Fault inversion contributes to ground deformation above inflating igneous sills
Magma emplacement is commonly accommodated by uplift of the overburden and free surface.By assuming this deformation is purely elastic, we can invert the shape and kinematics of ground deformation to model the geometry and dynamics of underlying intrusions.However, magma emplacement can be accommodated by viscoelastic and/or inelastic processes.We