GD
Geodynamics

edited by Constanza Rodriguez Piceda

She is a postdoctoral researcher at University of Plymouth (UK). Her research interests span from the role of fault networks with complex geometries in earthquake processes to the link of the lithospheric structure with observed seismic deformation. She is co-editor-in-chief of the GD blog team.

Mathematical closed-form solutions in Geodynamics: insightful or detrimental?

Mathematical closed-form solutions in Geodynamics: insightful or detrimental?

Mathematics is certainly not every scientist’s cup of tea. Despite the latter, they are, for the most part, very important, since most problems, regardless of their complexity, start and end with a mathematical equation (or set of equations). In this week’s blog, Dimitrios Papadomarkakis (student at the National Technical University of Athens), discusses the subject of closed-form (analytical) sol ...[Read More]

Cratons: building blocks of continents and their economic importance

Cratons: building blocks of continents and their economic importance

The 4.5 billion years of geologic evolution has shaped the tectonic processes in Earth we see today. Over the span of time, Earth has changed from being a magma ocean to a tectonically active planet, by transitioning through different tectonic regimes.  A silent witness of this journey have been cratons which have survived for billions of years. Therefore cratons preserve clues of past tectonic pr ...[Read More]

The hidden effects of academic excellence: workaholism in Academia

The hidden effects of academic excellence: workaholism in Academia

Years have passed since I started my academic career, and I have come to realise that, in academia, excellence appears to come with a price tag. Stress and pressure have become commonplace for academics, often normalising certain behaviours such as workaholism. This essay explores how workaholism have become a common practice in these working environments. It was late, the library lights were blin ...[Read More]

How do rocks fail and flow: A beginners guide to rock rheology

How do rocks fail and flow: A beginners guide to rock rheology

The field of rock rheology may seem a bit ‘odd’ at first glance to those geoscientists who are vaguely familiarized with the topic of geodynamics. Often, rocks are considered massive and competent geomaterials that display a sudden (and sometimes violent) brittle failure (earthquake alert!). However, when considering the high temperatures and large timescale characteristics of most geo ...[Read More]