Dynamic topography of passive continental margins and their hinterlands since the Cretaceous

Even though it is well accepted that the Earth’s surface topography has been affected by mantle-convection induced dynamic topography, its magnitude and time-dependence remain controversial.  The dynamic influence to topographic change along continental margins is particularly difficult to unravel, because their stratigraphic record is dominated by tectonic subsidence caused by rifting. We follow a three-fold … Read more…

A full-plate global reconstruction of the Neoproterozoic

Abstract Neoproterozoic tectonic geography was dominated by the formation of the supercontinent Rodinia, its break-up and the subsequent amalgamation of Gondwana. The Neoproterozoic was a tumultuous time of Earth history, with large climatic variations, the emergence of complex life and a series of continent-building orogenies of a scale not repeated until the Cenozoic. Here we … Read more…