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Fault lubrication and earthquake propagation in carbonate rocks. (2011)
Book Chapter
De Paola, N., Hirose, T., Mitchell, T., Di Toro, G., Viti, C., & Shimamoto, T. (2011). Fault lubrication and earthquake propagation in carbonate rocks. In R. I. Borja (Ed.), Multiscale and Multiphysics Processes in Geomechanics: Results of the Workshop on Multiscale and Multiphysics Processes in Geomechanics, Stanford, June 23–25, 2010 (153-156). Springer Verlag. https://doi.org/10.1007/978-3-642-19630-0_39

Friction experiments performed on dolomite/calcite at conditions typical during the propagation of large earthquakes (slip velocities v > 1 m/s and displacements d > 1 m) show that the frictional strength of experimental faults decays exponentially f... Read More about Fault lubrication and earthquake propagation in carbonate rocks..

Fault weakening due to CO2 degassing in the Northern Apennines: short- and long-term processes (2008)
Book Chapter
Collettini, C., Cardellini, C., Chiodini, G., De Paola, N., Holdsworth, R., & Smith, S. (2008). Fault weakening due to CO2 degassing in the Northern Apennines: short- and long-term processes. In C. Wibberley, W. Kurz, J. Imber, R. Holdsworth, & C. Collettini (Eds.), The Internal Structure of Fault Zones: Implications for Mechanical and Fluid-Flow Properties (1-20). The Geological Society. https://doi.org/10.1144/sp299.10

Abstract: The influx of fluids into fault zones can trigger two main types of weakening process that operate over different timescales and facilitate fault movement and earthquake nucleation. Short- and long-term weakening mechanisms along faults req... Read More about Fault weakening due to CO2 degassing in the Northern Apennines: short- and long-term processes.