Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Elisabetta Zizzo"'
Autor:
Attilio Sulli, Marilena Calarco, Mauro Agate, Ludovico Albano, Alessandro Bosman, Giuseppe Di Grigoli, Francesco Gargano, Valeria Lo Presti, Eleonora Martorelli, Valentina Pennino, Andrea Sposato, Elisabetta Zizzo, Giusy Anzelmo, Alessandro Bonfardeci, Daniele Casalbore, Gaspare Ciaccio, Aida Maria Conte, Michela Ingrassia, Sara Innangi, Francesco Interbartolo, Erika Lai, Claudio Lo Iacono, Maurizio Gasparo Morticelli, Carlo Luzzu, Paolo Emanuele Orrù, Fabrizio Pepe, Martina Pierdomenico, Claudia Romagnoli, Daniele Spatola, Francesco Latino Chiocci
Publikováno v:
Journal of Maps, Vol 20, Iss 1 (2024)
ABSTRACTWe present maps of geohazard features identified across north-western Sicily and Pantelleria in the framework of the Magic project (MArine Geohazard along Italian Coasts), which involved Italian marine geological researchers in 2007-2013. The
Externí odkaz:
https://doaj.org/article/37dc02b70d244d26832c311a80fa0490
Autor:
Maurizio Gasparo Morticelli, Elisabetta Zizzo, Attilio Sulli, Fabrizio Pepe, Daniele Spatola, Claudio Lo Iacono, Gaspare Ciaccio, Mauro Agate, Francesco Gargano
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
18 pages, 13 figures, 1 table
We present here for the first time a morpho-structural study of the submarine sector of the Ustica volcanic edifice, located in the south-western Tyrrhenian Sea, considered as an inactive volcanic system, middle Ple
We present here for the first time a morpho-structural study of the submarine sector of the Ustica volcanic edifice, located in the south-western Tyrrhenian Sea, considered as an inactive volcanic system, middle Ple
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::863a7a95595529a74795028003d4d7bc
http://hdl.handle.net/10261/239406
http://hdl.handle.net/10261/239406
A three-stage evolution has characterized the Sicilian Fold and Thrust Belt (SFTB) during the last 15 My: two main thin-skinned shortening events involving mainly Meso-Cenozoic carbonate units, followed by thick-skinned thrusting involving Plio-Pleis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89564ddbdb095a2921342b86b94210bd
http://hdl.handle.net/10447/479476
http://hdl.handle.net/10447/479476
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
Digital.CSIC: Repositorio Institucional del CSIC
Consejo Superior de Investigaciones Científicas (CSIC)
Journal of Maps, Vol 17, Iss 3, Pp 185-196 (2021)
instname
Digital.CSIC: Repositorio Institucional del CSIC
Consejo Superior de Investigaciones Científicas (CSIC)
Journal of Maps, Vol 17, Iss 3, Pp 185-196 (2021)
Geomorphological Tools for Mapping Natural Hazards.-- 12 pages, 7 figures, supplemental material https://doi.org/10.1080/17445647.2020.1866703.-- Software: The geomorphological main map and the Figures in the text were compiled using GLOBAL MAPPER, S
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9cf35424ba695eecb5dfa770a7b88db5
http://hdl.handle.net/10261/248257
http://hdl.handle.net/10261/248257
Publikováno v:
The Structural Geology Contribution to the Africa-Eurasia Geology: Basement and Reservoir Structure, Ore Mineralisation and Tectonic Modelling ISBN: 9783030014544
The Sicilian Fold and Thrust Belt developed during Neogene-Quaternary times characterized by main African-wards tectonic transport direction. Recent investigations highlighted extensive hinterland-verging tectonic structures active during late Plioce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b4347c0cff7f7737866e7d0ed51fa6d1
https://doi.org/10.1007/978-3-030-01455-1_54
https://doi.org/10.1007/978-3-030-01455-1_54
Backthrusting, nappe refolding, and normal faulting frequently characterize late collisional stage of an orogen. Shortening driven by backthrusting is widely reported in the Alpine orogen, and it has been proposed to be responsible for the increase o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::b64ba61fb9b5c1d82336984e5199f8f0
http://hdl.handle.net/10447/359217
http://hdl.handle.net/10447/359217
Autor:
Enrico Di Stefano, P. Graham Mortyn, Mattia Vallefuoco, Giorgio Tranchida, Elisabetta Zizzo, Rodolfo Sprovieri, Mario Sprovieri, Alessandro Incarbona, Luigi Giaramita, Renato Tonielli, Attilio Sulli, Serena Ferraro
Publikováno v:
Geo-marine letters 38 (2018): 241–258. doi:10.1007/s00367-018-0534-x
info:cnr-pdr/source/autori:Ferraro S.; Sulli A.; Di Stefano E.; Giaramita L.; Incarbona A.; Graham Mortyn P.; Sprovieri M.; Sprovieri R.; Tonielli R.; Vallefuoco M.; Zizzo E.; Tranchida G./titolo:Late Quaternary palaeoenvironmental reconstruction of sediment drift accumulation in the Malta Graben (central Mediterranean Sea)/doi:10.1007%2Fs00367-018-0534-x/rivista:Geo-marine letters/anno:2018/pagina_da:241/pagina_a:258/intervallo_pagine:241–258/volume:38
info:cnr-pdr/source/autori:Ferraro S.; Sulli A.; Di Stefano E.; Giaramita L.; Incarbona A.; Graham Mortyn P.; Sprovieri M.; Sprovieri R.; Tonielli R.; Vallefuoco M.; Zizzo E.; Tranchida G./titolo:Late Quaternary palaeoenvironmental reconstruction of sediment drift accumulation in the Malta Graben (central Mediterranean Sea)/doi:10.1007%2Fs00367-018-0534-x/rivista:Geo-marine letters/anno:2018/pagina_da:241/pagina_a:258/intervallo_pagine:241–258/volume:38
The Malta Graben is a deep tectonic depression in the Sicily Channel, bounded by NW-SE normal faults and filled by thick Pliocene-Quaternary deposits. A previous analysis of a giant piston core (LC09) from the Malta Graben had revealed a wide range o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76ef92f97f6f37ad55f638f8ca9305fe
http://hdl.handle.net/10447/289759
http://hdl.handle.net/10447/289759
The North Sicily continental margin is a very active region located in the Central Mediterranean. Strong seismicity, active tectonics and volcanism, fluid escape, high sediment supply, and widespread mass movements historically have exposed this regi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6a982b29f424553783119531e014b243
http://hdl.handle.net/10447/296847
http://hdl.handle.net/10447/296847
Publikováno v:
Atlas of Bedforms in the Western Mediterranean ISBN: 9783319339382
Multibeam bathymetric data revealed the occurrence of atrain of bedforms along a gully system in the Gulf of Palermo, Southern Tyrrhenian Sea. The observed gullies, located in the westernmost sector of the Gulf of Palermo, incise the outer shelf at a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::87c21722018e9bc0c368ffa7b770b702
https://doi.org/10.1007/978-3-319-33940-5_36
https://doi.org/10.1007/978-3-319-33940-5_36
Palermo is a populous city situated on the northern coast of Sicily, bordered by the Tyrrhenian Sea. This central part of the Mediterranean Sea features dramatic bathymetry, numerous subaqueous landslides and is also the epicentre to many subaqueous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::96f7ab79f91f348c0d499276a71bd49f
http://hdl.handle.net/10447/428426
http://hdl.handle.net/10447/428426