A facies analysis and preliminary palaeoclimate and biochronology investigation, are presented for the San Lorenzo lacustrine deposits, outcropping in the Pliocene to Pleistocene satellite Sant'Arcangelo Basin (Southern Apennines). Facies analysis shows that sedimentation developed in the inner zone of a terrigenous-dominated fresh water lake. The pollen record shows repeated alternations between two distinct vegetational assemblages, one dominated by steppe taxa, and the other one by forest taxa. The faunal assemblage is indicative of a late Biharian mammal age. The palaeomagnetic survey yielded three polarity intervals throughout the succession; the middle one is of reversed polarity (and is associated with a volcaniclastic layer radiomet...
The Acerno lacustrine basin is a tectonic palaeolake formed during the Middle Pleistocene. Pollen an...
The drainage integration of three Late Pleistocene intramontane basins located in the southern Itali...
The Pantano di San Gregorio Magno is a 4.7km2 large tectono-karstic basin located in the axial belt ...
A facies analysis and preliminary palaeoclimate and biochronology investigation, are presented for t...
The Sant’Arcangelo Basin is located in the southern part of the Apennine chain (Basilicata). It is f...
A continental depositional sequence was developed in a NW-SE trending syncline basin, which was form...
Quaternary lacustrine sedimentation of the San Lorenzo Succession represents one of the more recent ...
The late Quaternary evolution of the Mercure paleolacustrine basin (Lucanian Apennines, southern Ita...
Multidisciplinary investigations at Pagliare di Sassa (L’Aquila, central Italy) suggest that the loc...
The study site is located in the north-western part of the Caudina valley , a wide intramontane basi...
Defined as a piggyback basin, the Plio-Pleistocene Sant'Arcangelo basin is one of the more recent on...
An interdisciplinary investigation of the Pleistocene clay succession of Fornaci di Ranica (Italian ...
Multidisciplinary investigations at Pagliare di Sassa (L'Aquila, central Italy) suggest that the loc...
The Acerno lacustrine basin represents a tectonic palaeolake formed in the southern Apennines during...
The lacustrine succession of the Sessano basin represents the filling of a N-S trending structural d...
The Acerno lacustrine basin is a tectonic palaeolake formed during the Middle Pleistocene. Pollen an...
The drainage integration of three Late Pleistocene intramontane basins located in the southern Itali...
The Pantano di San Gregorio Magno is a 4.7km2 large tectono-karstic basin located in the axial belt ...
A facies analysis and preliminary palaeoclimate and biochronology investigation, are presented for t...
The Sant’Arcangelo Basin is located in the southern part of the Apennine chain (Basilicata). It is f...
A continental depositional sequence was developed in a NW-SE trending syncline basin, which was form...
Quaternary lacustrine sedimentation of the San Lorenzo Succession represents one of the more recent ...
The late Quaternary evolution of the Mercure paleolacustrine basin (Lucanian Apennines, southern Ita...
Multidisciplinary investigations at Pagliare di Sassa (L’Aquila, central Italy) suggest that the loc...
The study site is located in the north-western part of the Caudina valley , a wide intramontane basi...
Defined as a piggyback basin, the Plio-Pleistocene Sant'Arcangelo basin is one of the more recent on...
An interdisciplinary investigation of the Pleistocene clay succession of Fornaci di Ranica (Italian ...
Multidisciplinary investigations at Pagliare di Sassa (L'Aquila, central Italy) suggest that the loc...
The Acerno lacustrine basin represents a tectonic palaeolake formed in the southern Apennines during...
The lacustrine succession of the Sessano basin represents the filling of a N-S trending structural d...
The Acerno lacustrine basin is a tectonic palaeolake formed during the Middle Pleistocene. Pollen an...
The drainage integration of three Late Pleistocene intramontane basins located in the southern Itali...
The Pantano di San Gregorio Magno is a 4.7km2 large tectono-karstic basin located in the axial belt ...