Zobrazeno 1 - 10
of 148
pro vyhledávání: '"Capezzuoli E."'
Publikováno v:
In Marine and Petroleum Geology May 2019 103:549-563
Akademický článek
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Akademický článek
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Publikováno v:
Sedimentology (Amst., Print) 69 (2022): 1519–1546. doi:10.1111/sed.12961
info:cnr-pdr/source/autori:Luo L.C. [1], Wen H.[2,3], Brogi A.[4,5], Capezzuoli E.[1]/titolo:Factors controlling the geometry of travertine mounds: Insights from Heinitang (China)/doi:10.1111%2Fsed.12961/rivista:Sedimentology (Amst., Print)/anno:2022/pagina_da:1519/pagina_a:1546/intervallo_pagine:1519–1546/volume:69
info:cnr-pdr/source/autori:Luo L.C. [1], Wen H.[2,3], Brogi A.[4,5], Capezzuoli E.[1]/titolo:Factors controlling the geometry of travertine mounds: Insights from Heinitang (China)/doi:10.1111%2Fsed.12961/rivista:Sedimentology (Amst., Print)/anno:2022/pagina_da:1519/pagina_a:1546/intervallo_pagine:1519–1546/volume:69
Travertine mounds are common spring-constructed landforms with highly variable geometries, but factors controlling their development have not yet been fully understood. To investigate processes linked with their lateral and vertical growth, this stud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d1a819aaf1e66a8e3c49de0de5cce8b
https://doi.org/10.1111/sed.12961
https://doi.org/10.1111/sed.12961
Publikováno v:
Geological magazine
159 (2022): 853–872. doi:10.1017/S0016756822000036
info:cnr-pdr/source/autori:Mirabella F.[1], Braun T.[2], Brogi A.[3,4], Capezzuoli E.[5]/titolo:Pliocene-Quaternary seismogenic faults in the inner Northern Apennines (Valdelsa Basin, southern Tuscany) and their role in controlling the local seismicity/doi:10.1017%2FS0016756822000036/rivista:Geological magazine (Print)/anno:2022/pagina_da:853/pagina_a:872/intervallo_pagine:853–872/volume:159
159 (2022): 853–872. doi:10.1017/S0016756822000036
info:cnr-pdr/source/autori:Mirabella F.[1], Braun T.[2], Brogi A.[3,4], Capezzuoli E.[5]/titolo:Pliocene-Quaternary seismogenic faults in the inner Northern Apennines (Valdelsa Basin, southern Tuscany) and their role in controlling the local seismicity/doi:10.1017%2FS0016756822000036/rivista:Geological magazine (Print)/anno:2022/pagina_da:853/pagina_a:872/intervallo_pagine:853–872/volume:159
Pliocene–Quaternary faults are relevant structures with which to constrain the seismotectonic context and contribute to the evaluation of the seismic hazard of a region. Many of these faults, however, do not show clear surface evidence even when re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ea7dc6e9208abfd844e6cb30cb6b19d4
http://hdl.handle.net/11391/1516930
http://hdl.handle.net/11391/1516930
Akademický článek
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Publikováno v:
Journal of the Geological Society (Online) (2019): 1262–1272. doi:10.1144/jgs2018-202
info:cnr-pdr/source/autori:Spina A.[1], Capezzuoli E.[2], Brogi A.[3,4], Cirilli S.[1], Liotta D.[3,4]/titolo:Mid-to late Permian microfloristic evidence in the metamorphic successions of the Northern Apennines: insights for ageconstraining and palaeogeographical correlations/doi:10.1144%2Fjgs2018-202/rivista:Journal of the Geological Society (Online)/anno:2019/pagina_da:1262/pagina_a:1272/intervallo_pagine:1262–1272/volume
info:cnr-pdr/source/autori:Spina A.[1], Capezzuoli E.[2], Brogi A.[3,4], Cirilli S.[1], Liotta D.[3,4]/titolo:Mid-to late Permian microfloristic evidence in the metamorphic successions of the Northern Apennines: insights for ageconstraining and palaeogeographical correlations/doi:10.1144%2Fjgs2018-202/rivista:Journal of the Geological Society (Online)/anno:2019/pagina_da:1262/pagina_a:1272/intervallo_pagine:1262–1272/volume
Recent studies on the stratigraphy of Paleozoic successions belonging to key sectors of the inner Northern Apennines provide data that can be used to propose new hypotheses about the palaeogeography of the western Mediterranean domain during post-Her
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7f0181b0a8b9baad36806347a942e90b
https://doi.org/10.1144/jgs2018-202
https://doi.org/10.1144/jgs2018-202
Autor:
Brogi A.[1, Caggianelli A.[1], Liotta D.[1, Zucchi M.[1], Spina A.[3], Capezzuoli E.[4], Casini A.[5, Buracchi E.[5
Publikováno v:
Geosciences
Volume 11
Issue 3
Geosciences, Vol 11, Iss 124, p 124 (2021)
Geosciences (Basel) 11 (2021): 1–30. doi:10.3390/geosciences11030124
info:cnr-pdr/source/autori:Brogi A.[1,2], Caggianelli A.[1], Liotta D.[1,2], Zucchi M.[1], Spina A.[3], Capezzuoli E.[4], Casini A.[5,6], Buracchi E.[5,6]/titolo:The Gavorrano Monzogranite (Northern Apennines): An Updated Review of Host Rock Protoliths, Thermal Metamorphism and Tectonic Setting./doi:10.3390%2Fgeosciences11030124/rivista:Geosciences (Basel)/anno:2021/pagina_da:1/pagina_a:30/intervallo_pagine:1–30/volume:11
Volume 11
Issue 3
Geosciences, Vol 11, Iss 124, p 124 (2021)
Geosciences (Basel) 11 (2021): 1–30. doi:10.3390/geosciences11030124
info:cnr-pdr/source/autori:Brogi A.[1,2], Caggianelli A.[1], Liotta D.[1,2], Zucchi M.[1], Spina A.[3], Capezzuoli E.[4], Casini A.[5,6], Buracchi E.[5,6]/titolo:The Gavorrano Monzogranite (Northern Apennines): An Updated Review of Host Rock Protoliths, Thermal Metamorphism and Tectonic Setting./doi:10.3390%2Fgeosciences11030124/rivista:Geosciences (Basel)/anno:2021/pagina_da:1/pagina_a:30/intervallo_pagine:1–30/volume:11
We review and refine the geological setting of an area located nearby the Tyrrhenian seacoast, in the inner zone of the Northern Apennines (southern Tuscany), where a Neogene monzogranite body (estimated in about 3 km long, 1.5 km wide, and 0.7 km th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6e2f2e00d598e2082b59ccd03639b64e
Autor:
Capezzuoli E.[1], Spina A.[2], Brogi A.[3, Liotta D.[3, Bagnoli G.[5], Zucchi M.[3], Molli G.[5], Regoli R.[6]
Publikováno v:
Geosciences, Vol 11, Iss 84, p 84 (2021)
Geosciences (Basel) 11 (2021): 1–24. doi:10.3390/geosciences11020084
info:cnr-pdr/source/autori:Capezzuoli E.[1], Spina A.[2], Brogi A.[3,4], Liotta D.[3,4], Bagnoli G.[5], Zucchi M.[3], Molli G.[5], Regoli R.[6]/titolo:Reconsidering the variscan basement of southern tuscany (inner northern apennines)/doi:10.3390%2Fgeosciences11020084/rivista:Geosciences (Basel)/anno:2021/pagina_da:1/pagina_a:24/intervallo_pagine:1–24/volume:11
Geosciences
Volume 11
Issue 2
Geosciences (Basel) 11 (2021): 1–24. doi:10.3390/geosciences11020084
info:cnr-pdr/source/autori:Capezzuoli E.[1], Spina A.[2], Brogi A.[3,4], Liotta D.[3,4], Bagnoli G.[5], Zucchi M.[3], Molli G.[5], Regoli R.[6]/titolo:Reconsidering the variscan basement of southern tuscany (inner northern apennines)/doi:10.3390%2Fgeosciences11020084/rivista:Geosciences (Basel)/anno:2021/pagina_da:1/pagina_a:24/intervallo_pagine:1–24/volume:11
Geosciences
Volume 11
Issue 2
The Pre-Mesozoic units exposed in the inner Northern Apennines mostly consist of middle-late Carboniferous-Permian successions unconformably deposited on a continental crust consolidated at the end of the Variscan (i.e. Hercynian) orogenic cycle (Sil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::568058b6c37632bd08c86a742f4cdcdf
https://www.mdpi.com/2076-3263/11/2/84
https://www.mdpi.com/2076-3263/11/2/84