Cari colleghi
vi invitiamo a sottomettere un riassunto alla sessione P17 del Congresso congiunto della SIMP-SGI dal titolo "Geosciences: a tool in a changing world", che si terrà a Pisa dal 4 al 6 settembre 2017.
P17. Deformation and fluid flow in the crust from migmatites to epithermal systems
G. Musumeci (UNIPI), F. Mazzarini (INGV, Pisa), G. Viola (UNIBO), P. Garofalo (UNIBO)
Fluid rock interactions strongly control the petrophysical properties and the chemical composition of rocks at all scales. Hence, they have an important role in processes such as plate tectonics and the formation of economic ore deposits. Fluid flow and migration through crustal rocks occur at all scales commonly enhancing hydration and localized deformation. We welcome contributions focusing on the mechanisms, their rates and the interplay between fluid flow, reaction, deformation and mass transport processes at all geological scales, investigated through numerical and analogue modeling, field-based research and laboratory studies.
Grazie per la vostra attenzione e arrivederci a Pisa
Cari saluti
Giovanni Musumeci
Francesco Mazzarini