Most existing constraints on mantle flow or the dynamic pressure that drives this flow are either sparse or indirect. This study focuses on assessin...

Mantle plumes are structures associated with diapiric upwelling into the asthenosphere, requiring concomitant flow beneath the lithosphere away from t...

The nature of the collision events involved in the Himalayan orogeny offers insight into the role of convergent margins in plate reconfigurations, glo...