Abstract
The tectono-stratigraphic framework of the southern Montefeltro is
illustrative of the interaction between thin-skinned shearing and sedimentation
in the outer segment of the Apenninic orogenic system during the Neogene.
Mesozoic through Paleogene evaporitic-carbonatic-marly terrains constitute
the lower part of its autochthonous sedimentary cover. This Umbro-Marchean
Sequence compares with deposits of the contiguous Adriatic Foreland. Structural
style
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