When in extension, the Earth's crust accommodates deformation by breaking. Through time, faults grow into an intricate network that can be detected by changes in topography, or through modelling (numerical or analogue). This study demonstrates how the Python library Fatbox, the fault analysis toolbox, can extract the network pattern automatically from said datasets and characterise the geometry and kinematics of the fault network.

We introduce SEITCOM-1D, a new open-source software that connects the physical and chemical structure of the Earth’s crust and mantle with seismic observations. This relationship is often difficult to model, but SEITCOM-1D simplifies the process using geophysical and thermodynamic principles. It allows scientists to explore how variations in temperature and composition influence surface wave dispersion and receiver functions, helping to interpret what seismic data reveals about Earth's interior.

Transition zone between the Precambrian East European Craton and the Palaeozoic Platform, by integrating seismic interpretation with two-dimensional gravity and magnetic modelling. The combined data provide new insights into the complex tectonic evolution of the region.