Geodynamic modelling helps us understand Earth’s internal processes by providing a framework to test hypotheses. Analogue modelling uses physical models governed by the laws of nature, with resolution down to Planck’s length. In contrast, numerical modelling employs mathematical methods to approximate solutions to the physical laws governing Earth’s processes. Each modelling approach comes with it ...[Read More]
Coexisting Forces in Geodynamic Modelling: Pros, Cons, and Synergies of Analogue and Numerical Modelling
3D mantle flow imaged using the stereoscopic PIV technique in analogue models of slab rollover subduction (a, b) and slab rollback subduction (c, d). Adapted from Strak, Xue & Schellart (2024).