  The burgeoning need to sequester anthropogenic CO$_2$ for climate mitigation
and the need for energy sustenance leading upto enhanced geothermal energy
production has made it incredibly critical to study potential earthquakes due
to fluid activity in the subsurface. These earthquakes result from reactivation
of 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 leading
upto quantifying the earthquake magnitude.
