Structural geology of the eastern termination of the Mt. Kumeta-Alcantara line (NE sicily, Italy)-Reference-Cited by-同舟云学术

Structural geology of the eastern termination of the Mt. Kumeta-Alcantara line (NE sicily, Italy)

Published:2023-02-23 Issue:1 Volume:19 Page:
ISSN:1744-5647
Container-title:Journal of Maps
language:en
Short-container-title:Journal of Maps

Author:

Foti Alessandro¹^ORCID,Pavano Francesco²^ORCID,Romagnoli Gino³^ORCID,Tortorici Giuseppe⁴^ORCID,Catalano Stefano¹²^ORCID

Affiliation:

1. Department of Biological, Geological and Environmental Sciences (DBGES) – Section of Earth Science, University of Catania, Catania, Italy

2. Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, PA, USA

3. Italian Institute for Environmental Protection and Research, ISPRA (Istituto Superiore per la Protezione e la Ricerca Ambientale), Roma, Italy

4. Institute of Environmental Geology and Geoengineering of the Italian National Research Council, Monterotondo, Roma, Italy

Funder

Ministero dell'UniversitÃ e della Ricerca

Publisher

Informa UK Limited

Subject

Earth and Planetary Sciences (miscellaneous),Geography, Planning and Development

Link

https://www.tandfonline.com/doi/pdf/10.1080/17445647.2023.2179436

Reference34 articles.

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2. Principali domini strutturali dalla collisione continentale Neogenico-Quaternaria nel Mediterraneo centrale;Ben Avraham Z.;Memorie della Società Geologica Italiana,1990

3. Incipient extension along the active convergent margin of Nubia in Sicily, Italy: Cefalù-Etna seismic zone

4. Seismological and structural constraints on the 2011-2013, Mmax 4.6 seismic sequence at the south-eastern edge of the Calabrian arc (North-eastern Sicily, Italy);Cammarata L.;Geomorphology,2018

5. Carbone S. Catalano S. Grasso M. Lentini F. & Monaco C. (1990). Carta geologica della Sicilia centro-orientale. Scala 1:50.000. S.EL.CA. Firenze.

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