On the basis of a study of the mineral and microfaunal composition of Cretaceous sediments of the Nalzen basin, the Pech de Foix fold, and the Dreuilhe brachyanticline, a series of contiguous structures in the north Pyrenean marginal platform region in Ariege, France, the cyclic formation of terrigenous and reef deposits is discussed.

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.