In this new blog, Dr. Kai Li (GFZ Potsdam) talk about his PhD work, where he used accordion numerical models to explore the tectonic history of the South China Sea. His PhD research focuses on the impact of orogenic inheritance on rifts and rifted margins, employing advanced geodynamic modeling techniques. Have you ever tried to fit the west coast of Africa and the east coast of South America toge ...[Read More]
Phase transitions control plume layering during Earth’s secular cooling

Earth’s structure and dynamics have evolved quite a lot since its formation, and so has mantle dynamics and convection patterns changed along with it. It turns out that phase transition in certain mantle minerals can be an important driver of this change. Today, Ranpeng Li from GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany explains how coupling geodynamic models with thermodynami ...[Read More]
New Insights into Plume Buoyancy Fluxes and Dynamic Topography from Numerical Modelling
Figure 1. Illustration of the hotspot swell and plume buoyancy flux. White dashed line shows the original seafloor topography due to half-space cooling. Dark green line represents the surface dynamic topography caused by the dynamic uplift of the plume. One of the main surface expressions of dynamic topography are hotpot swells formed by mantle plumes. In this week’s post, Ziqi Ma, PhD candi ...[Read More]
ASPECT 2021 hackathon
Last year we introduced the ASPECT hackaton on this geodynamics blog. It was the first hackathon which went virtual which brought a whole set of new challenges. This year was the 8th version of the yearly hackathon, and it was still virtual (unfortunately). Fortunately lessons where learned from the previous virutal hackathon and generally from working more than a year online. Therefore a short bl ...[Read More]