A new geodynamic model for the Sardinian segment of the Hercynian chai
n is presented. The improvement of knowledge regarding several geologi
cal, metamorphic, magmatic and geochronological aspects of the Sardini
an Palaeozoic basement, mainly achieved in the last few years, allows
us to propose a more complete picture of its evolution. The occurrence
of remnants of an oceanic suture along a major tectonic lineament in
northern Sardinia, as well as the products of Ordovician calc-alkaline
magmatism, testifies to the presence, during the Lower Paleozoic, of
an ancient (Precambrian- Cambrian) oceanic domain and its consumption
along an Andean- type subduction zone. The following Carboniferous con
tinental collision caused crustal stacking with Barrovian metamorphism
and southward-migrating deformation from the suture zone toward the f
oreland. Early Carboniferous Culm-type facies sediments, deposited in
the outermost zone of the chain, imply that continental collision took
place earlier in the internal zone, from Late Devonian or Early Carbo
niferous. The collisional orogenic wedge experienced ductile extension
during the Late Carhoniferous as a result of gravitational collapse o
f the thickened continental crust. Extensional tectonism enhanced the
uplift of the chain and some regions underwent tectonic denudation or
LP/HT metamorphism and somewhere anatexis. The emplacement of calc-alk
aline batholiths and the development of Late Carboniferous - Early Per
mian molasse basins occurred during extension that prolonged throughou
t the Permian.