Zobrazeno 1 - 2
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pro vyhledávání: '"Benvenuti M.[3]"'
Autor:
Nirta G.[1], Vittori E.[1, Blumetti A.M.[2], Di Manna P.[2], Benvenuti M.[3], Montanari D.[1], Perini M.[4], Fiera F.[4], Moratti G.[1], Baglione M.[5], Piccardi L. [1]
Publikováno v:
Geomorphology (Amst.) 374 (2021). doi:10.1016/j.geomorph.2020.107486
info:cnr-pdr/source/autori:Nirta G.[1], Vittori E.[1,2], Blumetti A.M.[2], Di Manna P.[2], Benvenuti M.[3], Montanari D.[1], Perini M.[4], Fiera F.[4], Moratti G.[1], Baglione M.[5], Piccardi L. [1]/titolo:Geomorphological and paleoseismological evidence of capable faulting in the Northern Apennines (Italy): Insights into active tectonics and seismic hazard of the Lunigiana basin/doi:10.1016%2Fj.geomorph.2020.107486/rivista:Geomorphology (Amst.)/anno:2021/pagina_da:/pagina_a:/intervallo_pagine:/volume:374
info:cnr-pdr/source/autori:Nirta G.[1], Vittori E.[1,2], Blumetti A.M.[2], Di Manna P.[2], Benvenuti M.[3], Montanari D.[1], Perini M.[4], Fiera F.[4], Moratti G.[1], Baglione M.[5], Piccardi L. [1]/titolo:Geomorphological and paleoseismological evidence of capable faulting in the Northern Apennines (Italy): Insights into active tectonics and seismic hazard of the Lunigiana basin/doi:10.1016%2Fj.geomorph.2020.107486/rivista:Geomorphology (Amst.)/anno:2021/pagina_da:/pagina_a:/intervallo_pagine:/volume:374
The Lunigiana basin is a NW trending tectonic depression located in the Northern Apennines of Italy. The basin is bounded by active normal faults, characterized by moderate to strong seismicity, with historical earthquakes reaching up to magnitude 6
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b3385292bea8e727881e6179ab4f3126
http://www.cnr.it/prodotto/i/443767
http://www.cnr.it/prodotto/i/443767
Publikováno v:
Applied geochemistry 87 (2017): 176–187. doi:10.1016/j.apgeochem.2017.10.024
info:cnr-pdr/source/autori:Morelli G.[1,2], Rimondi V.[2], Benvenuti M.[3], Medas D.[4], Costagliola P.[3], Gasparon M.[1]/titolo:Experimental simulation of arsenic desorption from Quaternary aquifer sediments following sea water intrusion/doi:10.1016%2Fj.apgeochem.2017.10.024/rivista:Applied geochemistry/anno:2017/pagina_da:176/pagina_a:187/intervallo_pagine:176–187/volume:87
info:cnr-pdr/source/autori:Morelli G.[1,2], Rimondi V.[2], Benvenuti M.[3], Medas D.[4], Costagliola P.[3], Gasparon M.[1]/titolo:Experimental simulation of arsenic desorption from Quaternary aquifer sediments following sea water intrusion/doi:10.1016%2Fj.apgeochem.2017.10.024/rivista:Applied geochemistry/anno:2017/pagina_da:176/pagina_a:187/intervallo_pagine:176–187/volume:87
Alluvial sediments from the coastal area in southern Tuscany (Italy) characterized by a significant As anomaly (As >500 mg/kg) are subjected to seawater intrusion due to groundwater exploitation. Sequential extractions and kinetic experiments were ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b7488f6026435c150cec7aea7b73c215