Compressional intracontinental orogens are major zones of crustal thickening produced at
large distances from active plate boundaries. Consequently, any account of their initiation …

This paper describes selected results from over a dozen collaborative projects led by
Commonwealth Scientific and Industrial Research Organisation (CSIRO) in Australia …

Rapid tectonic uplift on the Alpine Fault, New Zealand, elevates topography, regional
geothermal gradients, and the depth to the brittle ductile transition, and drives fluid flow that …

A persistent problem in the study of garnet geochemistry is that the consideration of major
elements alone excludes a wealth of information preserved by trace elements, particularly …

Warm springs emanating from deep-reaching faults in orogenic belts with high topography
and orographic precipitation attest to circulation of meteoric water through crystalline …

Abstract The West Junggar in **njiang, western China, represents a significant gold
mineralization belt hosting over 200 gold deposits, with the Hatu gold deposit being the …

Both the sources and pathways of fluid circulation are key factors to understanding the
evolution of low-angle normal fault (LANF) systems and the distribution of mineral deposits …

Volcanoes represent one of the most critical geological settings for hazard modelling due to
their propensity to both unpredictably erupt and collapse, even in times of quiescence …

Downward flow of surface-derived water deep into the upper crust is investigated using 2-D
coupled hydrothermal numerical models. In the models, downward flow is driven by either …

The accommodation of intraplate stresses in preexisting weak regions of plate interiors is
here investigated using thin viscous sheet numerical models. The intraplate stresses are …