Abstract

Study of the eastward prolongation of the Villagrains-Landiras fold in the Garonne basin, France, throws light on the precise dating of some of the last movements of the Pyrenean orogeny. Not a very pronounced structure, it nevertheless has determined the course of the Garonne in the region and has influenced Miocene sedimentation in this part of the Aquitaine basin.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.