Matches in SemOpenAlex for { <https://semopenalex.org/work/W2968087890> ?p ?o ?g. }
- W2968087890 endingPage "1531" @default.
- W2968087890 startingPage "1514" @default.
- W2968087890 abstract "SUMMARY S-wave spectral amplitudes from 312 crustal earthquakes recorded at the Iranian National Broadband Seismic Network in the Alborz region between 2005 and 2017 are analysed in order to evaluate earthquake source parameters, path attenuation and site amplification functions using the non-parametric generalized inversion technique (GIT). We exploit a total number of 1117 seismograms with ML 3–5.6 in the frequency range 0.3–20 Hz. The evaluated non-parametric attenuation functions decay uniformly with distance for the entire frequency range and the estimated S-wave quality factor shows low Q values with relatively strong frequency dependence. We assume the omega-square source model to retrieve earthquake source parameters from the inverted source spectra. The obtained stress drops range from 0.02 to 16 MPa with a mean value of 1.1 MPa. Stress drop and radiated energy show fairly self-similar scaling with seismic moment over the available magnitude range; however, the magnitude range of this study is too narrow to draw a definite conclusion on source scaling characteristics. The obtained moment magnitude Mw and the local magnitude ML are linearly correlated and approximately equivalent in the range of Mw 3–4. For larger events, Mw generally underestimates ML by about 0.1–0.5 magnitude units. The estimated site amplification functions for horizontal component (GIT H) are nearly flat with no obvious pre-dominant frequency peaks for most stations, as expected for the sites of permanent broad-band seismic stations located on rock, though a few stations show amplification peaks from 1 to 8 Hz, with a maximum amplification of about a factor of 7 with respect to the reference site. The evaluated site responses for the vertical components present remarkable amplification or deamplification, leading to differences of the H/V amplitude levels in comparison with the GIT H amplification curves. The results of this study provide a valuable basis for predicting appropriate ground motions in a context of seismic hazard assessment." @default.
- W2968087890 created "2019-08-22" @default.
- W2968087890 creator A5003861471 @default.
- W2968087890 creator A5030863375 @default.
- W2968087890 creator A5054784928 @default.
- W2968087890 creator A5060499864 @default.
- W2968087890 date "2019-08-17" @default.
- W2968087890 modified "2023-09-27" @default.
- W2968087890 title "Non-parametric spectral modelling of source parameters, path attenuation and site effects from broad-band waveforms of the Alborz earthquakes (2005–2017)" @default.
- W2968087890 cites W1515101447 @default.
- W2968087890 cites W1557585847 @default.
- W2968087890 cites W1969797732 @default.
- W2968087890 cites W1971207705 @default.
- W2968087890 cites W1987610226 @default.
- W2968087890 cites W1989464914 @default.
- W2968087890 cites W1990677313 @default.
- W2968087890 cites W1993647865 @default.
- W2968087890 cites W1994553199 @default.
- W2968087890 cites W1996174093 @default.
- W2968087890 cites W2001167059 @default.
- W2968087890 cites W2001640355 @default.
- W2968087890 cites W2004693882 @default.
- W2968087890 cites W2008022126 @default.
- W2968087890 cites W2014537082 @default.
- W2968087890 cites W2014673467 @default.
- W2968087890 cites W2020399914 @default.
- W2968087890 cites W2020844434 @default.
- W2968087890 cites W2028156169 @default.
- W2968087890 cites W2028801653 @default.
- W2968087890 cites W2037941857 @default.
- W2968087890 cites W2038519446 @default.
- W2968087890 cites W2041598958 @default.
- W2968087890 cites W2048209931 @default.
- W2968087890 cites W2051158384 @default.
- W2968087890 cites W2053496294 @default.
- W2968087890 cites W2057255473 @default.
- W2968087890 cites W2059255625 @default.
- W2968087890 cites W2059938998 @default.
- W2968087890 cites W2063760158 @default.
- W2968087890 cites W2065566528 @default.
- W2968087890 cites W2075726938 @default.
- W2968087890 cites W2077076159 @default.
- W2968087890 cites W2084889084 @default.
- W2968087890 cites W2086098113 @default.
- W2968087890 cites W2086676159 @default.
- W2968087890 cites W2088025788 @default.
- W2968087890 cites W2093604272 @default.
- W2968087890 cites W2098577183 @default.
- W2968087890 cites W2103047019 @default.
- W2968087890 cites W2104782968 @default.
- W2968087890 cites W2104802194 @default.
- W2968087890 cites W2106641143 @default.
- W2968087890 cites W2107382178 @default.
- W2968087890 cites W2108656459 @default.
- W2968087890 cites W2115725291 @default.
- W2968087890 cites W2117897510 @default.
- W2968087890 cites W2120489623 @default.
- W2968087890 cites W2123949378 @default.
- W2968087890 cites W2125352847 @default.
- W2968087890 cites W2128781932 @default.
- W2968087890 cites W2128952027 @default.
- W2968087890 cites W2129924517 @default.
- W2968087890 cites W2130871605 @default.
- W2968087890 cites W2130917613 @default.
- W2968087890 cites W2133553327 @default.
- W2968087890 cites W2133651145 @default.
- W2968087890 cites W2140849331 @default.
- W2968087890 cites W2142360846 @default.
- W2968087890 cites W2146404654 @default.
- W2968087890 cites W2156240182 @default.
- W2968087890 cites W2158600705 @default.
- W2968087890 cites W2159613255 @default.
- W2968087890 cites W2160304238 @default.
- W2968087890 cites W2160987692 @default.
- W2968087890 cites W2164673848 @default.
- W2968087890 cites W2167291508 @default.
- W2968087890 cites W2236921216 @default.
- W2968087890 cites W2268296286 @default.
- W2968087890 cites W2283059580 @default.
- W2968087890 cites W2308005288 @default.
- W2968087890 cites W2554603693 @default.
- W2968087890 cites W2562928641 @default.
- W2968087890 cites W2604854830 @default.
- W2968087890 cites W2616833521 @default.
- W2968087890 cites W2765666437 @default.
- W2968087890 cites W2783213494 @default.
- W2968087890 cites W2900550994 @default.
- W2968087890 cites W2944617032 @default.
- W2968087890 cites W4230769750 @default.
- W2968087890 cites W4312768259 @default.
- W2968087890 doi "https://doi.org/10.1093/gji/ggz377" @default.
- W2968087890 hasPublicationYear "2019" @default.
- W2968087890 type Work @default.
- W2968087890 sameAs 2968087890 @default.
- W2968087890 citedByCount "3" @default.
- W2968087890 countsByYear W29680878902020 @default.
- W2968087890 countsByYear W29680878902021 @default.
- W2968087890 crossrefType "journal-article" @default.