Abstract
Abstract Concludes that the Cretaceous of the Bigorre region, France, is composed of a continuous series ranging from lower Cretaceous Aptian strata to upper Cretaceous Flysch deposits and that Cretaceous breccias of the region are not tectonic in origin but were formed at several different times by deposition of detrital material derived from pre-Cretaceous masses, which were present as topographic highs in the depositional basin.
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