In this work, we would like to better constrain the rheological structure and properties near the transition portion of the upper mantle in subduction zones. We used three-dimensional viscoelastic finite element models to study the postseismic deformation of the 2013 Mw8.3 Okhotsk earthquake.
Research member: Yan Hu
Collaborators: Nikolay Shestakov, Roland Bürgmann
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