Today we know the Earth as a tectonically busy planet, shaped by mantle convection and plate tectonics. But this is nothing compared to the earlier phases of planetary evolution. This week, Fabio Capitanio (ARC Future Fellow and Associate Professor at the School of Earth, Atmosphere and Environment at Monash University, Australia) takes us on a …[Read More]
Paleogeography refers to the past distribution of landmasses and oceans and gives important insights into the state of previous tectonics. This is a useful cornerstone for many aspects of geodynamics and this week Boris Robert – previously postdoctoral fellow at the Centre for Earth Evolution and Dynamics Oslo (Norway) and currently visiting scientist at GFZ …[Read More]
It is the smallest planet of the Solar System, the closest to the Sun and the quickest at orbiting around it, the one with the least inclined and most elongated orbit, the only one where a day lasts two-thirds of a full year, the one with the highest bulk density. Mercury is a planet of …[Read More]
Geodynamics does not stop at the core-mantle boundary – the Earth’s outer core is a truly dynamic geosystem. This week Stefano Maffei (Research fellow) and Chris Davies (Associate Professor) from the School of Earth and Environment at the University of Leeds tell us more about the possible interplay between mantle and core and some of …[Read More]
This week Ana-Catalina Plesa, Junior Research Group Leader at the German Aerospace Centre (DLR) in Berlin/Germany takes us on a journey to Mars. Enjoy the read about how spacecraft observations and numerical models provide InSight into the deep enigmas of the “red planet”. Over the course of its evolution, Mars has accumulated heat in its …[Read More]
