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The burgeoning need to sequester anthropogenic CO$_2$ for climate mitigationand the need for energy sustenance leading upto enhanced geothermal energyproduction has made it incredibly critical to study potential earthquakes dueto fluid activity in the subsurface. These earthquakes result from reactivationof faults in the subsurface due to pore pressure perturbations. In this work,we provide a framework to model fault slip due to pore pressure change leadingupto quantifying the earthquake magnitude.

A fault slip model to study earthquakes due to pore pressure perturbations