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220822 ||| eng |
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|a books978-3-0365-1878-7
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|a 9783036518787
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|a 9783036518770
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1 |
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|a Porfido, Sabina
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245 |
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|a New Perspectives in the Definition/Evaluation of Seismic Hazard through Analysis of the Environmental Effects Induced by Earthquakes
|h Elektronische Ressource
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260 |
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|a Basel, Switzerland
|b MDPI - Multidisciplinary Digital Publishing Institute
|c 2021
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300 |
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|a 1 electronic resource (424 p.)
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653 |
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|a machine learning
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|a georisk
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653 |
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|a DIC
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653 |
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|a earthquake
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653 |
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|a Pohang earthquake
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653 |
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|a Australian earthquakes
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653 |
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|a seismotectonic deformation
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653 |
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|a ground effects
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653 |
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|a Intraplate earthquake
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653 |
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|a laboratory tests
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653 |
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|a CPO
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653 |
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|a seismic zoning
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653 |
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|a surface rupture
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653 |
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|a EEE database
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653 |
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|a shear-wave velocity structure
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653 |
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|a cyclic triaxial tests
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653 |
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|a Structure-from-Motion
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653 |
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|a paleoliquefaction
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653 |
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|a Sakhalin Island
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653 |
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|a risk
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653 |
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|a intraplate region
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653 |
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|a earthquake catalogues
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653 |
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|a Late Cenozoic deformation
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653 |
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|a active fault
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653 |
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|a Research & information: general / bicssc
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653 |
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|a ground-shaking map
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653 |
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|a landslide
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653 |
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|a liquefaction
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653 |
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|a coseismic landslides
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653 |
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|a MMI
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653 |
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|a crustal model
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653 |
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|a earthquake mechanism
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653 |
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|a Tien Shan
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653 |
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|a amalgamation
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|a inversion
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653 |
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|a fully probabilistic technique
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|a disaster
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653 |
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|a Guatemala
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653 |
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|a one class classification
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653 |
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|a earthquake archaeological effects (EAEs)
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653 |
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|a spatial resolution
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653 |
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|a Spain
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653 |
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|a paleoseismogenic structure
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653 |
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|a Ecuador
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653 |
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|a inventory map
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653 |
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|a maximum possible magnitudes of earthquakes
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653 |
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|a earth observation (EO)
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|a ESI-07 scale
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|a expert estimate
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|a earthquake environmental effects
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|a Newmark's method
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|a seismic scenarios
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653 |
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|a seismic hazard
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653 |
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|a in situ tests
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|a earthquake forecasting
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653 |
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|a soil liquefaction
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|a emergency shelter
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|a Arctic-Asian seismic belt
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|a paleoearthquake
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|a earthquake environmental effects (EEEs)
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|a probabilistic seismic hazard
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|a model selection
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|a Suusamyr earthquake
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|a ESI scale
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|a intensity maps
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|a reverse earthquake
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|a ESI 2007 scale
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|a weighted coefficient
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|a digital elevation model (DEM)
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|a potential seismicity
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|a fault barrier
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|a historical and recent earthquakes
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653 |
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|a earthquake hazard
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653 |
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|a South Korea
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653 |
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|a earthquake-induced landslide
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653 |
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|a Pedernales earthquake
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|a suitability analysis
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653 |
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|a mass movements
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653 |
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|a site amplification
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|a ESI scale 2007
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|a regional segment
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|a catalog incompleteness
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|a attenuation
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653 |
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|a GMPE
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653 |
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|a geological control
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653 |
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|a geographic information systems (GIS)
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653 |
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|a Ulaanbaatar
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653 |
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|a earthquake hazards
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653 |
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|a Kyrgyzstan
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653 |
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|a microtremor H/V spectral ratio
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|a macroseismic intensity
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700 |
1 |
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|a Alessio, Giuliana
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700 |
1 |
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|a Gaudiosi, Germana
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700 |
1 |
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|a Nappi, Rosa
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041 |
0 |
7 |
|a eng
|2 ISO 639-2
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989 |
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|b DOAB
|a Directory of Open Access Books
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500 |
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|a Creative Commons (cc), https://creativecommons.org/licenses/by/4.0/
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028 |
5 |
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|a 10.3390/books978-3-0365-1878-7
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856 |
4 |
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|u https://www.mdpi.com/books/pdfview/book/4375
|7 0
|x Verlag
|3 Volltext
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856 |
4 |
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|u https://directory.doabooks.org/handle/20.500.12854/76905
|z DOAB: description of the publication
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|a 363
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|a 000
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|a 900
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|a 320
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|a 700
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|a The devastating effects caused by the recent catastrophic earthquakes that took place all over the world from Japan, New Zealand, to Chile, as well as those occurring in the Mediterranean basin, have once again shown that ground motion, although a serious source of direct damage, is not the only parameter to be considered, with most damage being the result of coseismic geological effects that are directly connected to the earthquake source or caused by ground shaking. The primary environmental effects induced by earthquakes as well as the secondary effects (sensu Environmental Seismic Intensity - ESI 2007 scale) must be considered for a more correct and complete evaluation of seismic hazards, at both regional and local scales. This Special Issue aims to collect all contributions that, using different methodologies, integrate new data produced with multi-disciplinary and innovative methods. These methodologies are essential for the identification and characterization of seismically active areas, and for the development of new hazard models, obtained using different survey techniques. The topic attracted a lot of interest, 19 peer-reviewed articles were collected; moreover, different areas of the world have been analyzed through these methodologies: Italy, USA, Spain, Australia, Ecuador, Guatemala, South Korea, Kyrgyzstan, Mongolia, Russia, China, Japan, and Nepal.
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