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By means of a geomorphological study and the correlation with the geochronologically constrained terraced deposits of the greater area of Rome, we attribute to the aggradational phase during marine isotopic stage (MIS) 5.5 a terraced deposit firstly described in the earliest local geological reports of the 19th century, in which a small set of lithic artifacts and vertebrate fossil remains was recovered...
The analysis of a large number of stratigraphic logs from boreholes, as well as an extensive field survey, suggests that the Middle Pleistocene sedimentary deposits in the area of Rome can be subdivided into two groups, each one characterised by a different stratigraphy and tectonic setting: a north-eastern sector, corresponding to the eastern urban area of Rome, and a south-western sector, corresponding...
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