ASPECT

From Mountains to Oceans: How the memory of ancient orogens guides the rupture of continents

Kai Li and edited by Pauline Gayrin October 15, 2025

Picture showing an orogen that transform in a rift

Modified from François et al., 2022.

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

Ranpeng Li and edited by Arijit Chakraborty August 20, 2025

Figure 1: A schematic summary. Time evolving in a clockwise direction. The dashed line marks a depth of 500 km, and the dotted shading indicates the pressure–temperature range where the wadsleyite ⇔ garnet (majorite) + ferropericlase phase transformation occurs. Purple shading marks areas of partial melting. The timeline calculation assumes a mantle potential temperature of 1900 K at ~3 Ga, cooling by about 100 K per Gyr.

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

Ziqi Ma, edited by Yinuo Zhang and edited by Constanza Rodriguez Piceda January 8, 2025

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

Menno Fraters August 4, 2021

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]