Showing papers by "Smail Mostefaoui published in 2016"

TL;DR: In this paper, the authors infer that micro-fracture healing occurred at higher temperatures than the ambient temperatures of faulting (250-300°C at 0.2 GPa), for which [Ti] were inherited by the ultra-fine recrystallized aggregates that overprinted both the magmatic quartz and the healed microfractures during the high temperature transient related to frictional seismic slip.