Abstract
The Ouenza carbonate platform is a decakilometric sedimentary system surrounded by marly formations, which have been acting during the main part of the Gargasian and have been interrupted at Clansayesian. The platform is made of an outer coral facies zone and an inner Rudist facies one. A triasic diapirism had initiated the platform statement, the main history of which is also determined by diapiric activity probably controled by the reactivation of an hercynian fault.
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