Tectonics and crustal structure of the Campania continental margin: relationships with volcanism
Summary ¶The crustal structure of the Campania continental margin is synthesized from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geological data reveal the presence of NE–SW faults, E–W faults and NW–SE faults. An older extensional event occurred along NW–SE faults and...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Milia, A. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2003 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag/Wien 2003 |
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| Übergeordnetes Werk: |
Enthalten in: Mineralogy and petrology - Springer-Verlag, 1987, 79(2003), 1-2 vom: Okt., Seite 33-47 |
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| Übergeordnetes Werk: |
volume:79 ; year:2003 ; number:1-2 ; month:10 ; pages:33-47 |
| Links: |
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| DOI / URN: |
10.1007/s00710-003-0005-5 |
|---|
| Katalog-ID: |
OLC206248366X |
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| 520 | |a Summary ¶The crustal structure of the Campania continental margin is synthesized from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geological data reveal the presence of NE–SW faults, E–W faults and NW–SE faults. An older extensional event occurred along NW–SE faults and was followed by the main extensional event linked to the activity of NE–SW normal faults. The latter were active between 700 and 400 ka producing half-grabens filled by more than 5 km of Quaternary deposits. The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by Middle Pleistocene rocks belonging to a transgressive-regressive cycle. A crustal section of the Campania margin displays an asymmetric linked fault system characterized by a 10–12 km-deep main detachment level, listric normal faults and rollover anticlines. Structural and stratigraphic data document that the inception of volcanic activity at Vesuvius occurred at 400 ka, just after the main extensional event, and the volcano is located at the margin of a rollover anticline. | ||
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10.1007/s00710-003-0005-5 doi (DE-627)OLC206248366X (DE-He213)s00710-003-0005-5-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Milia, A. verfasserin aut Tectonics and crustal structure of the Campania continental margin: relationships with volcanism 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag/Wien 2003 Summary ¶The crustal structure of the Campania continental margin is synthesized from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geological data reveal the presence of NE–SW faults, E–W faults and NW–SE faults. An older extensional event occurred along NW–SE faults and was followed by the main extensional event linked to the activity of NE–SW normal faults. The latter were active between 700 and 400 ka producing half-grabens filled by more than 5 km of Quaternary deposits. The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by Middle Pleistocene rocks belonging to a transgressive-regressive cycle. A crustal section of the Campania margin displays an asymmetric linked fault system characterized by a 10–12 km-deep main detachment level, listric normal faults and rollover anticlines. Structural and stratigraphic data document that the inception of volcanic activity at Vesuvius occurred at 400 ka, just after the main extensional event, and the volcano is located at the margin of a rollover anticline. Pleistocene Normal Fault Crustal Structure Seismic Reflection Extensional Event Torrente, M. M. aut Russo, M. aut Zuppetta, A. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 79(2003), 1-2 vom: Okt., Seite 33-47 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:79 year:2003 number:1-2 month:10 pages:33-47 https://doi.org/10.1007/s00710-003-0005-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4306 TE 1000 AR 79 2003 1-2 10 33-47 |
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10.1007/s00710-003-0005-5 doi (DE-627)OLC206248366X (DE-He213)s00710-003-0005-5-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Milia, A. verfasserin aut Tectonics and crustal structure of the Campania continental margin: relationships with volcanism 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag/Wien 2003 Summary ¶The crustal structure of the Campania continental margin is synthesized from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geological data reveal the presence of NE–SW faults, E–W faults and NW–SE faults. An older extensional event occurred along NW–SE faults and was followed by the main extensional event linked to the activity of NE–SW normal faults. The latter were active between 700 and 400 ka producing half-grabens filled by more than 5 km of Quaternary deposits. The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by Middle Pleistocene rocks belonging to a transgressive-regressive cycle. A crustal section of the Campania margin displays an asymmetric linked fault system characterized by a 10–12 km-deep main detachment level, listric normal faults and rollover anticlines. Structural and stratigraphic data document that the inception of volcanic activity at Vesuvius occurred at 400 ka, just after the main extensional event, and the volcano is located at the margin of a rollover anticline. Pleistocene Normal Fault Crustal Structure Seismic Reflection Extensional Event Torrente, M. M. aut Russo, M. aut Zuppetta, A. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 79(2003), 1-2 vom: Okt., Seite 33-47 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:79 year:2003 number:1-2 month:10 pages:33-47 https://doi.org/10.1007/s00710-003-0005-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4306 TE 1000 AR 79 2003 1-2 10 33-47 |
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10.1007/s00710-003-0005-5 doi (DE-627)OLC206248366X (DE-He213)s00710-003-0005-5-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Milia, A. verfasserin aut Tectonics and crustal structure of the Campania continental margin: relationships with volcanism 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag/Wien 2003 Summary ¶The crustal structure of the Campania continental margin is synthesized from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geological data reveal the presence of NE–SW faults, E–W faults and NW–SE faults. An older extensional event occurred along NW–SE faults and was followed by the main extensional event linked to the activity of NE–SW normal faults. The latter were active between 700 and 400 ka producing half-grabens filled by more than 5 km of Quaternary deposits. The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by Middle Pleistocene rocks belonging to a transgressive-regressive cycle. A crustal section of the Campania margin displays an asymmetric linked fault system characterized by a 10–12 km-deep main detachment level, listric normal faults and rollover anticlines. Structural and stratigraphic data document that the inception of volcanic activity at Vesuvius occurred at 400 ka, just after the main extensional event, and the volcano is located at the margin of a rollover anticline. Pleistocene Normal Fault Crustal Structure Seismic Reflection Extensional Event Torrente, M. M. aut Russo, M. aut Zuppetta, A. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 79(2003), 1-2 vom: Okt., Seite 33-47 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:79 year:2003 number:1-2 month:10 pages:33-47 https://doi.org/10.1007/s00710-003-0005-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4306 TE 1000 AR 79 2003 1-2 10 33-47 |
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10.1007/s00710-003-0005-5 doi (DE-627)OLC206248366X (DE-He213)s00710-003-0005-5-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Milia, A. verfasserin aut Tectonics and crustal structure of the Campania continental margin: relationships with volcanism 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag/Wien 2003 Summary ¶The crustal structure of the Campania continental margin is synthesized from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geological data reveal the presence of NE–SW faults, E–W faults and NW–SE faults. An older extensional event occurred along NW–SE faults and was followed by the main extensional event linked to the activity of NE–SW normal faults. The latter were active between 700 and 400 ka producing half-grabens filled by more than 5 km of Quaternary deposits. The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by Middle Pleistocene rocks belonging to a transgressive-regressive cycle. A crustal section of the Campania margin displays an asymmetric linked fault system characterized by a 10–12 km-deep main detachment level, listric normal faults and rollover anticlines. Structural and stratigraphic data document that the inception of volcanic activity at Vesuvius occurred at 400 ka, just after the main extensional event, and the volcano is located at the margin of a rollover anticline. Pleistocene Normal Fault Crustal Structure Seismic Reflection Extensional Event Torrente, M. M. aut Russo, M. aut Zuppetta, A. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 79(2003), 1-2 vom: Okt., Seite 33-47 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:79 year:2003 number:1-2 month:10 pages:33-47 https://doi.org/10.1007/s00710-003-0005-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4306 TE 1000 AR 79 2003 1-2 10 33-47 |
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550 VZ 13 ssgn TE 1000 VZ rvk Tectonics and crustal structure of the Campania continental margin: relationships with volcanism Pleistocene Normal Fault Crustal Structure Seismic Reflection Extensional Event |
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Tectonics and crustal structure of the Campania continental margin: relationships with volcanism |
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Milia, A. Torrente, M. M. Russo, M. Zuppetta, A. |
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tectonics and crustal structure of the campania continental margin: relationships with volcanism |
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Tectonics and crustal structure of the Campania continental margin: relationships with volcanism |
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Summary ¶The crustal structure of the Campania continental margin is synthesized from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geological data reveal the presence of NE–SW faults, E–W faults and NW–SE faults. An older extensional event occurred along NW–SE faults and was followed by the main extensional event linked to the activity of NE–SW normal faults. The latter were active between 700 and 400 ka producing half-grabens filled by more than 5 km of Quaternary deposits. The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by Middle Pleistocene rocks belonging to a transgressive-regressive cycle. A crustal section of the Campania margin displays an asymmetric linked fault system characterized by a 10–12 km-deep main detachment level, listric normal faults and rollover anticlines. Structural and stratigraphic data document that the inception of volcanic activity at Vesuvius occurred at 400 ka, just after the main extensional event, and the volcano is located at the margin of a rollover anticline. © Springer-Verlag/Wien 2003 |
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Summary ¶The crustal structure of the Campania continental margin is synthesized from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geological data reveal the presence of NE–SW faults, E–W faults and NW–SE faults. An older extensional event occurred along NW–SE faults and was followed by the main extensional event linked to the activity of NE–SW normal faults. The latter were active between 700 and 400 ka producing half-grabens filled by more than 5 km of Quaternary deposits. The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by Middle Pleistocene rocks belonging to a transgressive-regressive cycle. A crustal section of the Campania margin displays an asymmetric linked fault system characterized by a 10–12 km-deep main detachment level, listric normal faults and rollover anticlines. Structural and stratigraphic data document that the inception of volcanic activity at Vesuvius occurred at 400 ka, just after the main extensional event, and the volcano is located at the margin of a rollover anticline. © Springer-Verlag/Wien 2003 |
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Summary ¶The crustal structure of the Campania continental margin is synthesized from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geological data reveal the presence of NE–SW faults, E–W faults and NW–SE faults. An older extensional event occurred along NW–SE faults and was followed by the main extensional event linked to the activity of NE–SW normal faults. The latter were active between 700 and 400 ka producing half-grabens filled by more than 5 km of Quaternary deposits. The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by Middle Pleistocene rocks belonging to a transgressive-regressive cycle. A crustal section of the Campania margin displays an asymmetric linked fault system characterized by a 10–12 km-deep main detachment level, listric normal faults and rollover anticlines. Structural and stratigraphic data document that the inception of volcanic activity at Vesuvius occurred at 400 ka, just after the main extensional event, and the volcano is located at the margin of a rollover anticline. © Springer-Verlag/Wien 2003 |
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