Therefore, they conclude that the southern mantle experiences higher temperatures and lower viscosity. This is also supported by the thicker southern hemisphere crust slowing heat loss from the ...
The emerging model of mantle convection suggests that some relatively cool subducting slabs of oceanic plate (blue) are deflected at the 660 km discontinuity (dashed black line) whereas others ...
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 ...