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14 results on '"Giannandrea, Paolo"'

4. ll sito del Cimitero di Atella (PZ): un laboratorio di ricerca sul primo Acheuleano d’Europa

Author

Rocca, Roxane, Aureli, Daniele, Giannandrea, Paolo, Boschin, Francesco, Pereira, Alison, Nomade, Sébastien, Abruzzese, Claudia, Di Leo, Paola, Schiattarella, Marcello, Université Paris 1 Panthéon-Sorbonne - UFR Histoire de l'art et archéologie (UP1 UFR03), Université Paris 1 Panthéon-Sorbonne (UP1), Technologie et Ethnologie des Mondes Préhistoriques (TEMPS), and Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris Nanterre (UPN)-Centre National de la Recherche Scientifique (CNRS)

Subjects
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory, [SHS]Humanities and Social Sciences
Abstract

International audience

Published
2022

7. Nuovo progetto pluridisciplinare sul sito del Cimitero di Atella (Basilicata, PZ, Italia)

Author

Rocca, Roxane, Abruzzese, Claudia, Aureli, Daniele, Bahain, Jean Jacques, Beneduce, Paolo, Di Leo, Paola, Giannandrea, Paolo, Ivo, Salvatore, Gioia, Dario, Magri, Donatella, Nomade, Sebastien, Pereira, Alison, Schiattarella, Marcello, Sulpizio, Roberto, Voinchet, Pierre, Archéologies et Sciences de l'Antiquité (ArScAn), Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS), Anthropologie des techniques, des espaces et des territoires au Pliocène et au Pléistocène (AnTET), Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS)-Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS), U.R. Ecologia Preistorica, Dipartimento di Scienze Ambientali ', Histoire naturelle de l'Homme préhistorique (HNHP), Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Université de Perpignan Via Domitia (UPVD), Istituto di Metodologie per l'Analisi Ambientale (IMAA), Consiglio Nazionale delle Ricerche [Potenza] (CNR), Dipartimento di biologia ambientale, Università degli Studi di Roma 'La Sapienza' = Sapienza University [Rome], Département Homme et environnement (H&E), Muséum national d'Histoire naturelle (MNHN), CIRISIVU Dpto Geomineralogico, Università degli studi di Bari Aldo Moro (UNIBA), Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)-Centre National de la Recherche Scientifique (CNRS), Université Panthéon-Sorbonne (UP1)-Université Paris Nanterre (UPN)-Institut national de recherches archéologiques préventives (Inrap)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS), Université Panthéon-Sorbonne (UP1)-Université Paris Nanterre (UPN)-Institut national de recherches archéologiques préventives (Inrap)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS)-Université Panthéon-Sorbonne (UP1)-Université Paris Nanterre (UPN)-Institut national de recherches archéologiques préventives (Inrap)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS), Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD), Università degli Studi di Roma 'La Sapienza' [Rome], Università degli studi di Bari, Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Institut national de recherches archéologiques préventives (Inrap)-Centre National de la Recherche Scientifique (CNRS), Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Institut national de recherches archéologiques préventives (Inrap)-Centre National de la Recherche Scientifique (CNRS)-Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Institut national de recherches archéologiques préventives (Inrap)-Centre National de la Recherche Scientifique (CNRS), Università degli Studi di Roma 'La Sapienza' = Sapienza University [Rome] (UNIROMA), and Università degli studi di Bari Aldo Moro = University of Bari Aldo Moro (UNIBA)

Subjects
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory, ComputingMilieux_MISCELLANEOUS, [SHS]Humanities and Social Sciences
Abstract

International audience

Published
2016

12. Quaternary tectonostratigraphic evolution of the Vlora Basin, south‐western Albania.

Author

Palladino, Giuseppe, Giannandrea, Paolo, Siniscalchi, Agata, Magri', Cosimo, and Loiacono, Francesco

Subjects
*DISPLACED terranes, *SEDIMENTATION & deposition, *PLATE tectonics, *GEOMORPHOLOGY, *STRATIGRAPHIC geology
Abstract

The Vlora Bay is a roughly north‐west–south‐east‐oriented tectonic depression located at the collision zone between the Apulian Foreland and the Albano‐Hellenic Chain in south‐western Albania. The bay exhibits a triangular‐shaped geometry, which is the result of different tectonic phases that occurred mostly between the end of the Neogene and the Quaternary. The bay consists of two distinct physiographic sections: a shallow water marine offshore area and a recently emerged onshore sector. Along the onshore sector, Pleistocene clastic sediments filling the Pleistocene Vlora Basin crop out due to the recent uplift phases. The sedimentological and stratigraphic organization of the Vlora Basin deposits and the role played by Quaternary tectonic structures in their deposition are the main topics of this paper. A detailed field survey, supported by a geoelectrical survey, reveals a series of unconformity‐bounded stratigraphic units deposited in two north‐west–south‐east‐oriented subbasins. The two subbasins are separated by an intrabasinal, fault‐bounded, pre‐Quaternary morpho‐structural high and are mainly filled by shallow marine to continental deposits. A detailed structural analysis shows different tectonic phases affecting the area during the Pleistocene. Additionally, the geophysical survey facilitates the reconstruction of the deep structure of the basin and provides a better definition of the basin margins. Based on both geological and geophysical data, a tectonostratigraphic evolutionary model is proposed for the Vlora Basin Pleistocene sedimentary infill. This model consists of three phases of sedimentation that were essentially controlled by fault activity and by the progressive uplift of the area. [ABSTRACT FROM AUTHOR]

Published
2018
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14. Development of Pleistocene Fluvial Terraces on the Eastern Frontal Sector of the Southern Apennines Chain, Italy.

Author

Giannandrea, Paolo, Giano, Salvatore Ivo, and Sulpizio, Roberto

Subjects
FLUVIAL geomorphology, TERRACING, VALLEYS, CLIMATE change
Abstract

The investigation of Pleistocene fluvial terraces in the small river valley of the Pescogrosso Stream and surrounding areas has shown a complex and positive location for the study of a fluvial catchment development. The Pescogrosso Stream is a left tributary of the Sinni River and is placed on the eastern front of the fold-and-thrust belt of the southern Apennine chain of Italy. Sedimentological and geomorphological analyses of eight fluvial terraced units revealed that their formation and evolution were strictly controlled by regional tectonic uplift of the Ionian arc, by climatic changes, and by sea-level variations. In particular, the Ionian sea-level oscillations, as a factor in controlling the short-term fluvial terrace development, was the main factor responsible for the three older terraces' evolutions. Conversely, the evolution of the five younger terraces seems to have been controlled by the base-level variations of the Sinni River. Finally, the matching of much information derived from regional and local tectonics, the plot of longitudinal terrace profiles, and the application of a sequence-stratigraphic approach to fluvial depositional sequences allowed the recognition of three evolutionary stages of development in the Pescogrosso fluvial incised-valley system during Pleistocene times. [ABSTRACT FROM AUTHOR]

Published
2019
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