Gravity constraints on the underground structural framework and associated volcanism of the Maghrebian allochthonous domain: The Sejnene Numidian flysch, Tunisian Tell
The work proposed tectonic framework model for Numidian flysch of Tunisia.
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Gravity processing highlights unknown deep structuring and associated lineaments.
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NE-, NW-, E- and N- striking faults subdivide the area into differential sub-basins.
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Neogene NW- then N- striking stresses induced rejuvenation of inherited faults.
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Conjugate strike slip movements induced rising of synkinematic volcanic rocks.
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