Stress anomalies can be temporal or spatial, but a temporal stress perturbation is needed if the rupture occurs over the same patch (e.g., in the case of true anti-repeaters). Most of these models concern volcanic and induced seismicity, driven by geophysical processes involving deformation, ...
but a temporal stress perturbation is needed if the rupture occurs over the same patch (e.g., in the case of true anti-repeaters). Most of these models concern volcanic and
To address the main question – how to keep the sediment surface close to sea-level across the entire basin during rifting – it is necessary to generate a source of buoyancy proportional to the degree of stretching. Subsequently, the buoyancy needs to be lost over a short period of time fo...