Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Ciro Cerrone"'
Autor:
Mauro Bonasera, Ciro Cerrone, Fabiola Caso, Stefania Lanza, Giandomenico Fubelli, Giovanni Randazzo
Publikováno v:
Land, Vol 11, Iss 7, p 1106 (2022)
Capo Faro Promontory, located in Salina (Aeolian Islands, southern Italy), is a popular summer destination due to its volcanic morphologies, seaside, and enogastronomy. A flat area, right behind the scarp edge of a coastal cliff, hosts the Capo Faro
Externí odkaz:
https://doaj.org/article/fe43187ae27143de8fe996dce51ea1eb
The Neogene to Quaternary southern Apennines mountain belt is flanked to the SW by the Tyrrhenian Sea back-arc basin, which was formed since late Miocene times. Extensional tectonics related to back-arc basin formation affected the Tyrrhenian margin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ef778b7aa558c76f2d97b84f2009873
https://doi.org/10.5194/icg2022-540
https://doi.org/10.5194/icg2022-540
The complex interactions between the redistribution of water mass in the ocean basins due to continental ice sheet growth and decay, and the attendant Glacio-Isostatic Adjustment (GIA) process play a major role in controlling Relative Sea-Level (RSL)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aaae2a40d86108ac45ae1aadbb090b1f
https://doi.org/10.5194/icg2022-554
https://doi.org/10.5194/icg2022-554
The growth of a mountain chain results from a complex interplay between endogenous and exogenous processes. The former depends on the geodynamic setting and cause the uplift of the orogenic wedge whereas the latter tend to erode the uplifted topograp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66c7046077435d1e874688041cda1b53
https://doi.org/10.5194/icg2022-416
https://doi.org/10.5194/icg2022-416
An open access database containing raw data of Last Interglacial sea-level proxies for the Western Mediterranean has been compiled by reviewing hundreds of original published papers in accordance with the WALIS template (https://warmcoasts.eu/world-a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8b5c496ec072d69fe41828b8a3612ad
https://doi.org/10.5194/egusphere-egu21-13192
https://doi.org/10.5194/egusphere-egu21-13192
Autor:
Angela Mormone, Giuseppina Balassone, Alessandra Ascione, Ciro Cerrone, Paola Tuccimei, Michele Soligo, Gaetano Robustelli
New analyses of marine terraces in the Tyrrhenian Sea margin of Basilicata - northern Calabria (southern Italy) have been carried out. In the study area, c. 25 km in length, an impressive flight of marine terraces occurs, with the highest terraces re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8a97c46a24ea4046ab4be0e76ec287e9
http://hdl.handle.net/11588/859095
http://hdl.handle.net/11588/859095
Autor:
Ann-Kathrin Petersen, Deirdre D. Ryan, Thomas Felis, Thomas Lorscheid, Ciro Cerrone, Alessio Rovere, Paolo Stocchi, Karla Rubio-Sandoval
Publikováno v:
Earth System Science Data
Earth System Science Data, Vol 13, Pp 4819-4845 (2021)
Earth System Science Data, Vol 13, Pp 4819-4845 (2021)
We use a standardized template for Pleistocene sea-level data to review last interglacial (Marine Isotope Stage 5 – MIS 5) sea-level indicators along the coasts of the western Atlantic and southwestern Caribbean, on a transect spanning from Brazil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::15fc1af4a676229f0523dc120fe34e53
Autor:
Ciro Cerrone, Alessandra Ascione, Paola Tuccimei, Valentino Di Donato, Gaetano Robustelli, Michele Soligo, Stefano Mazzoli
Raised paleoshorelines were detected in the eastern margin of the Campania Plain, which is one of the largest coastal basins in the Tyrrhenian back-arc basin system associated with the Neogene to Quaternary Apennine orogen. The paleoshoreline remnant
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::578c4d7ea3967d5134c7f082e97eee8b
http://hdl.handle.net/11588/849475
http://hdl.handle.net/11588/849475