Le Massif du Taburno-Camposauro, une montagne calcaire en position de charnière à l'échelle de l'Apennin méridional (Italie du Sud)
The Taburno-Camposauro limestone faulted block has a key location between tyrrhenian and adriatic sides of the Southern Apennines, because of the relief disruption due to extensional Plio-Pleistocene neotectonics. From this, results a contrasted landscape, with prior gentle erosional landsurfaces (U...
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Physio-Géo
2010-03-01
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| Series: | Physio-Géo |
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| Online Access: | https://journals.openedition.org/physio-geo/1090 |
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| author | Bruno Comentale |
| author_facet | Bruno Comentale |
| author_sort | Bruno Comentale |
| collection | DOAJ |
| description | The Taburno-Camposauro limestone faulted block has a key location between tyrrhenian and adriatic sides of the Southern Apennines, because of the relief disruption due to extensional Plio-Pleistocene neotectonics. From this, results a contrasted landscape, with prior gentle erosional landsurfaces (Upper Miocene-Early Pliocene?) subsequently disrupted by huge fault scarps. After a microtectonic analysis along these fault scarps, also considering the deformation of breccia – which are regarded as genetically linked with the erosional landsurfaces shaping –, the discussion deals with the regional geomorphic pattern, mainly the nearest Matese mountain. |
| format | Article |
| id | doaj-art-b6016fccbd6e48c9acd0a18f821389c2 |
| institution | OA Journals |
| issn | 1958-573X |
| language | English |
| publishDate | 2010-03-01 |
| publisher | Physio-Géo |
| record_format | Article |
| series | Physio-Géo |
| spelling | doaj-art-b6016fccbd6e48c9acd0a18f821389c22025-08-20T02:37:54ZengPhysio-GéoPhysio-Géo1958-573X2010-03-014274210.4000/physio-geo.1090Le Massif du Taburno-Camposauro, une montagne calcaire en position de charnière à l'échelle de l'Apennin méridional (Italie du Sud)Bruno ComentaleThe Taburno-Camposauro limestone faulted block has a key location between tyrrhenian and adriatic sides of the Southern Apennines, because of the relief disruption due to extensional Plio-Pleistocene neotectonics. From this, results a contrasted landscape, with prior gentle erosional landsurfaces (Upper Miocene-Early Pliocene?) subsequently disrupted by huge fault scarps. After a microtectonic analysis along these fault scarps, also considering the deformation of breccia – which are regarded as genetically linked with the erosional landsurfaces shaping –, the discussion deals with the regional geomorphic pattern, mainly the nearest Matese mountain.https://journals.openedition.org/physio-geo/1090structural geomorphologyfault scarpspalaeotopographySouthern Italy |
| spellingShingle | Bruno Comentale Le Massif du Taburno-Camposauro, une montagne calcaire en position de charnière à l'échelle de l'Apennin méridional (Italie du Sud) Physio-Géo structural geomorphology fault scarps palaeotopography Southern Italy |
| title | Le Massif du Taburno-Camposauro, une montagne calcaire en position de charnière à l'échelle de l'Apennin méridional (Italie du Sud) |
| title_full | Le Massif du Taburno-Camposauro, une montagne calcaire en position de charnière à l'échelle de l'Apennin méridional (Italie du Sud) |
| title_fullStr | Le Massif du Taburno-Camposauro, une montagne calcaire en position de charnière à l'échelle de l'Apennin méridional (Italie du Sud) |
| title_full_unstemmed | Le Massif du Taburno-Camposauro, une montagne calcaire en position de charnière à l'échelle de l'Apennin méridional (Italie du Sud) |
| title_short | Le Massif du Taburno-Camposauro, une montagne calcaire en position de charnière à l'échelle de l'Apennin méridional (Italie du Sud) |
| title_sort | le massif du taburno camposauro une montagne calcaire en position de charniere a l echelle de l apennin meridional italie du sud |
| topic | structural geomorphology fault scarps palaeotopography Southern Italy |
| url | https://journals.openedition.org/physio-geo/1090 |
| work_keys_str_mv | AT brunocomentale lemassifdutaburnocamposaurounemontagnecalcaireenpositiondecharnierealechelledelapenninmeridionalitaliedusud |