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pro vyhledávání: '"Moratti, G."'
Autor:
Nirta, G., Vittori, E., Blumetti, A.M., Di Manna, P., Benvenuti, M., Montanari, D., Perini, M., Fiera, F., Moratti, G., Baglione, M., Piccardi, L.
Publikováno v:
In Geomorphology 1 February 2021 374
Publikováno v:
In Sedimentary Geology 15 November 2018 376:1-17
Publikováno v:
In Physics and Chemistry of the Earth April 2017 98:161-172
Akademický článek
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Autor:
Bonini M.[1], Maestrelli D.[1], Corti G.[1], Del Ventisette C.[1, Moratti G.[1], Carrasco-Núñez G.[3], Giordano G.[4], Lucci F.[4], Norini G.[5], Piccardi L.[1], Urbani S.[4], Montanari D.[1]
Publikováno v:
Journal of geophysical research. Solid earth (Online) 126 (2021): 1–32. doi:10.1029/2020JB020438
info:cnr-pdr/source/autori:Bonini M.[1], Maestrelli D.[1], Corti G.[1], Del Ventisette C.[1,2], Moratti G.[1], Carrasco-Núñez G.[3], Giordano G.[4], Lucci F.[4], Norini G.[5], Piccardi L.[1], Urbani S.[4], Montanari D.[1]/titolo:Modeling Intra-Caldera Resurgence Settings: Laboratory Experiments With Application to the Los Humeros Volcanic Complex (Mexico)/doi:10.1029%2F2020JB020438/rivista:Journal of geophysical research. Solid earth (Online)/anno:2021/pagina_da:1/pagina_a:32/intervallo_pagine:1–32/volume:126
info:cnr-pdr/source/autori:Bonini M.[1], Maestrelli D.[1], Corti G.[1], Del Ventisette C.[1,2], Moratti G.[1], Carrasco-Núñez G.[3], Giordano G.[4], Lucci F.[4], Norini G.[5], Piccardi L.[1], Urbani S.[4], Montanari D.[1]/titolo:Modeling Intra-Caldera Resurgence Settings: Laboratory Experiments With Application to the Los Humeros Volcanic Complex (Mexico)/doi:10.1029%2F2020JB020438/rivista:Journal of geophysical research. Solid earth (Online)/anno:2021/pagina_da:1/pagina_a:32/intervallo_pagine:1–32/volume:126
Scaled analogue models explored the role of different boundary conditions in intra‐caldera resurgence processes. Models investigated the role of magma intrusion depth (Series 1), asymmetric and symmetric caldera collapse (Series 2), as well as the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5581ab2bad63341498443018c51b2805
Autor:
Moratti, G.1 giovanna.moratti@igg.cnr.it, Benvenuti, M.1,2, Santo, A. P.1,2, Laurenzi, M. A.3, Braschi, E.1, Tommasini, S.2
Publikováno v:
International Journal of Earth Sciences. Oct2018, Vol. 107 Issue 7, p2491-2515. 25p.
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:
International journal of earth sciences (1999, Internet) 107 (2018): 2491–2515.
info:cnr-pdr/source/autori:Moratti G.[1], Benvenuti M.[1,2], Santo A.[1,2], Laurenzi M.[3], Braschi E.[1], Tommasini S.[2]/titolo:New 40Ar-39Ar dating of lower cretaceous basalts at the Southern front of the Central High Atlas, Morocco: insights of late mesozoic tectonics, sedimentation and magmatism/doi:/rivista:International journal of earth sciences (1999, Internet)/anno:2018/pagina_da:2491/pagina_a:2515/intervallo_pagine:2491–2515/volume:107
info:cnr-pdr/source/autori:Moratti G.[1], Benvenuti M.[1,2], Santo A.[1,2], Laurenzi M.[3], Braschi E.[1], Tommasini S.[2]/titolo:New 40Ar-39Ar dating of lower cretaceous basalts at the Southern front of the Central High Atlas, Morocco: insights of late mesozoic tectonics, sedimentation and magmatism/doi:/rivista:International journal of earth sciences (1999, Internet)/anno:2018/pagina_da:2491/pagina_a:2515/intervallo_pagine:2491–2515/volume:107
This study is based upon a stratigraphic and structural revision of a Middle Jurassic-Upper Cretaceous mostly continental succession exposed between Boumalne Dades and Tinghir (Southern Morocco), and aims at reconstructing the relation among sediment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::26d419597d7487d818017976ac9b4855
http://www.cnr.it/prodotto/i/392746
http://www.cnr.it/prodotto/i/392746
Publikováno v:
Sedimentary Geology 376 (2018): 1–17.
info:cnr-pdr/source/autori:Cavallina C.[1], Papini M.[1], Moratti G.[2], Benvenuti M. [1,2]/titolo:The Late Mesozoic evolution of the Central High Atlas domain (Morocco): suggestions from the paleo-drainage record of the Adrar Aglagal syncline/doi:/rivista:Sedimentary Geology/anno:2018/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:376
info:cnr-pdr/source/autori:Cavallina C.[1], Papini M.[1], Moratti G.[2], Benvenuti M. [1,2]/titolo:The Late Mesozoic evolution of the Central High Atlas domain (Morocco): suggestions from the paleo-drainage record of the Adrar Aglagal syncline/doi:/rivista:Sedimentary Geology/anno:2018/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:376
This paper illustrates the results of a stratigraphic, sedimentologic and structural study of the continental succession exposed at the core of the Adrar Aglagal syncline, located at the southern front of the Central High Atlas (Morocco). This struct
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::b96fb11b31902038da7f0a412fda56d5
http://www.cnr.it/prodotto/i/393746
http://www.cnr.it/prodotto/i/393746