The present-day physiographic-tectonic features of the Central Mediterranean region are the product of the geodynamic evolution in which a fundamental role is played by the distribution of crustal components. The orogenic belt is located between an old oceanic crust, the Ionian basin, which has been partially consumed, and a new oceanic crust, the abyssal plane of the Tyrrhenian basin. Moreover, the CROP-Mare project recognized a continental crust in the circum-Tyrrhenian margins associated with migrated tectonic stacks that were colliding with the continental blocks of the Africa and Adria plates.
|Titolo:||The Apenninic-Maghrebian Orogen in the Central Mediterranean Region: a review.|
|Autori interni:||CARBONE, Serafina|
|Data di pubblicazione:||2010|
|Rivista:||ANALELE STIINTIFICE ALE UNIVERSITATII "AL.I. CUZA" DIN IASI. GEOLOGIE|
|Appare nelle tipologie:||1.1 Articolo in rivista|