Abstract

Compares the overthrust structure in the border zone of the Jura mountains in the Bresse region, France, with nappe structures in the Mediterranean region (nappes of the Riff and Tell regions of north Africa and of Tuscany, Italy). There are numerous similarities in style and age, but the mechanism was not exactly the same in all cases.

First Page Preview

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