Abstract Convergence of the Indian Plate towards Eurasia has led to the building of the
Himalaya, the highest mountain range on Earth. Active mountain building involves a …

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 …

Abstract The September 2018, M_w M w 7.5 Sulawesi earthquake occurring on the Palu-
Koro strike-slip fault system was followed by an unexpected localized tsunami. We show that …

Large prehistoric rockslides tend to occur within spatio-temporal clusters suggesting a
common trigger such as earthquake shaking or enhanced wet periods. Yet, trigger …

There is increasing evidence that the Himalayan seismicity can be bimodal: blind
earthquakes (up to Mw~ 7.8) tend to cluster in the downdip part of the seismogenic zone …

Dynamic modeling of sequences of earthquakes and aseismic slip (SEAS) provides a self‐
consistent, physics‐based framework to connect, interpret, and predict diverse geophysical …

Orogenic wedges commonly display an inner wedge, where crystalline units have been
exhumed, and an outer wedge formed by imbricated sedimentary units detached from the …

A major goal in earthquake physics is to derive a constitutive framework for fault slip that
captures the dependence of shear strength on fault rheology, sliding velocity, and pore-fluid …

Slip accommodation in subduction zones ranges from aseismic slip phenomena to regular
megathrust earthquakes, and strongly depends on pore fluid pressure. We develop a new …