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The authors regret the presence of incomplete information in the author affiliations (reported correctly above) and in the acknowledgments of the original article (provided in the amended version below). The authors are obliged to Mr. Vincenzo Manise
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::5140a371b5c559511f70d2cba43222b7
https://hdl.handle.net/11585/922484
https://hdl.handle.net/11585/922484
Autor:
Arriolabengoa, M, D’Angeli, I M, De Waele, J, Parise, M, Ruggieri, R, Sanna, L, Madonia, G, Vattano, M
Almost 20% of Italy is characterized by the outcropping of carbonate massifs ranging in age from Cambrian to Quaternary. Coastal karst is present in many Italian regions: from North-East to South and West: the Gulf of Trieste, the Conero (South of An
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::76dfa3852ef57550358c824916b94a6d
http://hdl.handle.net/11585/606211
http://hdl.handle.net/11585/606211
Italy is a country hosting a large number of hypogenic sulfuric acid (SAS) speleogenesis caves, mostly located along the Apennine chain, but also in Campania (along the coastline of Capo Palinuro), Apulia (along the coastline of Santa Cesarea Terme)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::44b1c9e0217d029f72507341191550b5
http://hdl.handle.net/10447/238907
http://hdl.handle.net/10447/238907
Autor:
Addesso, R., Baldantoni, D., Bellino, A., Vigliotta, G., De Waele, J., D’Angeli, I. M., Saiz-Jimenez, C., Miller, A. Z., Gonzalez-Pimentel, J. L., Jurado, V., Cubero, B., Carbone, C., Amato, M.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3666::54e46c8043829d74ce83ae07be3144fe
http://hdl.handle.net/11386/4715547
http://hdl.handle.net/11386/4715547
Autor:
D’Angeli I. M, Bontognali T. R. R, Tisato N, TUCCIMEI, Paola, Scholz D, Ginés J, Ginés A, Fornós J, Villa I. M, De Waele J., SOLIGO, Michele
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3668::a5a678b8d2c71a32f72d53284a0243e6
https://hdl.handle.net/11590/174820
https://hdl.handle.net/11590/174820
Autor:
Jean Claude Nobécourt, Philippe Audra, Ilenia M. D’Angeli, Jean-Yves Bigot, Jo De Waele, Marco Vattano, Ermanno Galli, Giuliana Madonia
Publikováno v:
Hypogene Karst Regions and Caves of the World ISBN: 9783319533476
Karst in Sicily develops in both Messinian gypsum and Mesozoic or Tertiary limestone rocks. Caves are also found in the basalts of Mount Etna. Except for some rare cases, until recently most caves developed in limestone were considered to be of epige
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a705b9217578819a5f7540c4219da806
http://hdl.handle.net/10447/240689
http://hdl.handle.net/10447/240689
Sulphuric acid speleogenesis (SAS) related to the upwelling of acid water enriched in H2S and CO2 represents an unusual way of cave development. Since meteoric infiltration waters are not necessarily involved in speleogenesis, caves can form without
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::2b74ea3e5ff7d532a7281312da8cee7d
http://hdl.handle.net/10447/243214
http://hdl.handle.net/10447/243214