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. From Bao (2024a)

Seven ways scientists have pictured the deep mantle beneath East Africa and the Indian Ocean, from a single giant plume to many separate sources. Our map tests these ideas against both seismic images and lava chemistry. From Bao et al. (2026)

The many forms of MgSiO3, the most abundant mineral in Earth’s mantle, across pressure and temperature. Each box shows how magnesium (orange), silicon (blue) and oxygen (red) are arranged in a crystal, or in the liquid at the top. From Acquadro et al. (2026)

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