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Papers by Stefano Marabini

Research paper thumbnail of Aspetti geomorfologici. Rapporti tra evoluzione geologica e insediamento umano nel faentino

Research paper thumbnail of Explanatory Notes of the Litho-Palaeoenvironmental Maps of Italy During the Last Two Climatic Extremes

Vengono presentate le carte paleoambientali dell'Italia durante i due ultimi eventi estremi p... more Vengono presentate le carte paleoambientali dell'Italia durante i due ultimi eventi estremi paleoclimatici (l'ultimo massimo glaciale e l'optimum climatico olocenico

Research paper thumbnail of Map 2 - Holocene Climatic Optimum (8 ± 1 ka cal BP) average surface air temperature of about 2.5 °C higher than today

Thematic map of Holocene climatic Optimum, with informations on glaciers, vertebrates, serpulids,... more Thematic map of Holocene climatic Optimum, with informations on glaciers, vertebrates, serpulids, lakes, vegetation, alluvial plains, Apennine foothills, marine bathymetry and bottom morphology, shore lines, sea surface temperature, archaeology, active faults

Research paper thumbnail of Studio sismotettonico dell'Appennino forlivese: il progetto GEOSIS

Bollettino di geodesia e scienze affini, 1990

Research paper thumbnail of Original visual imaging in Marsili’s (1658–1730) geology and mapping

Italian Journal of Geosciences

Research paper thumbnail of OPT3 72dpimod

Research paper thumbnail of Analisi di facies e macrotettonica della vena del gesso di Romagna

Bollettino Della Societa Geologica Italiana, 1985

Research paper thumbnail of A Younger Dryas sediment wave and enhanced erosion at millennial time scales in a non-glacierized catchment, Northern Apennines, Italy

EGU General Assembly Conference Abstracts, Apr 1, 2018

Research paper thumbnail of Lo studio della sezione “Il Fronte” per la definizione del piano Tarantiano (Puglia, Italy)

F. Antonioli, A. Deino, L. Ferranti, J. Keller, S. Marabini, G. Mastronuzzi, A. Negri, A. Piva, G... more F. Antonioli, A. Deino, L. Ferranti, J. Keller, S. Marabini, G. Mastronuzzi, A. Negri, A. Piva, G.B.Vai & L. Vigliotti , The study of “Il Fronte” Section to define the Tarentian Stage (Puglia, Italy). The Italian Commission on Stratigraphy of the SGI is seeking for a marine section suitable for defining the Upper Pleistocene GSSP. This Series has been usually identified with the Tyrrhenian Stage which in the wake of formalization received different meaning from stratigraphers and geomorphologits. Hence, the proposal of a new Upper Pleistocene Stage name and type area, the Tarentian, created in 1994. Criteria for defining the Tarentian Stage and selecting its GSSP can be the beginning of MIS 5 (~ 134 ka) and the beginning of MIS 1 (~ 10 ka) taken for the base of the Holocene. The Tarentian Stage also contains MIS 5.5 highstand with its peak at ~ 125 ka. Upper Pleistocene marine deposits of thickness exceeding 1 to 2 m are rarely exposed on land except for some Mediterranean countries...

Research paper thumbnail of Carta Geologica D’Italia – Faenza Foglio 239 della carta 1:50.000 dell’I.G.M

Research paper thumbnail of Adding geological criterion VIII to the dossier for nominating the sila national park to the unesco world heritage list

Research paper thumbnail of The Tarentian Fronte Section (Taranto, Italy): a suitable Upper Pleistocene GSSP

Research paper thumbnail of Gli straordinari aspetti geologici della Sila

La Sila costituisce un vasto acrocoro a forma rettangolare, in direzione N-S, posizionato nella p... more La Sila costituisce un vasto acrocoro a forma rettangolare, in direzione N-S, posizionato nella parte centrale della Regione Calabria ed esteso per circa 1.700 chilometri quadrati, interrotto irregolarmente da catene e cime piu elevate, come M. Botte Donato (m. 1928), Monte Nero (m. 1881), Monte Stella (m. 1812), Monte Gariglione (m. 1765) e Monte Femmina Morta (m. 1770). I suoi limiti morfologici sono la Piana di Sibari e la parte terminale del Fiume Crati a nord; le valli dei fiumi Crati e Savuto ad ovest; la piana di Lamezia Terme, il fiume Amato, la Sella di Marcellinara e la costa ionica catanzarese a sud; il marchesato e la costa ionica crotonese e cosentina ad est. La superficie sommitale del Massiccio, in riferimento alla quale si usa la definizione di Altopiano Silano, conserva ancora i caratteri di una vasta spianata continentale, evoluta in clima caldo-umido tra il Pliocene superiore ed il Pleistocene inferiore, con un intenso stato di alterazione nelle rocce affioranti, ...

Research paper thumbnail of In search of the Upper Pleistocene GSSP: bridging the gap in the correlation of Marine and Continental sedimentary successions

Research paper thumbnail of The evolution of “fairy chimneys” in Goreme valley (Cappadocia, Turkey): new geomorphological and stratigraphic assessments

Research paper thumbnail of Assetto paleidografico e centuriazione romana nella pianura faentina

Assetto paleidografico e centuriazione romana nella pianura faentina, 2004

Research paper thumbnail of The Fronte Candidate Section for the Upper Pleistocene GSSP: A Short Report

We report new data regarding the environmental history of the Taranto Area since MIS 11, which po... more We report new data regarding the environmental history of the Taranto Area since MIS 11, which possibly led to the peculiar sediment preservation characterizing the Fronte Section. This section is a very promising candidate for the Upper Pleistocene GSSP. Some preliminary results achieved after the multiple core drilling at the Fronte locality (Taranto, Italy) are reported as well.

Research paper thumbnail of Provenance of the Cotignola Quarry Sands (Northern Apennines) as a Tool for Palaeogeographical Studies on the Action of Senio and Santerno Rivers in the Romagna Floodplain

Research paper thumbnail of A High-Resolution Upper Pleistocene Palaeomagnetic Record from the Fronte Section at Taranto, Italy

Research paper thumbnail of A possible Upper Pleistocene global boundary stratotype section and point (GSSP): The Fronte Section at Taranto (Italy)

Research paper thumbnail of Aspetti geomorfologici. Rapporti tra evoluzione geologica e insediamento umano nel faentino

Research paper thumbnail of Explanatory Notes of the Litho-Palaeoenvironmental Maps of Italy During the Last Two Climatic Extremes

Vengono presentate le carte paleoambientali dell'Italia durante i due ultimi eventi estremi p... more Vengono presentate le carte paleoambientali dell'Italia durante i due ultimi eventi estremi paleoclimatici (l'ultimo massimo glaciale e l'optimum climatico olocenico

Research paper thumbnail of Map 2 - Holocene Climatic Optimum (8 ± 1 ka cal BP) average surface air temperature of about 2.5 °C higher than today

Thematic map of Holocene climatic Optimum, with informations on glaciers, vertebrates, serpulids,... more Thematic map of Holocene climatic Optimum, with informations on glaciers, vertebrates, serpulids, lakes, vegetation, alluvial plains, Apennine foothills, marine bathymetry and bottom morphology, shore lines, sea surface temperature, archaeology, active faults

Research paper thumbnail of Studio sismotettonico dell'Appennino forlivese: il progetto GEOSIS

Bollettino di geodesia e scienze affini, 1990

Research paper thumbnail of Original visual imaging in Marsili’s (1658–1730) geology and mapping

Italian Journal of Geosciences

Research paper thumbnail of OPT3 72dpimod

Research paper thumbnail of Analisi di facies e macrotettonica della vena del gesso di Romagna

Bollettino Della Societa Geologica Italiana, 1985

Research paper thumbnail of A Younger Dryas sediment wave and enhanced erosion at millennial time scales in a non-glacierized catchment, Northern Apennines, Italy

EGU General Assembly Conference Abstracts, Apr 1, 2018

Research paper thumbnail of Lo studio della sezione “Il Fronte” per la definizione del piano Tarantiano (Puglia, Italy)

F. Antonioli, A. Deino, L. Ferranti, J. Keller, S. Marabini, G. Mastronuzzi, A. Negri, A. Piva, G... more F. Antonioli, A. Deino, L. Ferranti, J. Keller, S. Marabini, G. Mastronuzzi, A. Negri, A. Piva, G.B.Vai & L. Vigliotti , The study of “Il Fronte” Section to define the Tarentian Stage (Puglia, Italy). The Italian Commission on Stratigraphy of the SGI is seeking for a marine section suitable for defining the Upper Pleistocene GSSP. This Series has been usually identified with the Tyrrhenian Stage which in the wake of formalization received different meaning from stratigraphers and geomorphologits. Hence, the proposal of a new Upper Pleistocene Stage name and type area, the Tarentian, created in 1994. Criteria for defining the Tarentian Stage and selecting its GSSP can be the beginning of MIS 5 (~ 134 ka) and the beginning of MIS 1 (~ 10 ka) taken for the base of the Holocene. The Tarentian Stage also contains MIS 5.5 highstand with its peak at ~ 125 ka. Upper Pleistocene marine deposits of thickness exceeding 1 to 2 m are rarely exposed on land except for some Mediterranean countries...

Research paper thumbnail of Carta Geologica D’Italia – Faenza Foglio 239 della carta 1:50.000 dell’I.G.M

Research paper thumbnail of Adding geological criterion VIII to the dossier for nominating the sila national park to the unesco world heritage list

Research paper thumbnail of The Tarentian Fronte Section (Taranto, Italy): a suitable Upper Pleistocene GSSP

Research paper thumbnail of Gli straordinari aspetti geologici della Sila

La Sila costituisce un vasto acrocoro a forma rettangolare, in direzione N-S, posizionato nella p... more La Sila costituisce un vasto acrocoro a forma rettangolare, in direzione N-S, posizionato nella parte centrale della Regione Calabria ed esteso per circa 1.700 chilometri quadrati, interrotto irregolarmente da catene e cime piu elevate, come M. Botte Donato (m. 1928), Monte Nero (m. 1881), Monte Stella (m. 1812), Monte Gariglione (m. 1765) e Monte Femmina Morta (m. 1770). I suoi limiti morfologici sono la Piana di Sibari e la parte terminale del Fiume Crati a nord; le valli dei fiumi Crati e Savuto ad ovest; la piana di Lamezia Terme, il fiume Amato, la Sella di Marcellinara e la costa ionica catanzarese a sud; il marchesato e la costa ionica crotonese e cosentina ad est. La superficie sommitale del Massiccio, in riferimento alla quale si usa la definizione di Altopiano Silano, conserva ancora i caratteri di una vasta spianata continentale, evoluta in clima caldo-umido tra il Pliocene superiore ed il Pleistocene inferiore, con un intenso stato di alterazione nelle rocce affioranti, ...

Research paper thumbnail of In search of the Upper Pleistocene GSSP: bridging the gap in the correlation of Marine and Continental sedimentary successions

Research paper thumbnail of The evolution of “fairy chimneys” in Goreme valley (Cappadocia, Turkey): new geomorphological and stratigraphic assessments

Research paper thumbnail of Assetto paleidografico e centuriazione romana nella pianura faentina

Assetto paleidografico e centuriazione romana nella pianura faentina, 2004

Research paper thumbnail of The Fronte Candidate Section for the Upper Pleistocene GSSP: A Short Report

We report new data regarding the environmental history of the Taranto Area since MIS 11, which po... more We report new data regarding the environmental history of the Taranto Area since MIS 11, which possibly led to the peculiar sediment preservation characterizing the Fronte Section. This section is a very promising candidate for the Upper Pleistocene GSSP. Some preliminary results achieved after the multiple core drilling at the Fronte locality (Taranto, Italy) are reported as well.

Research paper thumbnail of Provenance of the Cotignola Quarry Sands (Northern Apennines) as a Tool for Palaeogeographical Studies on the Action of Senio and Santerno Rivers in the Romagna Floodplain

Research paper thumbnail of A High-Resolution Upper Pleistocene Palaeomagnetic Record from the Fronte Section at Taranto, Italy

Research paper thumbnail of A possible Upper Pleistocene global boundary stratotype section and point (GSSP): The Fronte Section at Taranto (Italy)

Research paper thumbnail of Tommaso Ismaelli, Giuseppe Scardozzi (edited by), "ANCIENT QUARRIES AND BUILDING SITES IN ASIA MINOR. Research on Hierapolis in Phrygia and other cities in south-western Anatolia: archaeology, archeometry, conservation", Bibliotheca Archaeologica 45, Edipuglia

This volume presents the results of the Marmora Phrygiae Project, financed by the Italian Ministr... more This volume presents the results of the Marmora Phrygiae Project, financed by the Italian Ministry of Education, University and Research (MIUR – Ministero dell’Istruzione, dell’Università e della Ricerca) as part of the “Futuro in Ricerca” programme (FIRB 2012). In the period 2013-2016, following a multidisciplinary approach, the project sought to reconstruct the building stone procurement strategies adopted in the city of Hierapolis in Phrygia (Turkey), across a broad chronological time span from the Hellenistic epoch to the Byzantine period. Extensive knowledge of the territory surrounding the city and detailed research into its monuments provided the basis for a painstaking historical reconstruction. The volume describes the economic, social, technological and legal aspects of the use of marble and presents the results of the archaeometric investigations that were conducted in order to characterise the building stones, determine their provenance and assess the state of conservation of the monuments. In addition, the volume illustrates recent research conducted by teams of various nationalities into the marble quarrying districts and monumental complexes of the main settlements of south-western Asia Minor in the Imperial and Byzantine epochs.