|
|
|
|
|
Vincenzo Pascucci, Gabriela Frulio and Stefano Andreucci
The study area is located in NW Sardinia Island (Italy), Mediterranean Sea. Sardinia is considered stable since the late Pliocene with a negligible subsidence of about 0.01 mm/y. It is therefore normally used to reconstruct the Pleistocene and Holocene s...
ver más
|
|
|
|
|