Abstract
The Cap Bon peninsula is crossed by major tectonic accidents which limit the ditchs of Grombalia, Sidi Daoud and Korba. Among these accidents the Aïn Oktor's faults operate in the marin quaternary deposits of Tunis gulf as senestrial strike slip faults. The distribution of seisms and thermal springs confirms the actuel sismotectonic working of Cap Bon's grabens.
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