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Marco Tallini

Biographic Data

ID1884116
NAMEMarco Tallini
GIVEN NAMESMarco
FAMILY NAMETallini
SIGNATURETALLINI M
AFFILIATIONSUniversity of L'Aquila
ORCID0000-0003-4641-7824
VERIFIEDYes
TOTAL WORKS6
TOTAL CITATIONS9
WORKS AS AUTHOR6
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2004
LATEST PUBLICATION YEAR2021
H-INDEX2
  • The tectono-stratigraphic evolution of the Fucino Basin (central Apennines, Italy)

    Open Access•Gianmarco Mondati, Marco Spadi et al.•ARTICLE•Journal of Maps•2021

    We present the geological map of the north-eastern margin of the Fucino Basin, which is mainly characterized by Plio-Quaternary continental deposits that show transition from deeper-water lacustrine environment, marginal lacustrine system, and fluvial facies. These deposits unconformably overlie upper Messinian Lago-Mare sediments and pre-orogenic carbonate succession. The occurrence of Caspiocypris tiberina in the Plio-Quaternary lacustrine sedi…

  • High-resolution seismic reflection exploration for evaluating the seismic hazard in a Plio-Quaternary intermontane basin (L'Aquila downtown, central Italy)

    Open Access•Marco Tallini, Marco Spadi et al.•ARTICLE•Quaternary International•2019

  • Plio-Quaternary geology of the Paganica-San Demetrio-Castelnuovo Basin (Central Italy)

    Open Access•Marco Nocentini, Donald Cosentino et al.•ARTICLE•Journal of Maps•2018

    We present the geological map at 1:25,000 scale of the Plio-Quaternary Paganica-San Demetrio-Castelnuovo Basin corresponding to the epicentral area of the 6 April 2009 Mw: 6.29 L’Aquila earthquake. The map focuses on the relationships between the active tectonics and the Plio-Quaternary deposits and on the early evolution of this continental basin. Fine-scale geological field surveys, coupled with paleontological data, facies analyses, well logs …

  • Plio-Quaternary geology of L’Aquila – Scoppito Basin (Central Italy)

    Open Access•Marco Nocentini, Riccardo Asti et al.•ARTICLE•Journal of Maps•2017

    We present a geological map at 1:25,000 scale of the Plio-Quaternary L’Aquila-Scoppito intermontane basin (central Italy), which corresponds to the epicentral area of the 6th April 2009 L’Aquila earthquake (Mw: 6.29). The map is derived from geological field surveys at 1:5000 scale and takes into account previously published maps. It is supported by a fine-scale LiDAR digital elevation model, paleontological analyses, 14C dating, well log analyse…

  • Mammuthus meridionalis (Nesti, 1825) from Campo di Pile (L'Aquila, Abruzzo, Central Italy)

    Open Access•Silvano Agostini, Maria Rita Palombo et al.•ARTICLE•Quaternary International•2012•Cited by: 3•References: 2

  • Ground penetrating radar investigations for the restoration of historic buildings

    Open Access•Danilo Ranalli, Marco Scozzafava et al.•ARTICLE•Journal of Cultural Heritage•2004•Cited by: 6•References: 4

  • Ground penetrating radar investigations for the restoration of historic buildings

    Open Access•Danilo Ranalli, Marco Scozzafava et al.•ARTICLE•Journal of Cultural Heritage•2004•Cited by: 6•References: 4

  • Mammuthus meridionalis (Nesti, 1825) from Campo di Pile (L'Aquila, Abruzzo, Central Italy)

    Open Access•Silvano Agostini, Maria Rita Palombo et al.•ARTICLE•Quaternary International•2012•Cited by: 3•References: 2

  • Ground penetrating radar investigations for the restoration of historic buildings

    Open Access•Danilo Ranalli, Marco Scozzafava et al.•ARTICLE•Journal of Cultural Heritage•2004•Cited by: 6•References: 4

  • Mammuthus meridionalis (Nesti, 1825) from Campo di Pile (L'Aquila, Abruzzo, Central Italy)

    Open Access•Silvano Agostini, Maria Rita Palombo et al.•ARTICLE•Quaternary International•2012•Cited by: 3•References: 2

  • Plio-Quaternary geology of L’Aquila – Scoppito Basin (Central Italy)

    Open Access•Marco Nocentini, Riccardo Asti et al.•ARTICLE•Journal of Maps•2017

    We present a geological map at 1:25,000 scale of the Plio-Quaternary L’Aquila-Scoppito intermontane basin (central Italy), which corresponds to the epicentral area of the 6th April 2009 L’Aquila earthquake (Mw: 6.29). The map is derived from geological field surveys at 1:5000 scale and takes into account previously published maps. It is supported by a fine-scale LiDAR digital elevation model, paleontological analyses, 14C dating, well log analyse…

  • Plio-Quaternary geology of the Paganica-San Demetrio-Castelnuovo Basin (Central Italy)

    Open Access•Marco Nocentini, Donald Cosentino et al.•ARTICLE•Journal of Maps•2018

    We present the geological map at 1:25,000 scale of the Plio-Quaternary Paganica-San Demetrio-Castelnuovo Basin corresponding to the epicentral area of the 6 April 2009 Mw: 6.29 L’Aquila earthquake. The map focuses on the relationships between the active tectonics and the Plio-Quaternary deposits and on the early evolution of this continental basin. Fine-scale geological field surveys, coupled with paleontological data, facies analyses, well logs …

  • High-resolution seismic reflection exploration for evaluating the seismic hazard in a Plio-Quaternary intermontane basin (L'Aquila downtown, central Italy)

    Open Access•Marco Tallini, Marco Spadi et al.•ARTICLE•Quaternary International•2019

  • The tectono-stratigraphic evolution of the Fucino Basin (central Apennines, Italy)

    Open Access•Gianmarco Mondati, Marco Spadi et al.•ARTICLE•Journal of Maps•2021

    We present the geological map of the north-eastern margin of the Fucino Basin, which is mainly characterized by Plio-Quaternary continental deposits that show transition from deeper-water lacustrine environment, marginal lacustrine system, and fluvial facies. These deposits unconformably overlie upper Messinian Lago-Mare sediments and pre-orogenic carbonate succession. The occurrence of Caspiocypris tiberina in the Plio-Quaternary lacustrine sedi…

Geology (6 works) · Paleontology (5 works) · Quaternary (5 works) · Structural basin (5 works) · Geomorphology (4 works) · earthquake and tectonic studies (3 works) · Fluvial (3 works) · Geography (3 works) · Pleistocene (3 works) · Seismic Waves and Analysis (3 works)

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