All Outputs (3)

Coseismic ultramylonites: An investigation of nanoscale viscous flow and fault weakening during seismic slip (2019)
Journal Article
Pozzi, G., De Paola, N., Holdsworth, R. E., Bowen, L., Nielsen, S. B., & Dempsey, E. D. (2019). Coseismic ultramylonites: An investigation of nanoscale viscous flow and fault weakening during seismic slip. Earth and Planetary Science Letters, 516, 164-175. https://doi.org/10.1016/j.epsl.2019.03.042

Faults weaken during the propagation of earthquakes due to the onset of thermally-activated mechanisms, which vary depending on the rock type. Recent experimental work suggests that carbonate-hosted faults are lubricated by viscous flow in nano-granu... Read More about Coseismic ultramylonites: An investigation of nanoscale viscous flow and fault weakening during seismic slip.

A new interpretation for the nature and significance of mirror-like surfaces in experimental carbonate-hosted seismic faults (2018)
Journal Article
Pozzi, G., De Paola, N., Nielsen, S., Holdsworth, R., & Bowen, L. (2018). A new interpretation for the nature and significance of mirror-like surfaces in experimental carbonate-hosted seismic faults. Geology, 46(7), 583-586. https://doi.org/10.1130/g40197.1

Highly reflective, continuous smooth surfaces, known as "mirror-like surfaces" (MSs), have been observed in experimental carbonate-hosted faults, which were sheared at both seismic and aseismic velocities. MSs produced during high-velocity friction e... Read More about A new interpretation for the nature and significance of mirror-like surfaces in experimental carbonate-hosted seismic faults.

Tertiary pegmatite dikes of the Central Alps (2014)
Journal Article
Guastoni, A., Pennacchioni, G., Pozzi, G., Fioretti, A., & Walter, J. (2014). Tertiary pegmatite dikes of the Central Alps. The Canadian Mineralogist, 52(2), 191-219. https://doi.org/10.3749/canmin.52.2.191

The largest field of Alpine Oligocene pegmatite dikes is in the Central Alps within the Southern Steep Belt (SSB) of the Alpine nappes; it extends for about 100 km in an E–W direction and 15 km in a N–S direction north of the Periadriatic Fault, from... Read More about Tertiary pegmatite dikes of the Central Alps.