9in fold and thrust belts developing at convergent margins, the migration of the advancing wedge is accompanied by bulging of the downgoing plate, followed by the development of a foredeep basin filled by a thick succession of syn-orogenic sediments. The transition from forebulge to foredeep marks a key moment in the evolution of the orogenic system. In deep water environments, the record of this transition is typically complete and progressive. Conversely, in the shallow-water/continental environment of many collisional systems, the uplift of the forebulge area can imply emersion and erosion, obliterating the stratigraphic record of key steps of the evolution of the orogenic system. The southern Apennines constitute one of these collisiona...
The Upper Oligocene Macigno Formation cropping out in the coastal section of SW Tuscany represents t...
Syn-orogenic deposits within foredeep basins undergo exten- sion related to the initiation of the ba...
Stratigraphic and structural data indicate that, at the beginning of the Miocene, the frontal part o...
In fold and thrust belts developing at convergent margins, the migration of the advancing wedge is a...
9noThe Apennines are a retreating collisional belt where the foreland basin system, across large dom...
ABSTRACT: The Northern Apennines provide an example of long-term deep-water sedimentation in an unde...
Assessment of vertical and horizontal displacements and displacement rates within the western Adriat...
The Southern Apennine fold and thrust belt differs from other parts of the peri-Tyrrhenian orogen. I...
The Southern Apenninic chain was built up from the late Oligocene–early Miocene to the middle Pleist...
In the Northern Apennines of Italy the Ligurian and Subligurian Units (LSU) were involved, since the...
The Upper Oligocene Macigno Formation cropping out in the coastal section of SW Tuscany represents t...
Syn-orogenic deposits within foredeep basins undergo exten- sion related to the initiation of the ba...
Stratigraphic and structural data indicate that, at the beginning of the Miocene, the frontal part o...
In fold and thrust belts developing at convergent margins, the migration of the advancing wedge is a...
9noThe Apennines are a retreating collisional belt where the foreland basin system, across large dom...
ABSTRACT: The Northern Apennines provide an example of long-term deep-water sedimentation in an unde...
Assessment of vertical and horizontal displacements and displacement rates within the western Adriat...
The Southern Apennine fold and thrust belt differs from other parts of the peri-Tyrrhenian orogen. I...
The Southern Apenninic chain was built up from the late Oligocene–early Miocene to the middle Pleist...
In the Northern Apennines of Italy the Ligurian and Subligurian Units (LSU) were involved, since the...
The Upper Oligocene Macigno Formation cropping out in the coastal section of SW Tuscany represents t...
Syn-orogenic deposits within foredeep basins undergo exten- sion related to the initiation of the ba...
Stratigraphic and structural data indicate that, at the beginning of the Miocene, the frontal part o...