Postseismic uplift of the Andes following the 2010 Maule earthquake: Implications for mantle rheology
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DOI: 10.1002/2016gl071995
Abstract: Postseismic surface deformation associated with great subduction earthquakes is controlled by asthenosphere rheology, frictional properties of the fault, and structural complexity. Here by modeling GPS displacements in the 6 years following the 2010Mw 8.8 Maule… read more here.
Keywords: viscosity; maule earthquake; rheology; postseismic uplift ... See more keywords