Quake Catalogs from an Optical Monitoring of an Interfacial Crack Propagation, fracture front dynamics is governed by local and irregular avalanches with large velocity fluctuations. Events defined as high velocity bursts are ranked in catalogs with analogoas characteristics to seismicity catalogs: time of occurence, epicenter location and energy parameter (moment). Despite d