During the past five decades, numerical modeling of subduction, one of the most
challenging and captivating geodynamic processes, remained in the core of geodynamic …

This hands-on introduction to numerical geodynamic modelling provides a solid grounding
in the necessary mathematical theory and techniques, including continuum mechanics and …

Understanding the interactions between surface and deep Earth processes is important for
research in many diverse scientific areas including climate, environment, energy …

Although many different mechanisms for subduction initiation have been proposed, only few
of them are viable in terms of consistency with observations and reproducibility in numerical …

It is well documented that the interplay between crustal thickening and surface processes
determines growth of continent‐continent collision orogens from small and cold to large and …

Geodynamic modelling provides a powerful tool to investigate processes in the Earth's crust,
mantle, and core that are not directly observable. However, numerical models are inherently …

Subsidence and uplift patterns and thermal history of sedimentary basins are controlled by
tectonics, mantle dynamics and surface processes, such as erosion, sediment transport and …

Established theories ascribe much of the observed long‐term Cenozoic climate cooling to
atmospheric carbon consumption by erosion and weathering of tectonically uplifted terrains …

The horizontal propagation of slab detachment (slab tearing) is known to control lateral
migration of the mountain uplift along the collisional belt. However, along‐strike differential …

Surface processes and magmatism condition the structural evolution of continental rifts and
passive margins through mechanical and thermal effects on the lithosphere rheology …