Fault zone hydraulic properties provide an independent estimate of coseismic fracturing at 8 km depth (Gole Larghe Fault Zone, Italian Southern Alps)

The Gole Larghe Fault Zone (GLFZ, Italian S Alps) was exhumed from c. 8 km, where it was characterized by seis- mic activity (pseudotachylytes) but also by hydrous fluid flow (alteration halos and precipitation of hydrothermal minerals in veins and cataclasites). The fault zone has previously been quantitatively characterized (Bistacchi 2011, PAGEOPH; Smith 2013, JSG) providing a rich dataset to generate 3D Discrete Fracture Network (DFN) models and simulate fault hydraulic properties. A fundamental parameter that cannot be directly evaluated in the field is the fraction of fractures-faults that were open over a certain time period in the evolution of the fault zone. Based on field and microstructural evidence, we infer that the opening and closing of fractures resulted in a toggle-switch mechanism for fluid flow during the seismic cycle: higher permeability was obtained in the syn- to post-seismic period, when the largest number of fractures was (re)opened by off-fault deformation, then permeability dropped due to fracture cementation. Postseismic permeability has been evaluated in a few cases in the world thanks to seismological evidence of fluid migration along active fault systems. Therefore, we were able to develop a parametric hydraulic model of the GLFZ and calibrate it to obtain the fraction of faults-fractures that were open in the postseismic period to obtain realistic fluid flow and permeability values. This fraction is very close to the percolation threshold of the DFN, and it can be converted to fracture intensity (fracture surface per unit volume in the fault zone), which could be integrated to obtain the fracture energy due to off-fault fracturing. Since the fracture energy due to on-fault processes has already been estimated for the GLFZ (Pittarello, 2008, EPSL), this also allows us to estimate the total fracture energy