Continental transform faults are dominantly highly localized strike-slip shear zones
hundreds of kilometers long that accumulate tens to hundreds of kilometers of displacement …

A numerical model of the coupled processes of tectonic deformation and surface erosion in
convergent orogens is developed to investigate the nature of the interaction between these …

Published geological data on Late Quaternary offsets on the Alpine Fault, New Zealand,
have been assembled into a common format and analysed with respect to uncertainties …

The region between India and South China has evolved tectonically as an accommodation
zone during postcollisional intracontinental deformation between the Indian and Eurasian …

In order to understand how orogens “work,” a quantitative approach demonstrating proof of
concept is essential. Our goal is to reconcile the diverse array of tectonic features observed …

Geodynamical numerical modeling has been combined with crustal structural restoration of
the central Pyrenees in order to gain insight into fundamental processes that control the …

Topographic relief, strain partitioning and crust‐mantle coupling within convergent orogens
may be systematically related to the distribution of strength as a function of depth within …

The large scale structure of the earth is caused by geodynamic processes which are
explained using energetic, kinematic and dynamic descriptions. While" geodynamic …

Crustal-scale channel flow numerical models support recent interpretations of Himalayan-
Tibetan tectonics proposing that gravitationally driven channel flows of low-viscosity, melt …

To advance our understanding of the kinematics of the Xuefengshan tectonic belt (XFSTB)
and the Mesozoic tectonics of the South China Block (SCB), this paper presents new data …