Zobrazeno 1 - 10
of 71
pro vyhledávání: '"MARCO STEFANI"'
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 94, Iss 3 (2020)
The Rhaetic facies, as developed in the Southern Alpine region of Italy, were deposited in a strongly subsiding, fault-dissected trough (the Lombardian Basin) bounded by carbonate platforms. The main part of the Rhaetic succession consists of decamet
Externí odkaz:
https://doaj.org/article/85dca28e042e49e7855f9340e04eb334
Publikováno v:
IEEE Design & Test. 39:15-22
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::656819d5797762b40b7d7b0dff51fb31
https://doi.org/10.1109/mdat.2022.3142193
https://doi.org/10.1109/mdat.2022.3142193
Autor:
Sara Amoroso, Kyle M. Rollins, Giuseppe Di Giulio, Lara Wacha, Kosta Urumović, Diana Faieta, Radovan Filjak, Daniela Fontana, Stefano Lugli, Maria Manuel, Giuliano Milana, Luca Minarelli, Marko Budić, Nikola Belić, Tomislav Kurečić, Luka Sorić, Marco Stefani, Gabriele Tarabusi, Maurizio Vassallo
Publikováno v:
2nd Croatian Conference on Earthquake Engineering ‒ 2CroCEE.
Earthquakes and related coseismic effects at the surface, such as liquefaction and lateral spreading, can impact humans due to the resulting economic or social disruptions (e.g. slope and foundation failures, flotation of buried structures, etc.). In
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88fcc37d223c60f7eec9537b99583963
https://doi.org/10.5592/co/2crocee.2023.21
https://doi.org/10.5592/co/2crocee.2023.21
Autor:
MARCO STEFANI, ANDREA GOLFIERI
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 95, Iss 1 (2018)
This paper deals with Rhaetic facies at the Lombardy-Trentino border, in the Giudicarie Region. This area is characterized by important facies changes crossing strike slip faults. Two coeval sections, showing remarkable facies differences, are examin
Externí odkaz:
https://doaj.org/article/1905a5e184f648bb9ac62bf487a593bf
Publikováno v:
Annals of Geophysics, Vol 59, Iss 5 (2016)
The 2012 earthquakes sequence stroke a wide area of the alluvial plain in the Emilia-Romagna Region and triggered a new research interest on the role of the subsurface stratigraphic architecture and petrophysical property distribution in the modulati
Externí odkaz:
https://doaj.org/article/587587fb5e644253830a2a72d476f271
Publikováno v:
Journal of Sedimentary Research. 89:13-27
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::940c9b09f4de4ee584f3b9086bc8573e
https://doi.org/10.2110/jsr.2019.1
https://doi.org/10.2110/jsr.2019.1
Autor:
Maurizio Vassallo, Giordano Teza, Vincenzo Sapia, Aura Cecilia Salocchi, Francesca Romana Cinti, Mauro Mariotti, Alessandra Smedile, Paolo Marco De Martini, Giuliano Milana, Sara Amoroso, Diego Marchetti, Fawzi Doumaz, Maria R. Manuel, Kord J. Wissmann, Cesare Comina, F. Loddo, Dario Conforti, Daniela Pantosti, Guido Gottardi, Paola Monaco, Kyle M. Rollins, Marco Anzidei, Marco Stefani, Igino Coco, Arianna Pesci, Brian Metcalfe, Andrea Carpena, Valerio Materni, Sebastiano Foti, Antonio Pesce, Giuseppe Di Giulio, Gabriele Tarabusi, Luca Minarelli, Stefano Lugli, Fabio Giannattasio, Daniela Fontana, Riccardo Civico, Paul Andersen, Laura Tonni, María Fernanda García Martínez
In the engineering geology field increased attention has been posed in recent years to potential liquefaction mitigation interventions in susceptible sand formations. In silty sands this is a major challenge because, as the fines content increases, v
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::392fdab0c197ccee70ea22602d5755dd
https://hdl.handle.net/11380/1207292
https://hdl.handle.net/11380/1207292
Autor:
Riccardo Caputo, Kyriaki Iordanidou, Luca Minarelli, Giorgos Papathanassiou, Maria Eliana Poli, Dimitra Rapti-Caputo, Sotiris Sboras, Marco Stefani, Adriano Zanferrari
Publikováno v:
Annals of Geophysics, Vol 55, Iss 4 (2012)
In May 2012, two moderate (-to-strong) earthquakes that were associated with a noticeable aftershock sequence affected the eastern sector of the Po Plain, Italy, in correspondence with a buried portion of the Apennines thrust belt. The Provinces of F
Externí odkaz:
https://doaj.org/article/3c352a0029ec476d812aa9762116be18
Publikováno v:
Annals of Geophysics, Vol 55, Iss 4 (2012)
Massive surface fracturing and sand ejection took place during the main shock of the May 20, 2012, earthquake (Ml = 5.9) in the Emilia-Romagna region, northern Italy. These phenomena were induced by the liquefaction of water-saturated sand layers, an
Externí odkaz:
https://doaj.org/article/4ce73ded12174af48018e61c5ffe8c7d