This is an exciting opportunity for students with an interest in the deep Earth to become part of a large consortium of UK and international researchers funded by NERC. More...
As part of their independent research project two MSci
students, Joe Potten and Rebecca Pearce are taking part in a larger 4-year Chilean-funded project involving Tom Mitchell
(UCL), Jose Cembrano and Gonzalo Yanez ,both from Pontificia Universidad Católica de Chile. This project aims to
focus on the nature and tectono-magmatic significance of transverse crustal
structures in the Andes, with some selected case studies from the Southern
The Ainsa Deepwater Channel Project, Spanish Pyrenees
An Integrated Outcrop Study: Project Manager: Professor Kevin T. Pickering
Introduction to the Ainsa Channel System
The Ainsa Channel System, south-central Pyrenees, occurs in the oldest part of the Campodarbe Group, and it is of Upper Eocene age. The Ainsa Channel Complex is per- haps the most famous of the submarine channel outcrops within Western Europe. The Ainsa channels consist of two principal channel complexes (Ainsa I and Ainsa II) which are separated by thin- and very thin-bedded sandy turbidites and marls. The Ainsa I Channel Complex is an example of an erosional-depositional system. The Ainsa II Chan- nel Complex contains significant erosional cut-downs, with infill of essentially non- erosive sandy facies. The channel dimensions are at a seismic scale.