A detailed gravimetric study has been integrated with the most recent stratigraphic data in the area comprised between the Arno river and the foothills of the Northern Apennines, in northern Tuscany (central Italy). A Plio-Pleistocene basin lies in this area: its sedimentary succession can be subdivided from the bottom, in five all ostratigraphic units: (1) Lower-Middle Pliocene shallow marine deposits; (2) Late Pliocene (?)- Early Pleistocene fluvio-lacustrine deposits; (3) late-Early Pleistocene-Middle Pleistocene alluvial to fluvial red conglomerates (Montecarlo Formation); (4) Middle Pleistocene alluvial to fluvial red conglomerates (Cerbaie and Casa Poggio ai Lecci Formations); (5) alluvial to fluvial deposits of Late Pleistocene age. ...
The stratigraphy and geomorphology of the Quaternary Po Basin fill record the tectonic evolution of ...
The southern Tuscany represents the internal portion of the Northern Apennines. Its geological setti...
An integration of seismological data with geological and geomorphological information aided by seism...
The post-Middle Pliocene stratigraphic evolution of lower Valdarno (northern Tuscany) is revie...
The Barga Basin, located between the Apuane Alps and the Northern Apennines, was the site of a fines...
The "Livorno-Sillaro" line represents one of the most important transversal structure of the inner N...
he "Livorno-Empoli" fault represents the westernmost segment of one a major transversal structure of...
We examine the tectonic evolution and structural characteristics of the Quaternary intermontane Muge...
The Plio-Pleistocene successions of the lower Valdarno have been studi ed since the XIX century prev...
Through the integration of sedimentological, radar interferometry and structural studies, a complex ...
"The late Quaternary Arno valley fill, in western Tuscany, was formed during the last glacio-eustati...
The Northern Apennines chain is an active orogen developed in a continental collisional setting. Dur...
The Plio-Pleistocene Calvello-Anzi Basin (CAB) represents a synorogenic shallow marine to alluvial s...
This paper illustrates the results of structural studies carried out in the western margin of Tuscan...
ABSTRACT: Incised valleys entirely filled with fluvial deposits are rarely described in the literatu...
The stratigraphy and geomorphology of the Quaternary Po Basin fill record the tectonic evolution of ...
The southern Tuscany represents the internal portion of the Northern Apennines. Its geological setti...
An integration of seismological data with geological and geomorphological information aided by seism...
The post-Middle Pliocene stratigraphic evolution of lower Valdarno (northern Tuscany) is revie...
The Barga Basin, located between the Apuane Alps and the Northern Apennines, was the site of a fines...
The "Livorno-Sillaro" line represents one of the most important transversal structure of the inner N...
he "Livorno-Empoli" fault represents the westernmost segment of one a major transversal structure of...
We examine the tectonic evolution and structural characteristics of the Quaternary intermontane Muge...
The Plio-Pleistocene successions of the lower Valdarno have been studi ed since the XIX century prev...
Through the integration of sedimentological, radar interferometry and structural studies, a complex ...
"The late Quaternary Arno valley fill, in western Tuscany, was formed during the last glacio-eustati...
The Northern Apennines chain is an active orogen developed in a continental collisional setting. Dur...
The Plio-Pleistocene Calvello-Anzi Basin (CAB) represents a synorogenic shallow marine to alluvial s...
This paper illustrates the results of structural studies carried out in the western margin of Tuscan...
ABSTRACT: Incised valleys entirely filled with fluvial deposits are rarely described in the literatu...
The stratigraphy and geomorphology of the Quaternary Po Basin fill record the tectonic evolution of ...
The southern Tuscany represents the internal portion of the Northern Apennines. Its geological setti...
An integration of seismological data with geological and geomorphological information aided by seism...