| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4717042 | Lithos | 2010 | 26 Pages |
Abstract
A detailed reconstruction of the tectono-metamorphic evolution of this Hercynian continental crustal portion allowed a Late Palaeozoic geodynamic scenario to be envisaged, in which tectonic and magmatic processes mutually interacted to define, in a feedback-type evolution, the tectono-thermal regime operating during the gravitational collapse of a previously thickened Hercynian crust.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Gerolamo Angì, Rosolino Cirrincione, Eugenio Fazio, Patrizia Fiannacca, Gaetano Ortolano, Antonino Pezzino,