Motivation & Scope: Mantle convection is the principal control on Earth's thermal and geological evolution. It is central to our understanding of the origin and evolution of tectonic deformation, the thermal and compositional evolution of the mantle and, ultimately, the evolution of Earth as a whole. Plate tectonics and volcanism are surface manifestations of mantle
Mantle convection and possible mantle plumes beneath Antarctica
Pulsing Mantle Plumes: Causes And Geological Consequences
Pangaea's breakup: the roles of mantle plumes, orogens and
Mantle plumes and their role in Earth processes
Geophysics ANU Research School of Earth Sciences
PDF) Deep Origin of Hotspots--the Mantle Plume Model
PDF) Pulsation of mantle plumes
A tree of Indo-African mantle plumes imaged by seismic tomography
Mantle plumes and mantle dynamics in the Wilson cycle
Buoyant hydrous mantle plume from the mantle transition zone
Professor Rhodri Davies ANU Research School of Earth Sciences