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Jason Phipps-Morgan has had a profound scientific career, marked by an enduring curiosity about the workings of the Earth, particularly the dynamics of deformation, melting, and phase transformations across various geological scenarios. His research encompasses mantle flow, melting, melt migration at ridges, hotspots, arcs, hydrothermal flow reactions at ridges and trenches, and fluid flow reactions related to carbon sequestration in terrestrial subseafloor environments. Since the mid-1990s, he has been involved in geodynamic models linked to mid-ocean ridge processes and the genesis of oceanic crust within the uppermost mantle. His work, which includes gathering new observations using marine geophysical techniques, has taken him on numerous deepwater research expeditions. In the 2000s, Phipps-Morgan focused on subduction zone dynamics, particularly the processes associated with plate bending and the formation of subduction channels, which are crucial for large earthquake generation. Over the past five years, he has contributed significantly to the development of a parallel-computing toolbox for modeling complex 3D Earth systems that involve non-linear interactions in deformation and fluid flow. His research has paved the way for creating customizable code-tools in parallel computing, particularly using MATLAB/MPI, to further explore the dynamic processes of our planet.
Department of Architecture