Ask any question about EPFL courses, lectures, exercises, research, news, etc. or try the example questions below.
DISCLAIMER: The Graph Chatbot is not programmed to provide explicit or categorical answers to your questions. Rather, it transforms your questions into API requests that are distributed across the various IT services officially administered by EPFL. Its purpose is solely to collect and recommend relevant references to content that you can explore to help you answer your questions.
Fluid pressurisation at depth can reactivate pre-existing fractures and faults by triggering frictional slip that ranges from slow (aseismic) slip to dynamic rupture. These can occur in response to either anthropogenic fluid injection (e.g. hydraulic stimulation) or via natural occurrences (e.g. serpentine dehydration). Hydraulic stimulation, widely used in geo-energy applications, enhances rock permeability by reactivating fractures using pressurized fluid injection. Recent studies have made significant