Solid Earth Dynamics

The Large Low Shear Velocity Provinces

What is the present-day physical and chemical state of the solid Earth? How did it dynamically evolve over geological time, leaving behind the geological, geophysical and geochemical signatures across the globe?

My research on solid Earth dynamics focuses on the following aspects:

An estimate of the global hotspot potential temperature, from Bao et al. (2022)

Rising lab plumes imaged by bubbles from a rigid half sphere, representing an end-member scenario of the Large Low Shear Velocity Province.

Mantle rocks deform like viscous fluid over geological time-scales.