Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Agostini A.[4]"'
Autor:
Braschi E.[1], Mastroianni F.[2, Di Salvo S.[2], Casalini M.[2], Agostini S.[4], Vougioukalakis G.[5], Francalanci L.[2]
Publikováno v:
Lithos (Oslo. Print) 410-411 (2022). doi:10.1016/j.lithos.2021.106574
info:cnr-pdr/source/autori:Braschi E.[1], Mastroianni F.[2,3], Di Salvo S.[2], Casalini M.[2], Agostini S.[4], Vougioukalakis G.[5], Francalanci L.[2]/titolo:Unveiling the occurrence of transient, multi-contaminated mafic magmas inside a rhyolitic reservoir feeding an explosive eruption (Nisyros, Greece)/doi:10.1016%2Fj.lithos.2021.106574/rivista:Lithos (Oslo. Print)/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:410-411
info:cnr-pdr/source/autori:Braschi E.[1], Mastroianni F.[2,3], Di Salvo S.[2], Casalini M.[2], Agostini S.[4], Vougioukalakis G.[5], Francalanci L.[2]/titolo:Unveiling the occurrence of transient, multi-contaminated mafic magmas inside a rhyolitic reservoir feeding an explosive eruption (Nisyros, Greece)/doi:10.1016%2Fj.lithos.2021.106574/rivista:Lithos (Oslo. Print)/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:410-411
The investigation of heterogeneous magma systems enhances the understanding of magma differentiation and transfer processes in active volcanoes, thus constraining the dynamics driving the eruptions and the related hazard. Magma heterogeneity is gener
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3974f15e0fe6441ba3dbb981f00d3f43
http://hdl.handle.net/2158/1254714
http://hdl.handle.net/2158/1254714
Autor:
Mastroianni F.[1, Braschi E.[3], Casalini M.[2], Agostini S.[4], Di Salvo S.[2], Vougioukalakis G.[5], Francalanci L.[2]
Publikováno v:
Data in brief 42 (2022). doi:10.1016/j.dib.2022.108077
info:cnr-pdr/source/autori:Mastroianni F.[1,2], Braschi E.[3], Casalini M.[2], Agostini S.[4], Di Salvo S.[2], Vougioukalakis G.[5], Francalanci L.[2]/titolo:Data on unveiling the occurrence of transient, multi-contaminated mafic magmas inside a rhyolitic reservoir feeding an explosive eruption (Nisyros, Greece)/doi:10.1016%2Fj.dib.2022.108077/rivista:Data in brief/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:42
info:cnr-pdr/source/autori:Mastroianni F.[1,2], Braschi E.[3], Casalini M.[2], Agostini S.[4], Di Salvo S.[2], Vougioukalakis G.[5], Francalanci L.[2]/titolo:Data on unveiling the occurrence of transient, multi-contaminated mafic magmas inside a rhyolitic reservoir feeding an explosive eruption (Nisyros, Greece)/doi:10.1016%2Fj.dib.2022.108077/rivista:Data in brief/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:42
This data article includes the description and the geochemical and mineralogical dataset of 67 pyroclastic rock samples from the Upper Pumice (UP) explosive activity of Nisyros volcano (eastern South Aegean Active Volcanic Arc). A detailed field and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b87dad0879cbbb142ab57463d321991b
https://doi.org/10.1016/j.dib.2022.108077
https://doi.org/10.1016/j.dib.2022.108077
Publikováno v:
Periodico di mineralogia (Testo stamp.) 90 (2021): 59–83. doi:10.13133/2239-1002/16620
info:cnr-pdr/source/autori:Salari G.[1], Lustrino M.[1,2], Ghorbani M.R.[3], Agostini S.[4], Fedele L.[5]/titolo:Petrological characterization of the Cenozoic igneous rocks of the Tafresh area, central Urumieh-Dokhtar Magmatic Arc (Iran)/doi:10.13133%2F2239-1002%2F16620/rivista:Periodico di mineralogia (Testo stamp.)/anno:2021/pagina_da:59/pagina_a:83/intervallo_pagine:59–83/volume:90
info:cnr-pdr/source/autori:Salari G.[1], Lustrino M.[1,2], Ghorbani M.R.[3], Agostini S.[4], Fedele L.[5]/titolo:Petrological characterization of the Cenozoic igneous rocks of the Tafresh area, central Urumieh-Dokhtar Magmatic Arc (Iran)/doi:10.13133%2F2239-1002%2F16620/rivista:Periodico di mineralogia (Testo stamp.)/anno:2021/pagina_da:59/pagina_a:83/intervallo_pagine:59–83/volume:90
We report a petrographic and whole-rock geochemical characterization of the Cenozoic volcanic rocks cropping out in the Tafresh area of the central Urumieh-Dokhtar Magmatic Arc of Iran. The investigated rocks range mainly from basaltic andesite to da
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::64141424f29ade81e3d4d0a6bea44d06
http://hdl.handle.net/11573/1535787
http://hdl.handle.net/11573/1535787
Autor:
Taussi M.[1], Godoy B.[2], Piscaglia F.[3], Morata D.[2], Agostini A.[4], Le Roux P.[5], González-Maurel O.[5, Gallmeyer G.[6], Menzies A.[6], Renzulli A.[1
Publikováno v:
Journal of volcanology and geothermal research 373 (2019): 179–198. doi:10.1016/j.jvolgeores.2019.01.021
info:cnr-pdr/source/autori:Taussi M.[1], Godoy B.[2], Piscaglia F.[3], Morata D.[2], Agostini A.[4], Le Roux P.[5], González-Maurel O.[5,6], Gallmeyer G.[6], Menzies A.[6], Renzulli A.[1,3]/titolo:The upper crustal magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna, northern Chile) as inferred from the erupted lavas and their enclaves/doi:10.1016%2Fj.jvolgeores.2019.01.021/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:179/pagina_a:198/intervallo_pagine:179–198/volume:373
info:cnr-pdr/source/autori:Taussi M.[1], Godoy B.[2], Piscaglia F.[3], Morata D.[2], Agostini A.[4], Le Roux P.[5], González-Maurel O.[5,6], Gallmeyer G.[6], Menzies A.[6], Renzulli A.[1,3]/titolo:The upper crustal magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna, northern Chile) as inferred from the erupted lavas and their enclaves/doi:10.1016%2Fj.jvolgeores.2019.01.021/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:179/pagina_a:198/intervallo_pagine:179–198/volume:373
The evolution of the magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna Volcanic Complex, northern Chile) was investigated through petrographic, geochemical and isotopic studies of representative lavas a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::182ba00063760c305b4e7c49b0043bea
https://hdl.handle.net/11576/2665116
https://hdl.handle.net/11576/2665116
Publikováno v:
Tectonophysics (Amst. Online) 728-729 (2018): 75–91. doi:10.1016/j.tecto.2018.02.011
info:cnr-pdr/source/autori:Corti G.[1,2], Sani F.[3], Agostini S.[4], Philippon M.[5,6], Sokoutis D.[5,6], Willingshofer E.[7]/titolo:Off-axis volcano-tectonic activity during continental rifting: Insights from the transversal Goba-Bonga lineament, Main Ethiopian Rift (East Africa)/doi:10.1016%2Fj.tecto.2018.02.011/rivista:Tectonophysics (Amst. Online)/anno:2018/pagina_da:75/pagina_a:91/intervallo_pagine:75–91/volume:728-729
Tectonophysics
Tectonophysics, Elsevier, 2018, 728, pp.75-91. ⟨10.1016/j.tecto.2018.02.011⟩
Tectonophysics, 728-729, 75. Elsevier
info:cnr-pdr/source/autori:Corti G.[1,2], Sani F.[3], Agostini S.[4], Philippon M.[5,6], Sokoutis D.[5,6], Willingshofer E.[7]/titolo:Off-axis volcano-tectonic activity during continental rifting: Insights from the transversal Goba-Bonga lineament, Main Ethiopian Rift (East Africa)/doi:10.1016%2Fj.tecto.2018.02.011/rivista:Tectonophysics (Amst. Online)/anno:2018/pagina_da:75/pagina_a:91/intervallo_pagine:75–91/volume:728-729
Tectonophysics
Tectonophysics, Elsevier, 2018, 728, pp.75-91. ⟨10.1016/j.tecto.2018.02.011⟩
Tectonophysics, 728-729, 75. Elsevier
International audience; The Main Ethiopian Rift, East Africa, is characterized by the presence of major, enigmatic structures which strike approximately orthogonal to the trend of the rift valley. These structures are marked by important deformation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3cbc40029d1c7879c900d459d543a2ad
http://www.cnr.it/prodotto/i/393587
http://www.cnr.it/prodotto/i/393587