Paleomagnetism has played an important role in the development of geodynamic models for the Italian peninsula. Paleomagnetic data from this area have been increasingly reported since the late 1960s, placing important constraints on geodynamics. A brief outline of the main concepts underlying a paleomagnetic study is provided in the first part of this paper. We also discuss the criteria for the assessment of the reliability of paleomagnetic data. Finally, the data collected over the past 25 years in peninsular and insular Italy are synthetically reviewed, discussing the main implications for the geodynamic evolution of the Tyrrhenian í Apennines í foreland system
The paleomagnetism of the Plio-Pleistocene continental sediments cropping out at the north-eastern e...
In this paper, new paleomagnetic results from the Calabrian Arc are presented, together with a crit...
Starting from middle Miocene, the inner sector of the Calabria Arc (southern Italy) was characterise...
Paleomagnetism has played an important role in the development of geodynamic models for the Italian ...
The Apennines are a mountain belt developed during the Neogene along the western margin of the Adria...
A review is given of paleomagnetic data that have become available during the last years. The accen...
Paleomagnetism is proving to represent one of the most powerful dating tools of volcanics emplaced ...
A review is given of paleomagnetic data that have become available during the last years. The accent...
The southern Apennine belt is formed by nappes that have undergone large (i. e. hundreds of kms) ho...
A preliminary collection of 43 palaeomagnetic samples (10 sites) from the miogeosynclinal and suppos...
VandenBerg, J., 1983. Reappraisal of paleomagnetic data from Gargano (South Italy). In: E. McClellan...
We report on new paleomagnetic results obtained from 27 sites sampled in the Plio-Pleistocene sequen...
New paleomagnetic data are presented from Tuscany and the Southern Alps (Italy). A paleomagnetic st...
The Roveto Valley is a narrow, elongated, NW-trending depression filled with continental Plio-Quater...
We report on a palaeomagnetic study of upper Miocene sediments from the Amantea basin, located on th...
The paleomagnetism of the Plio-Pleistocene continental sediments cropping out at the north-eastern e...
In this paper, new paleomagnetic results from the Calabrian Arc are presented, together with a crit...
Starting from middle Miocene, the inner sector of the Calabria Arc (southern Italy) was characterise...
Paleomagnetism has played an important role in the development of geodynamic models for the Italian ...
The Apennines are a mountain belt developed during the Neogene along the western margin of the Adria...
A review is given of paleomagnetic data that have become available during the last years. The accen...
Paleomagnetism is proving to represent one of the most powerful dating tools of volcanics emplaced ...
A review is given of paleomagnetic data that have become available during the last years. The accent...
The southern Apennine belt is formed by nappes that have undergone large (i. e. hundreds of kms) ho...
A preliminary collection of 43 palaeomagnetic samples (10 sites) from the miogeosynclinal and suppos...
VandenBerg, J., 1983. Reappraisal of paleomagnetic data from Gargano (South Italy). In: E. McClellan...
We report on new paleomagnetic results obtained from 27 sites sampled in the Plio-Pleistocene sequen...
New paleomagnetic data are presented from Tuscany and the Southern Alps (Italy). A paleomagnetic st...
The Roveto Valley is a narrow, elongated, NW-trending depression filled with continental Plio-Quater...
We report on a palaeomagnetic study of upper Miocene sediments from the Amantea basin, located on th...
The paleomagnetism of the Plio-Pleistocene continental sediments cropping out at the north-eastern e...
In this paper, new paleomagnetic results from the Calabrian Arc are presented, together with a crit...
Starting from middle Miocene, the inner sector of the Calabria Arc (southern Italy) was characterise...