[PDF][PDF] Geology of the central Apennines: a regional review
D Cosentino, P Cipollari, P Marsili… - Journal of the virtual …, 2010 - researchgate.net
Journal of the virtual explorer, 2010•researchgate.net
The Meso-Cenozoic stratigraphical successions that crop out in central Italy are part of the
sedimentary wedge developed on the southern Neotethyan passive margin. On the previous
Late Triassic shallow-water carbonate platform, a basin-platform system developed in the
area as a consequence of a rifting stage that affected the whole Neotethyan region during
the Middle Liassic. The palaeogeography related to the basin-platform system was
persistent until early Tertiary time.
sedimentary wedge developed on the southern Neotethyan passive margin. On the previous
Late Triassic shallow-water carbonate platform, a basin-platform system developed in the
area as a consequence of a rifting stage that affected the whole Neotethyan region during
the Middle Liassic. The palaeogeography related to the basin-platform system was
persistent until early Tertiary time.
Abstract
The Meso-Cenozoic stratigraphical successions that crop out in central Italy are part of the sedimentary wedge developed on the southern Neotethyan passive margin. On the previous Late Triassic shallow-water carbonate platform, a basin-platform system developed in the area as a consequence of a rifting stage that affected the whole Neotethyan region during the Middle Liassic. The palaeogeography related to the basin-platform system was persistent until early Tertiary time.
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