Deep-seated gravitational slope deformations (DSGSDs) show a wide range of geomorphological characteristics and kinematic behaviours. In many cases, deforming rock masses move on a continuous surface or a thick basal shear zone (BSZ) overlying the stable bedrock. The nature of this boundary is a significant issue in scientific debates since examples of BSZs have been observed or inferred in some DSGSDs worldwide. In the central Apennines, although several cases of DSGSDs have been described in recent decades, no evidence of BSZs has been documented thus far. This work presents the first case of a BSZ found in the region at the bottom of a large-scale gravitational deformation that affects the Mesozoic-Cenozoic carbonate ridge overhanging th...
The present work illustrates three cases of deep-seated gravitational slope deformation (DSGSD) in a...
Active faulting is one of the main factors that induce deep-seated gravitational slope deformations ...
Many areas of the Earth’s crust deform by distributed extensional faulting and the occurrence of ear...
Deep-seated gravitational slope deformations (DSGSDs) show a wide range of geomorphological characte...
During the last 30 years of studies in the field of mass movements located in the calcareous-marly a...
The attention to deep-seated gravitational slope deformations (DSGSDs) has steadily increased in the...
The attention to deep-seated gravitational slope deformations (DSGSDs) has steadily increased in the...
The Upper Scrivia Valley in the Ligurian Apennines is characterized by a large-scale landslides area...
Eight cases of large-scale gravitational movements (with evidence of rock-slide type displacements) ...
In this study, we analyse deep-seated gravitational slope deformations (DSGSDs) in central Sardinia....
International audienceActive faulting and deep-seated gravitational slope deformation (DGSD) are com...
The study, developed over a wide mountain sector of the central Apennines (Italy), highlights the ro...
A deep-seated gravitational slope deformation (DGSD) affects the eastern side of the Chianti Mts. Ri...
Among the causes of deep-seated gravitational slope deformations (DGSD), the most important is relie...
Some features make north-western Tuscany prone to Deep-seated Gravitational Slope Deformations (DGSD...
The present work illustrates three cases of deep-seated gravitational slope deformation (DSGSD) in a...
Active faulting is one of the main factors that induce deep-seated gravitational slope deformations ...
Many areas of the Earth’s crust deform by distributed extensional faulting and the occurrence of ear...
Deep-seated gravitational slope deformations (DSGSDs) show a wide range of geomorphological characte...
During the last 30 years of studies in the field of mass movements located in the calcareous-marly a...
The attention to deep-seated gravitational slope deformations (DSGSDs) has steadily increased in the...
The attention to deep-seated gravitational slope deformations (DSGSDs) has steadily increased in the...
The Upper Scrivia Valley in the Ligurian Apennines is characterized by a large-scale landslides area...
Eight cases of large-scale gravitational movements (with evidence of rock-slide type displacements) ...
In this study, we analyse deep-seated gravitational slope deformations (DSGSDs) in central Sardinia....
International audienceActive faulting and deep-seated gravitational slope deformation (DGSD) are com...
The study, developed over a wide mountain sector of the central Apennines (Italy), highlights the ro...
A deep-seated gravitational slope deformation (DGSD) affects the eastern side of the Chianti Mts. Ri...
Among the causes of deep-seated gravitational slope deformations (DGSD), the most important is relie...
Some features make north-western Tuscany prone to Deep-seated Gravitational Slope Deformations (DGSD...
The present work illustrates three cases of deep-seated gravitational slope deformation (DSGSD) in a...
Active faulting is one of the main factors that induce deep-seated gravitational slope deformations ...
Many areas of the Earth’s crust deform by distributed extensional faulting and the occurrence of ear...