Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Bruno Quadrio"'
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 14, Iss 4, Pp 731-737 (2014)
Natural hazards and earth system sciences
14 (2014): 731–737. doi:10.5194/nhess-14-731-2014
info:cnr-pdr/source/autori:Giocoli, A.; Quadrio, B.; Bellanova, J.; Lapenna, V.; Piscitelli, S./titolo:Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw=6.1, northern Italy)/doi:10.5194%2Fnhess-14-731-2014/rivista:Natural hazards and earth system sciences (Print)/anno:2014/pagina_da:731/pagina_a:737/intervallo_pagine:731–737/volume:14
Natural hazards and earth system sciences
14 (2014): 731–737. doi:10.5194/nhess-14-731-2014
info:cnr-pdr/source/autori:Giocoli, A.; Quadrio, B.; Bellanova, J.; Lapenna, V.; Piscitelli, S./titolo:Electrical resistivity tomography for studying liquefaction induced by the May 2012 Emilia-Romagna earthquake (Mw=6.1, northern Italy)/doi:10.5194%2Fnhess-14-731-2014/rivista:Natural hazards and earth system sciences (Print)/anno:2014/pagina_da:731/pagina_a:737/intervallo_pagine:731–737/volume:14
This work shows the result of an electrical resistivity tomography (ERT) survey carried out for imaging and characterizing the shallow subsurface affected by the coseismic effects of the Mw=6.1 Emilia-Romagna (northern Italy) earthquake that occurred
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d72dd3fc04b2ce4dd0f8749f164c6671
https://doi.org/10.5194/nhess-14-731-2014
https://doi.org/10.5194/nhess-14-731-2014
Publikováno v:
Geomorphology. 206:97-106
Fault scarps affecting post-LGM (Last Glacial Maximum) slopes are usually seen as an indication of active tectonics, even if they can barely provide analytical data concerning single coseismic fault rupture (offset amount and age) or significant clue
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c314ecb636d28a742d9f3f13e2d75695
https://doi.org/10.1016/j.geomorph.2013.09.023
https://doi.org/10.1016/j.geomorph.2013.09.023
A New Step for Seismic Microzonation Studies in Italy: Standards for Data Storage and Representation
Publikováno v:
Engineering Geology for Society and Territory-Volume 5 ISBN: 9783319090474
As one of the major components of earthquake risk mitigation studies, seismic microzonation can be defined as the process of mapping the distribution of site response with respect to ground shaking intensity and ground failure susceptibility such as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::804a3fb8bfb4ef961a200a68c407856a
https://doi.org/10.1007/978-3-319-09048-1_223
https://doi.org/10.1007/978-3-319-09048-1_223
Publikováno v:
Engineering Geology for Society and Territory-Volume 5 ISBN: 9783319090474
Following the enactment of Italian Law 77, 2009, almost all the Italian regions have been funded to produce seismic microzonation studies, according to the three levels of detail provided by Instructions and Criteria for Seismic Microzonation, in mun
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::71b787fcf7e84a596545f6b1e8f63697
https://doi.org/10.1007/978-3-319-09048-1_214
https://doi.org/10.1007/978-3-319-09048-1_214
Publikováno v:
Bulletin of earthquake engineering
12 (2014): 1383–1403. doi:10.1007/s10518-013-9436-5
info:cnr-pdr/source/autori:Pagliaroli A., Quadrio B., Lanzo G., Sanò T./titolo:Numerical modelling of site effects in the Palatine hill, Roman Forum and Coliseum archaeological area/doi:10.1007%2Fs10518-013-9436-5/rivista:Bulletin of earthquake engineering (Print)/anno:2014/pagina_da:1383/pagina_a:1403/intervallo_pagine:1383–1403/volume:12
12 (2014): 1383–1403. doi:10.1007/s10518-013-9436-5
info:cnr-pdr/source/autori:Pagliaroli A., Quadrio B., Lanzo G., Sanò T./titolo:Numerical modelling of site effects in the Palatine hill, Roman Forum and Coliseum archaeological area/doi:10.1007%2Fs10518-013-9436-5/rivista:Bulletin of earthquake engineering (Print)/anno:2014/pagina_da:1383/pagina_a:1403/intervallo_pagine:1383–1403/volume:12
Historical sources report that Rome has experienced considerable earthquake ground motion in the past, even though it is quite far from high-magnitude seismogenic sources. Damage distribution seems to be predominantly controlled by ground shaking amp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d0ddf37dfba69bb4af4ef3175937da7d
http://hdl.handle.net/11573/558742
http://hdl.handle.net/11573/558742
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