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Etude stratigraphique des territoires couverts par les feuilles de Moirans-en-Montagne et de Nantua au 50.000 (super e )


, : Etude stratigraphique des territoires couverts par les feuilles de Moirans-en-Montagne et de Nantua au 50.000 (super e ). Bulletin du Service de la Carte Geologique de la France 60: 463-490

The salient point in the stratigraphy of this region is the importance and number of variations of the facies. Throughout the stratigraphic column the facies alternate and recur repeatedly. It is difficult to identify an isolated outcrop, as similar facies occur in two or three stages on different horizons. There is more conformity in the Liassic, Oxfordian, and Argovian than in other stages. These changes of facies are characteristic, for the most part, of shallow epicontinental seas swept by submarine currents and sediments in constant motion.

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