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pro vyhledávání: '"Russo Ermolli E. [6]"'
Autor:
Amato V. [1], Aucelli P. [2], D'Argenio B. [3], Da Prato S. [4], Ferraro L. [3], Pappone G.[2], Petrosino P. [5], Rosskopf C. [1], Russo Ermolli E. [6]
Publikováno v:
Rendiconti lincei. Scienze fisiche e naturali 23 (2012): 45–59.
info:cnr-pdr/source/autori:Amato V. [1]; Aucelli P. [2]; D'Argenio B. [3]; Da Prato S. [4]; Ferraro L. [3]; Pappone G.[2]; Petrosino P. [5]; Rosskopf C. [1]; Russo Ermolli E. [6]/titolo:Holeocene environmental evolution of the coastal sector in front of the Poseidonia-Paestum archeological area (Sele plain, southern Italy)./doi:/rivista:Rendiconti lincei. Scienze fisiche e naturali/anno:2012/pagina_da:45/pagina_a:59/intervallo_pagine:45–59/volume:23
info:cnr-pdr/source/autori:Amato V. [1]; Aucelli P. [2]; D'Argenio B. [3]; Da Prato S. [4]; Ferraro L. [3]; Pappone G.[2]; Petrosino P. [5]; Rosskopf C. [1]; Russo Ermolli E. [6]/titolo:Holeocene environmental evolution of the coastal sector in front of the Poseidonia-Paestum archeological area (Sele plain, southern Italy)./doi:/rivista:Rendiconti lincei. Scienze fisiche e naturali/anno:2012/pagina_da:45/pagina_a:59/intervallo_pagine:45–59/volume:23
The Sele river plain is located along the western Tyrrhenian margin of the southern Apennine Chain and is confined seaward by a straight sandy coast formed during the Last Interglacial and the Holocene. The coastal plain is characterised by beach-dun
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::3deaa51136369d2526555b7b4bd0e03e
https://publications.cnr.it/doc/208235
https://publications.cnr.it/doc/208235