Temporal and geochemical evolution of the Cenozoic intraplate volcanism of Zealandia
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Pacific plate slab pull and intraplate deformation in the early Cenozoic
Large tectonic plates are known to be susceptible to internal deformation, leading to a range of phenomena including intraplate volcanism. However, the space and time dependence of intraplate deformation and its relationship with changing plate boundary configurations, subducting slab geometries, and absolute plate motion is poorly understood. We utilise a buoyancy-driven Stokes flow solver, BE...
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