Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Emy Fuffa"'
Publikováno v:
AIMS Geosciences, Vol 6, Iss 3, Pp 258-270 (2020)
In recent months, humanity, is experiencing a set of situations that have completely changed the existing balances, worldwide. The pandemic from COVID-19 brings the collective memory back to the terrible Spanish flu, thought to have infected a third
Externí odkaz:
https://doaj.org/article/42766d0d62664240956247a0a990f88b
Autor:
Domenico Aringoli, Piero Farabollini, Gilberto Pambianchi, Marco Materazzi, Margherita Bufalini, Emy Fuffa, Matteo Gentilucci, Gianni Scalella
Publikováno v:
Land, Vol 10, Iss 5, p 510 (2021)
In many areas of the Umbria-Marche Apennines, evident traces of huge landslides have been recognized; these probably occurred in the Upper Pleistocene and are conditioned by the tectonic-structural setting of the involved Meso-Cenozoic formations, in
Externí odkaz:
https://doaj.org/article/96acf907fa654ec7ab1c6b368ac7ca20
Autor:
Geomore srl, Sara Prati, Gilberto Pambianchi, Marco Materazzi, Maurizio Mainiero, Francesca Lugeri, Francesco Lampa, Matteo Gentilucci, Emy Fuffa, Roberto Cingolani, Margherita Bufalini, Fabrizio Bendia, Domenico Aringoli, Piero Farabollini
Publikováno v:
Rendiconti Online della Società Geologica Italiana. 58:28-33
Publikováno v:
AIMS Geosciences, Vol 6, Iss 3, Pp 258-270 (2020)
In recent months, humanity, is experiencing a set of situations that have completely changed the existing balances, worldwide. The pandemic from COVID-19 brings the collective memory back to the terrible Spanish flu, thought to have infected a third
Autor:
Marco Materazzi, Matteo Gentilucci, Gilberto Pambianchi, Emy Fuffa, Domenico Aringoli, G. Scalella, Piero Farabollini, Margherita Bufalini
Publikováno v:
Land, Vol 10, Iss 510, p 510 (2021)
Land
Volume 10
Issue 5
Land
Volume 10
Issue 5
In many areas of the Umbria-Marche Apennines, evident traces of huge landslides have been recognized
these probably occurred in the Upper Pleistocene and are conditioned by the tectonic-structural setting of the involved Meso-Cenozoic formations
these probably occurred in the Upper Pleistocene and are conditioned by the tectonic-structural setting of the involved Meso-Cenozoic formations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6f3b0bb6a7f13bd6050147784a55d813
http://hdl.handle.net/11581/452066
http://hdl.handle.net/11581/452066