Zobrazeno 1 - 10
of 77
pro vyhledávání: '"Claudio Scarpati"'
Publikováno v:
Scientific Reports, Vol 10, Iss 1, Pp 1-13 (2020)
Abstract Large ignimbrites are the product of devastating explosive eruptions that have repeatedly impacted climate and life on global scale. The assemblage of vertical and lateral lithofacies variations within an ignimbrite sheet, its internal archi
Externí odkaz:
https://doaj.org/article/ffd5f31950f1480f8559fd15d754800e
Autor:
Claudio Scarpati
Publikováno v:
Geologos. 29:65-67
Not provided.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b67c16bcf4c544193851563775ffdb5
https://doi.org/10.14746/logos.2023.29.1.07
https://doi.org/10.14746/logos.2023.29.1.07
Autor:
Claudio Scarpati
Publikováno v:
Geologos. 28:175-177
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::702d32899e49c028292bea8b2a1989a8
https://doi.org/10.2478/logos-2022-0015
https://doi.org/10.2478/logos-2022-0015
Publikováno v:
Lithos. :106854
A mineralogical, major, LA-ICP-MS trace element mineral chemistry and bulk-rock geochemical study of juvenile samples of the Mercato, Avellino, Pompeii and Pollena eruptions, collected in stratigraphically and volcano- logically well-characterized se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7f271fd188ed5e8eac4350bfff3426df
https://doi.org/10.1016/j.lithos.2022.106854
https://doi.org/10.1016/j.lithos.2022.106854
Autor:
Annamaria Perrotta, Claudio Scarpati
Publikováno v:
The Encyclopedia of Ancient History. :1-2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e83d6fb4b492a65b4c0ceb8a4c7045db
https://doi.org/10.1002/9781444338386.wbeah16187.pub2
https://doi.org/10.1002/9781444338386.wbeah16187.pub2
Autor:
Domenico Sparice, Massimo Osanna, Annamaria Perrotta, Valeria Amoretti, Giulia Chiominto, Michele Silani, Carlo Rescigno, Claudio Scarpati, Lorenzo Fedele, Ileana Santangelo, Francesco Muscolino
Plinian eruptions are powerful explosive volcanic events that impact large areas with cubic kilometers of magma emplaced as pyroclastic material accumulated in thick blankets around the volcanic vents. The violence of the emplacement mechanism (i.e.,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4f22bedd226eeae7c68e500fe15b327c
https://hdl.handle.net/11591/485792
https://hdl.handle.net/11591/485792
Autor:
Lorenzo Fedele, Michele Silani, Ileana Santangelo, Carlo Rescigno, Domenico Sparice, Annamaria Perrotta, Francesco Muscolino, Massimo Osanna, Valeria Amoretti, Giulia Chiominto, Claudio Scarpati
Plinian eruptions are highly energetic events that release cubic kilometres of magma in the form of pyroclastic material (pumice, lithic clasts and ash). These products tend to accumulate near the vent with considerable thickness. The rapid burial of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b20621ded54049ad59f111edb44bd856
http://hdl.handle.net/11591/465175
http://hdl.handle.net/11591/465175
The petrological features of scoria samples and enclosed holocrystalline xenoliths from the last ~1000 years of activity of the La Soufriere volcano of St. Vincent (Lesser Antilles) are described in detail here. The products of the investigated prehi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3e3610008a6e539b906bdff9572ba2a8
http://hdl.handle.net/11588/849239
http://hdl.handle.net/11588/849239
Publikováno v:
Scientific Reports
Scientific Reports, Vol 10, Iss 1, Pp 1-13 (2020)
Scientific Reports, Vol 10, Iss 1, Pp 1-13 (2020)
Large ignimbrites are the product of devastating explosive eruptions that have repeatedly impacted climate and life on global scale. The assemblage of vertical and lateral lithofacies variations within an ignimbrite sheet, its internal architecture,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4c63dbaaa092da4a34a7bb9ce9b8fa51
https://doi.org/10.1038/s41598-020-79164-7
https://doi.org/10.1038/s41598-020-79164-7