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Publikováno v:
Italian Journal of Geosciences. :715-721
The Ponticello formation is represented by a siliciclastic and calciclastic sedimentary succession, outcropping in the campanian sector of the Southern Apennines, and structured in four main sequences (lithozones). A transition interval is localized
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::886ce1834bd882debe8bb6768abaf65b
https://doi.org/10.3301/ijg.2009.128.3.715
https://doi.org/10.3301/ijg.2009.128.3.715
