Figure 1. Topography of the Gibraltar Arc region. The shaded area indicates the position of positive seismic velocity anomaly supposedly representing the position of the slab at 270 km depth from seismic tomography (Amaru, 2007). The purple line shows the position of the modelled cross-section for the model shown in this blog. Blue dots indicate the regional intermediate seismicity (between 40 km ...[Read More]
Reflections on the geological and geodynamic evolution of the Southern Central Andes
We live in the very heart of the Digital Age, where Artificial Intelligence (AI) is already playing a dominant role in our world. We have to ask ourselves what the future will hold for the field of Geosciences in the next years to come? In this week’s blog, our main goal is to share our views regarding the benefits and risks of AI in Geosciences. We live in an ever-evolving world, where technolo ...[Read More]
The ability to easily compile and quickly evaluate both geological and geophysical data is essential for geodynamicists to understand Earth’s evolution. This week Dr. Ben Mather, a Research Fellow at the University of Sydney, introduces us to GPlately, a new tool designed to accelerate spatio-temporal data analysis in GPlates. GPlately is a Python package that enables the reconstruction of ...[Read More]
