FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2110147479> ?p ?o ?g. }

• W2110147479 endingPage "290" @default.
• W2110147479 startingPage "268" @default.
• W2110147479 abstract "Propagation of short period S waves through the crust is strongly controlled by scattering loss and intrinsic absorption. Scattering loss controls the shape of the seismic envelope and the spatial distribution of the energy while intrinsic absorption produces an exponential decay as a function of time which is independent of the coordinates. Since both parameters have a different effect, it is possible to compute them by means of the Multiple Lapse Time Window Analysis (MLTWA). In this paper, high resolution maps of Japan for both seismic S-wave attenuation parameters are obtained by using the MLTWA with data provided by the Hi-net seismic network. The maps show strong regional variation of the parameters. The variations depend mainly on the tectonic setting of each region and volcanism mechanisms. In the scattering loss maps, in the 1–2 Hz map, there is a very different behaviour between the northeast (stronger scattering loss) and the southwest (much weaker scattering loss). In the northeast of Japan, areas with strong scattering loss correspond mainly to the location of the volcanic arcs. In Southwest Japan, Chugoku region and the west side of Kii peninsula show strong scattering levels for the 4–8 Hz and higher frequency bands. In Hokkaido, strong scattering loss and intrinsic absorption can be observed for the lower frequency bands. In the Sendai plain, we find strong scattering loss for all the frequency bands. Under all these areas low velocity anomalies have been detected in previous works. In Tohoku area the east side shows lower intrinsic attenuation than the west side. This characteristic seems to extend to the southern part of Hokkaido and to central Japan. In Kanto area, the values of intrinsic absorption are lower than in the surrounding areas; but in the region around the Itoigawa-Shizuoka tectonic line and in its western side strong absorption areas are observed. The behaviour of each area for intrinsic absorption is similar to the behaviour observed in the Q-1c maps. The MLTWA is based on the hypothesis of multiple isotropic scattering in a medium with the homogeneous distribution of scattering mean free path and intrinsic absorption. Although these hypotheses are very simple, the results are very informative on the characteristics of each region, and show the usefulness of studying the properties of scattered seismic waves in the understanding of the properties of the crust." @default.
• W2110147479 created "2016-06-24" @default.
• W2110147479 creator A5071146585 @default.
• W2110147479 creator A5071242926 @default.
• W2110147479 date "2010-01-01" @default.
• W2110147479 modified "2023-10-14" @default.
• W2110147479 title "Spatial distribution of scattering loss and intrinsic absorption of short-period<i>S</i>waves in the lithosphere of Japan on the basis of the Multiple Lapse Time Window Analysis of Hi-net data" @default.
• W2110147479 cites W1583021339 @default.
• W2110147479 cites W1612216475 @default.
• W2110147479 cites W1968114304 @default.
• W2110147479 cites W1974341929 @default.
• W2110147479 cites W1975789639 @default.
• W2110147479 cites W1977504503 @default.
• W2110147479 cites W1982388448 @default.
• W2110147479 cites W1982559181 @default.
• W2110147479 cites W1984657613 @default.
• W2110147479 cites W1989892229 @default.
• W2110147479 cites W1992215128 @default.
• W2110147479 cites W1996231119 @default.
• W2110147479 cites W2002184344 @default.
• W2110147479 cites W2015985360 @default.
• W2110147479 cites W2016748552 @default.
• W2110147479 cites W2017332054 @default.
• W2110147479 cites W2021121782 @default.
• W2110147479 cites W2022169694 @default.
• W2110147479 cites W2023794237 @default.
• W2110147479 cites W2028839654 @default.
• W2110147479 cites W2030379059 @default.
• W2110147479 cites W2032932075 @default.
• W2110147479 cites W2040800355 @default.
• W2110147479 cites W2040954164 @default.
• W2110147479 cites W2047006856 @default.
• W2110147479 cites W2047979420 @default.
• W2110147479 cites W2050020243 @default.
• W2110147479 cites W2055184659 @default.
• W2110147479 cites W2067231302 @default.
• W2110147479 cites W2078075699 @default.
• W2110147479 cites W2082179942 @default.
• W2110147479 cites W2084982717 @default.
• W2110147479 cites W2086360347 @default.
• W2110147479 cites W2092714623 @default.
• W2110147479 cites W2093445222 @default.
• W2110147479 cites W2095286915 @default.
• W2110147479 cites W2109152678 @default.
• W2110147479 cites W2110603984 @default.
• W2110147479 cites W2114673757 @default.
• W2110147479 cites W2115941220 @default.
• W2110147479 cites W2120206066 @default.
• W2110147479 cites W2132342875 @default.
• W2110147479 cites W2146036776 @default.
• W2110147479 cites W2156027049 @default.
• W2110147479 cites W2160716113 @default.
• W2110147479 cites W2163855257 @default.
• W2110147479 cites W2164452278 @default.
• W2110147479 cites W4298289438 @default.
• W2110147479 cites W4312827208 @default.
• W2110147479 doi "https://doi.org/10.1111/j.1365-246x.2009.04394.x" @default.
• W2110147479 hasPublicationYear "2010" @default.
• W2110147479 type Work @default.
• W2110147479 sameAs 2110147479 @default.
• W2110147479 citedByCount "118" @default.
• W2110147479 countsByYear W21101474792012 @default.
• W2110147479 countsByYear W21101474792013 @default.
• W2110147479 countsByYear W21101474792014 @default.
• W2110147479 countsByYear W21101474792015 @default.
• W2110147479 countsByYear W21101474792016 @default.
• W2110147479 countsByYear W21101474792017 @default.
• W2110147479 countsByYear W21101474792018 @default.
• W2110147479 countsByYear W21101474792019 @default.
• W2110147479 countsByYear W21101474792020 @default.
• W2110147479 countsByYear W21101474792021 @default.
• W2110147479 countsByYear W21101474792022 @default.
• W2110147479 countsByYear W21101474792023 @default.
• W2110147479 crossrefType "journal-article" @default.
• W2110147479 hasAuthorship W2110147479A5071146585 @default.
• W2110147479 hasAuthorship W2110147479A5071242926 @default.
• W2110147479 hasBestOaLocation W21101474791 @default.
• W2110147479 hasConcept C120665830 @default.
• W2110147479 hasConcept C121332964 @default.
• W2110147479 hasConcept C127313418 @default.
• W2110147479 hasConcept C165205528 @default.
• W2110147479 hasConcept C16942324 @default.
• W2110147479 hasConcept C184652730 @default.
• W2110147479 hasConcept C191486275 @default.
• W2110147479 hasConcept C77928131 @default.
• W2110147479 hasConcept C78542244 @default.
• W2110147479 hasConcept C8058405 @default.
• W2110147479 hasConceptScore W2110147479C120665830 @default.
• W2110147479 hasConceptScore W2110147479C121332964 @default.
• W2110147479 hasConceptScore W2110147479C127313418 @default.
• W2110147479 hasConceptScore W2110147479C165205528 @default.
• W2110147479 hasConceptScore W2110147479C16942324 @default.
• W2110147479 hasConceptScore W2110147479C184652730 @default.
• W2110147479 hasConceptScore W2110147479C191486275 @default.
• W2110147479 hasConceptScore W2110147479C77928131 @default.
• W2110147479 hasConceptScore W2110147479C78542244 @default.
• W2110147479 hasConceptScore W2110147479C8058405 @default.
• W2110147479 hasIssue "1" @default.

• next