No evidence of slow slip events but anomalous transients in horizontal displacement time series along the Sumatra–Andaman subduction zone
In the decades following the occurrence of the 2004 Sumatra–Andaman earthquake, the epicentral region has been enduring large-scale postseismic deformation as evident from continuous GPS measurements in the Andaman–Nicobar region. Although the contribution of postseismic deformation continues to decrease exponentially,...