The Southern Apennines, Calabro-Peloritane block, and Sicilian Maghrebides form a ~700 km long orogenic bend, known as Calabrian Arc (Cifelli et al., 2007). The bending of this orogenic system was realized progressively through opposite-sense rotation of the two limbs, counterclockwise (CCW) in the Southern Apennines and clockwise (CW) in the Sicilian Maghrebides, synchronous to the Miocene-to-Present opening of the Tyrrhenian Sea. Despite the wealth of paleomagnetic data from the Southern Apennines, the main Miocene rotational phase still remains poorly constrained in time and, more importantly, data from the most internal paleogeographic domains of the belt are completely lacking. The Gorgoglione Formation, a middle Miocene piggy-back d...
We report on an extensive paleomagnetic study (36 sites) of the Tuscan Nappe succession from the No...
New palaeomagnetic data from upper Triassic to Pliocene sediments reveal that in eastern Sicily a ma...
In the past few years, a wealth of paleomagnetic data gathered from Neogene sediments consistently s...
The Southern Apennines, Calabro-Peloritane block, and Sicilian Maghrebides form a ~ 700 km long orog...
The Southern Apennines, Calabro-Peloritane block, and Sicilian Maghrebides form a ~700 km long oroge...
The southern Apennine belt is formed by nappes that have undergone large (i. e. hundreds of kms) hor...
In this paper, new paleomagnetic results from the Calabrian Arc are presented, together with a crit...
The present-day arcuate shape of the Calabrian Arc has been accomplished during Neogene and Early Pl...
We report on a palaeomagnetic study of upper Miocene sediments from the Amantea basin, located on th...
The present-day arcuate shape of the Calabrian Arc has been accomplished during Neogene and Early Pl...
The Apennines are a mountain belt developed during the Neogene along the western margin of the Adria...
Paleomagnetic studies of sediments from the Calabro-Peloritan block in southern Italy consequently i...
We report on an extensive paleomagnetic study (36 sites) of the Tuscan Nappe succession from the No...
In the Central Mediterranean area, one of the most interesting geodynamical processes on our Earth ...
The post-collisional Neogene Southern Apennines thrust belt presents a complex Pliocene-Quaternary k...
We report on an extensive paleomagnetic study (36 sites) of the Tuscan Nappe succession from the No...
New palaeomagnetic data from upper Triassic to Pliocene sediments reveal that in eastern Sicily a ma...
In the past few years, a wealth of paleomagnetic data gathered from Neogene sediments consistently s...
The Southern Apennines, Calabro-Peloritane block, and Sicilian Maghrebides form a ~ 700 km long orog...
The Southern Apennines, Calabro-Peloritane block, and Sicilian Maghrebides form a ~700 km long oroge...
The southern Apennine belt is formed by nappes that have undergone large (i. e. hundreds of kms) hor...
In this paper, new paleomagnetic results from the Calabrian Arc are presented, together with a crit...
The present-day arcuate shape of the Calabrian Arc has been accomplished during Neogene and Early Pl...
We report on a palaeomagnetic study of upper Miocene sediments from the Amantea basin, located on th...
The present-day arcuate shape of the Calabrian Arc has been accomplished during Neogene and Early Pl...
The Apennines are a mountain belt developed during the Neogene along the western margin of the Adria...
Paleomagnetic studies of sediments from the Calabro-Peloritan block in southern Italy consequently i...
We report on an extensive paleomagnetic study (36 sites) of the Tuscan Nappe succession from the No...
In the Central Mediterranean area, one of the most interesting geodynamical processes on our Earth ...
The post-collisional Neogene Southern Apennines thrust belt presents a complex Pliocene-Quaternary k...
We report on an extensive paleomagnetic study (36 sites) of the Tuscan Nappe succession from the No...
New palaeomagnetic data from upper Triassic to Pliocene sediments reveal that in eastern Sicily a ma...
In the past few years, a wealth of paleomagnetic data gathered from Neogene sediments consistently s...