GD
Geodynamics

Wit & Wisdom

Dislocation Creep and the Development of Deformation Fabrics

Dislocation Creep and the Development of Deformation Fabrics

Assume you are under stress. What do you do? Take a walk in the park, order your favorite takeout, have a breakdown, or internally slip along preferred slip systems and develop a fabric? The response will mostly depend on what kind of material you are, how much stress you are under, and what environmental conditions you are subjected to. For instance, someone might listen to classical music after ...[Read More]

From Rocks to Models: Reconciling Field Geology with Geodynamic Simulations

From Rocks to Models: Reconciling Field Geology with Geodynamic Simulations

When reading a scientific paper or a text explaining the physical workings of the Earth, one of the most striking aspects is the methodological approach—sometimes involving numerical models, other times fieldwork and/or rock geochemistry. This diversity of approaches can initially cause some discomfort, a feeling that things are like square pegs in round holes. How can a computer model dialogue wi ...[Read More]

Applying for a PhD in Geoscience: To do or not to do

Applying for a PhD in Geoscience: To do or not to do

Fresh out of your bachelor’s degree, or more commonly these days, your master’s degree, it can be tempting to pursue your PhD as quickly as possible. While there are compelling reasons to dive straight in, rushing into a PhD might not be your best choice.   To be or not to be a researcher? Before you start firing off applications, take a step back. Forget any expectations you had ...[Read More]

Don’t Stop Me Now: A Fracture Mechanics Perspective on Earthquake Nucleation

Schematic for a possible earthquake nucleation scenario. Inset figure adapted after Lebihain et al. (2021) and McLaskey (2019).

How do earthquakes start? Earthquakes occur when a block of rock rapidly slides past another along an interface or a discontinuity in the medium and release energy in the form of seismic waves. Turns out, the surface of the earth is riddled with a lot of these discontinuities, which we call “faults”. If we plot the locations of earthquakes on a world map (Figure 1a), we will see that they highligh ...[Read More]