It is unlikely that the Earth's mantle — the layer beneath the crust and above the core — was completely homogeneous when it initially formed. Over time, cooling-induced convection as well as ...
We apply these models to a range of problems, including faulting, mantle convection, and melting and melt migration in the Earth’s mantle, as well as to societally-relevant issues, such as the dynamic ...
over the course of long-term mantle convection, formed two prominent LLVP regions which have remained stable throughout 4.5 billion years of geological evolution. Differences in the deep mantle ...
Heat energy is conducted from the hot end of an object to the cold end. The atoms are fixed in place but are free to vibrate. When part of a solid absorbs heat energy the atoms vibrate faster and ...
My research focuses on the understanding of the present-day physical and chemical structure of the Earth's mantle and crust as well as its physical and chemical evolution over geologic time. Within ...