Multi-phase reactivations and inversions of Paleozoic–Mesozoic extensional basins during the Wilson cycle: case studies from the North Sea (UK) and the Northern Apennines (Italy)
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| Názov: | Multi-phase reactivations and inversions of Paleozoic–Mesozoic extensional basins during the Wilson cycle: case studies from the North Sea (UK) and the Northern Apennines (Italy) |
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| Autori: | Scisciani, Vittorio, Patruno, Stefano, Tavarnelli, Enrico, Calamita, Fernando, Pace, Paolo, Iacopini, David |
| Prispievatelia: | Wilson, RW, Houseman, GA, McCaffrey, KJW, Dore, AG, Buiter, SJH, Scisciani, V., Patruno, S., Tavarnelli, Enrico, Calamita, F., Pace, P., Iacopini, D. |
| Zdroj: | Geological Society, London, Special Publications. 470:205-243 |
| Informácie o vydavateľovi: | Geological Society of London, 2019. |
| Rok vydania: | 2019 |
| Predmety: | Northern Apennines (Italy), 13. Climate action, Paleozoic-Mesozoic extensional basin, positive and negative inversion, Wilson cycle, North Sea (UK), Paleozoic-Mesozoic extensional basins, 01 natural sciences, 0105 earth and related environmental sciences |
| Popis: | The Caledonian and Variscan orogens in northern Europe and the Alpine-age Apennine range in Italy are classic examples of thrust belts that were developed at the expense of formerly rifted, passive continental margins that subsequently experienced various degrees of post-orogenic collapse and extension. The outer zones of orogenic belts, and their adjoining foreland domains and regions, where the effects of superposed deformations are mild to very mild make it possible to recognize and separate structures produced at different times and to correctly establish their chronology and relationships. In this paper we integrate subsurface data (2D and 3D seismic reflection and well logs), mainly from the North Sea, and structural field evidence, mainly from the Apennines, with the aim of reconstructing and refining the structural evolution of these two provinces which, in spite of their different ages and present-day structural framework, share repeated pulses of alternating extension and compression. The main outcome of this investigation is that in both scenarios, during repeated episodes of inversion that are a characteristic feature of the Wilson cycle, inherited basement structures were effective in controlling stress localization along faults affecting younger sedimentary cover rocks. |
| Druh dokumentu: | Article Part of book or chapter of book |
| Popis súboru: | application/pdf; STAMPA |
| Jazyk: | English |
| ISSN: | 2041-4927 0305-8719 |
| DOI: | 10.1144/sp470-2017-232 |
| Prístupová URL adresa: | http://hdl.handle.net/11588/762939 https://sp.lyellcollection.org/online-first/470 https://usiena-air.unisi.it/handle/11365/1080680 https://abdn.pure.elsevier.com/en/publications/multi-phase-reactivations-and-inversions-of-paleozoicmesozoic-ext https://www.iris.unina.it/handle/11588/762939 https://pubs.geoscienceworld.org/books/book/2211/chapter/123620418/Multi-phase-reactivations-and-inversions-of http://ui.adsabs.harvard.edu/abs/2019GSLSP.470..205S/abstract https://hdl.handle.net/11564/712691 https://doi.org/10.1144/SP470-2017-232 https://sp.lyellcollection.org/content/470/1/1 https://hdl.handle.net/11588/762939 https://doi.org/10.1144/SP470-2017-232 https://sp.lyellcollection.org/online-first/470 |
| Rights: | STM Policy #2 CC 0 |
| Prístupové číslo: | edsair.doi.dedup.....1a0781050b73e0a09032b9836f23e75d |
| Databáza: | OpenAIRE |
Nájsť tento článok vo Web of Science | Abstrakt: | The Caledonian and Variscan orogens in northern Europe and the Alpine-age Apennine range in Italy are classic examples of thrust belts that were developed at the expense of formerly rifted, passive continental margins that subsequently experienced various degrees of post-orogenic collapse and extension. The outer zones of orogenic belts, and their adjoining foreland domains and regions, where the effects of superposed deformations are mild to very mild make it possible to recognize and separate structures produced at different times and to correctly establish their chronology and relationships. In this paper we integrate subsurface data (2D and 3D seismic reflection and well logs), mainly from the North Sea, and structural field evidence, mainly from the Apennines, with the aim of reconstructing and refining the structural evolution of these two provinces which, in spite of their different ages and present-day structural framework, share repeated pulses of alternating extension and compression. The main outcome of this investigation is that in both scenarios, during repeated episodes of inversion that are a characteristic feature of the Wilson cycle, inherited basement structures were effective in controlling stress localization along faults affecting younger sedimentary cover rocks. |
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| ISSN: | 20414927 03058719 |
| DOI: | 10.1144/sp470-2017-232 |