A multi-disciplinary study of deformation of the basaltic cover over fine-grained valley fills: a case study from Eastern Sardinia, Italy
Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Deiana, Rita [verfasserIn] Dieni, Iginio [verfasserIn] Massari, Francesco [verfasserIn] Perri, Maria Teresa [verfasserIn] Rossi, Matteo [verfasserIn] Brovelli, Alessandro [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
Plio-Pleistocene basaltic plateau |
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| Übergeordnetes Werk: |
Enthalten in: Geologische Rundschau - Berlin : Springer, 1910, 105(2015), 4 vom: 01. Aug., Seite 1245-1255 |
|---|---|
| Übergeordnetes Werk: |
volume:105 ; year:2015 ; number:4 ; day:01 ; month:08 ; pages:1245-1255 |
| Links: |
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| DOI / URN: |
10.1007/s00531-015-1230-y |
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| Katalog-ID: |
SPR006726488 |
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| 520 | |a Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. The geophysical results, which demonstrate the existence of a disrupted layered system, were used to build a numerical geomechanical model that suggest the depressions originated by local collapses of the basaltic cover due to the compaction of the underlying fine-grained valley fills. | ||
| 650 | 4 | |a Plio-Pleistocene basaltic plateau |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Loading subsidence |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Electrical resistivity tomography |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Geomechanical modeling |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Dieni, Iginio |e verfasserin |4 aut | |
| 700 | 1 | |a Massari, Francesco |e verfasserin |4 aut | |
| 700 | 1 | |a Perri, Maria Teresa |e verfasserin |4 aut | |
| 700 | 1 | |a Rossi, Matteo |e verfasserin |4 aut | |
| 700 | 1 | |a Brovelli, Alessandro |e verfasserin |4 aut | |
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10.1007/s00531-015-1230-y doi (DE-627)SPR006726488 (SPR)s00531-015-1230-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Deiana, Rita verfasserin aut A multi-disciplinary study of deformation of the basaltic cover over fine-grained valley fills: a case study from Eastern Sardinia, Italy 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. The geophysical results, which demonstrate the existence of a disrupted layered system, were used to build a numerical geomechanical model that suggest the depressions originated by local collapses of the basaltic cover due to the compaction of the underlying fine-grained valley fills. Plio-Pleistocene basaltic plateau (dpeaa)DE-He213 Loading subsidence (dpeaa)DE-He213 Electrical resistivity tomography (dpeaa)DE-He213 Geomechanical modeling (dpeaa)DE-He213 Dieni, Iginio verfasserin aut Massari, Francesco verfasserin aut Perri, Maria Teresa verfasserin aut Rossi, Matteo verfasserin aut Brovelli, Alessandro verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 105(2015), 4 vom: 01. Aug., Seite 1245-1255 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:105 year:2015 number:4 day:01 month:08 pages:1245-1255 https://dx.doi.org/10.1007/s00531-015-1230-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 105 2015 4 01 08 1245-1255 |
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10.1007/s00531-015-1230-y doi (DE-627)SPR006726488 (SPR)s00531-015-1230-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Deiana, Rita verfasserin aut A multi-disciplinary study of deformation of the basaltic cover over fine-grained valley fills: a case study from Eastern Sardinia, Italy 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. The geophysical results, which demonstrate the existence of a disrupted layered system, were used to build a numerical geomechanical model that suggest the depressions originated by local collapses of the basaltic cover due to the compaction of the underlying fine-grained valley fills. Plio-Pleistocene basaltic plateau (dpeaa)DE-He213 Loading subsidence (dpeaa)DE-He213 Electrical resistivity tomography (dpeaa)DE-He213 Geomechanical modeling (dpeaa)DE-He213 Dieni, Iginio verfasserin aut Massari, Francesco verfasserin aut Perri, Maria Teresa verfasserin aut Rossi, Matteo verfasserin aut Brovelli, Alessandro verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 105(2015), 4 vom: 01. Aug., Seite 1245-1255 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:105 year:2015 number:4 day:01 month:08 pages:1245-1255 https://dx.doi.org/10.1007/s00531-015-1230-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 105 2015 4 01 08 1245-1255 |
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10.1007/s00531-015-1230-y doi (DE-627)SPR006726488 (SPR)s00531-015-1230-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Deiana, Rita verfasserin aut A multi-disciplinary study of deformation of the basaltic cover over fine-grained valley fills: a case study from Eastern Sardinia, Italy 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. The geophysical results, which demonstrate the existence of a disrupted layered system, were used to build a numerical geomechanical model that suggest the depressions originated by local collapses of the basaltic cover due to the compaction of the underlying fine-grained valley fills. Plio-Pleistocene basaltic plateau (dpeaa)DE-He213 Loading subsidence (dpeaa)DE-He213 Electrical resistivity tomography (dpeaa)DE-He213 Geomechanical modeling (dpeaa)DE-He213 Dieni, Iginio verfasserin aut Massari, Francesco verfasserin aut Perri, Maria Teresa verfasserin aut Rossi, Matteo verfasserin aut Brovelli, Alessandro verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 105(2015), 4 vom: 01. Aug., Seite 1245-1255 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:105 year:2015 number:4 day:01 month:08 pages:1245-1255 https://dx.doi.org/10.1007/s00531-015-1230-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 105 2015 4 01 08 1245-1255 |
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10.1007/s00531-015-1230-y doi (DE-627)SPR006726488 (SPR)s00531-015-1230-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Deiana, Rita verfasserin aut A multi-disciplinary study of deformation of the basaltic cover over fine-grained valley fills: a case study from Eastern Sardinia, Italy 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. The geophysical results, which demonstrate the existence of a disrupted layered system, were used to build a numerical geomechanical model that suggest the depressions originated by local collapses of the basaltic cover due to the compaction of the underlying fine-grained valley fills. Plio-Pleistocene basaltic plateau (dpeaa)DE-He213 Loading subsidence (dpeaa)DE-He213 Electrical resistivity tomography (dpeaa)DE-He213 Geomechanical modeling (dpeaa)DE-He213 Dieni, Iginio verfasserin aut Massari, Francesco verfasserin aut Perri, Maria Teresa verfasserin aut Rossi, Matteo verfasserin aut Brovelli, Alessandro verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 105(2015), 4 vom: 01. Aug., Seite 1245-1255 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:105 year:2015 number:4 day:01 month:08 pages:1245-1255 https://dx.doi.org/10.1007/s00531-015-1230-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 105 2015 4 01 08 1245-1255 |
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10.1007/s00531-015-1230-y doi (DE-627)SPR006726488 (SPR)s00531-015-1230-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Deiana, Rita verfasserin aut A multi-disciplinary study of deformation of the basaltic cover over fine-grained valley fills: a case study from Eastern Sardinia, Italy 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. The geophysical results, which demonstrate the existence of a disrupted layered system, were used to build a numerical geomechanical model that suggest the depressions originated by local collapses of the basaltic cover due to the compaction of the underlying fine-grained valley fills. Plio-Pleistocene basaltic plateau (dpeaa)DE-He213 Loading subsidence (dpeaa)DE-He213 Electrical resistivity tomography (dpeaa)DE-He213 Geomechanical modeling (dpeaa)DE-He213 Dieni, Iginio verfasserin aut Massari, Francesco verfasserin aut Perri, Maria Teresa verfasserin aut Rossi, Matteo verfasserin aut Brovelli, Alessandro verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 105(2015), 4 vom: 01. Aug., Seite 1245-1255 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:105 year:2015 number:4 day:01 month:08 pages:1245-1255 https://dx.doi.org/10.1007/s00531-015-1230-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 105 2015 4 01 08 1245-1255 |
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This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. 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A multi-disciplinary study of deformation of the basaltic cover over fine-grained valley fills: a case study from Eastern Sardinia, Italy |
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Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. The geophysical results, which demonstrate the existence of a disrupted layered system, were used to build a numerical geomechanical model that suggest the depressions originated by local collapses of the basaltic cover due to the compaction of the underlying fine-grained valley fills. |
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Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. The geophysical results, which demonstrate the existence of a disrupted layered system, were used to build a numerical geomechanical model that suggest the depressions originated by local collapses of the basaltic cover due to the compaction of the underlying fine-grained valley fills. |
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Abstract The Pliocene to Early Pleistocene volcanic activity which generated the basaltic plateau of the Orosei-Dorgali area in Eastern Sardinia led to the disruption of the local hydrographic network by damming some tracts of the fluvial valleys incised in the granite basement. This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. The geophysical results, which demonstrate the existence of a disrupted layered system, were used to build a numerical geomechanical model that suggest the depressions originated by local collapses of the basaltic cover due to the compaction of the underlying fine-grained valley fills. |
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This resulted in the formation of lacustrine basins, whose fine-grained fills were partly interfingered and eventually covered by younger lava flows. In the SW part of the plateau, close to the Galtellì village, a number of unknown depressions, locally named “Paules,” were formed. In order to reconstruct their subsurface structure, two electrical resistivity tomography surveys were carried out across these depressions. 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