FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4310010382> ?p ?o ?g. }

• W4310010382 endingPage "2948" @default.
• W4310010382 startingPage "2925" @default.
• W4310010382 abstract "The return period of large earthquakes in intraplate regions is more in comparison to the interplate regions. Also, the intraplate region is less instrumented and hence, these regions are devoid of acceleration time histories of large and great earthquakes. The mainland Gujarat region is one of such intraplate regions for which acceleration time histories are not available, however, is vulnerable for earthquakes of M ∼ 6.0. Simulation is performed in these scenarios and the prerequisite is the knowledge of source parameters and scaling laws. We analyzed the spectra of the P- and S-waves recorded by the stations of Gujarat Seismic Network for the mainland Gujarat region of western Deccan Volcanic Province, India. Additionally, we developed scaling laws based on the obtained source parameters. We analyze 177 digital records from 43 local earthquakes during the period 2007–2016 with a magnitude of Ml = 2.5–4.3, which are located in a distance range of 10–250 km, using Brune’s seismic source model (Brune 1970, 1971). According to our study, the calculated stress drop values do not vary considerably with seismic moment values and are generally between 1 and 100 bar for most of the events. Therefore, the earthquakes in this region adhere to the law of self-similarity. As widely observed for conventional earthquakes, we find an inverse relationship between seismic moment and corner frequency for these events. Based on a linear regression analysis between the assessed seismic moment (M0) and corner frequency (fc), we developed the scaling relation M0fc3 = 2.29 × 1015. Scaling relations developed here are in agreement with those developed for the nearby Kachchh region and various other seismically active areas around the world. Use of regional scaling is recommended instead of global scaling laws for better estimation of seismic hazard. The source parameters and scaling laws presented here can be used for a variety of applications in mainland Gujarat, including the assessment of seismic hazards and the development of earthquake scenarios." @default.
• W4310010382 created "2022-11-30" @default.
• W4310010382 creator A5004821840 @default.
• W4310010382 creator A5046192421 @default.
• W4310010382 date "2022-11-25" @default.
• W4310010382 modified "2023-09-30" @default.
• W4310010382 title "Source parameters and scaling relations for small earthquakes in mainland Gujarat region of Western Deccan Volcanic Province, India" @default.
• W4310010382 cites W1603888885 @default.
• W4310010382 cites W1629132018 @default.
• W4310010382 cites W1852221269 @default.
• W4310010382 cites W1885142023 @default.
• W4310010382 cites W1970520886 @default.
• W4310010382 cites W1975437198 @default.
• W4310010382 cites W1980811494 @default.
• W4310010382 cites W1983900669 @default.
• W4310010382 cites W1990790800 @default.
• W4310010382 cites W1992626998 @default.
• W4310010382 cites W1994018849 @default.
• W4310010382 cites W1994553199 @default.
• W4310010382 cites W1996174093 @default.
• W4310010382 cites W1996603668 @default.
• W4310010382 cites W2007792583 @default.
• W4310010382 cites W2011836965 @default.
• W4310010382 cites W2013240345 @default.
• W4310010382 cites W2021308529 @default.
• W4310010382 cites W2032137675 @default.
• W4310010382 cites W2044490798 @default.
• W4310010382 cites W2045878906 @default.
• W4310010382 cites W2046832133 @default.
• W4310010382 cites W2053496294 @default.
• W4310010382 cites W2060453543 @default.
• W4310010382 cites W2066336061 @default.
• W4310010382 cites W2073222026 @default.
• W4310010382 cites W2074554314 @default.
• W4310010382 cites W2077076159 @default.
• W4310010382 cites W2077951553 @default.
• W4310010382 cites W2078100914 @default.
• W4310010382 cites W2088025788 @default.
• W4310010382 cites W2095987427 @default.
• W4310010382 cites W2102334847 @default.
• W4310010382 cites W2106641143 @default.
• W4310010382 cites W2108717155 @default.
• W4310010382 cites W2109657428 @default.
• W4310010382 cites W2114646782 @default.
• W4310010382 cites W2115725291 @default.
• W4310010382 cites W2120007352 @default.
• W4310010382 cites W2129742752 @default.
• W4310010382 cites W2130871605 @default.
• W4310010382 cites W2130917613 @default.
• W4310010382 cites W2131006534 @default.
• W4310010382 cites W2132282308 @default.
• W4310010382 cites W2132379360 @default.
• W4310010382 cites W2132963780 @default.
• W4310010382 cites W2133564330 @default.
• W4310010382 cites W2134936968 @default.
• W4310010382 cites W2138010249 @default.
• W4310010382 cites W2140750477 @default.
• W4310010382 cites W2142256591 @default.
• W4310010382 cites W2145639782 @default.
• W4310010382 cites W2146404654 @default.
• W4310010382 cites W2149485118 @default.
• W4310010382 cites W2156594022 @default.
• W4310010382 cites W2165452994 @default.
• W4310010382 cites W2166173218 @default.
• W4310010382 cites W2179073092 @default.
• W4310010382 cites W2272415331 @default.
• W4310010382 cites W2278283721 @default.
• W4310010382 cites W2319736957 @default.
• W4310010382 cites W2336187603 @default.
• W4310010382 cites W2342214944 @default.
• W4310010382 cites W2344155946 @default.
• W4310010382 cites W2414133340 @default.
• W4310010382 cites W2465821637 @default.
• W4310010382 cites W2484591400 @default.
• W4310010382 cites W2517711249 @default.
• W4310010382 cites W2521614805 @default.
• W4310010382 cites W2561460856 @default.
• W4310010382 cites W2586237553 @default.
• W4310010382 cites W2811024290 @default.
• W4310010382 cites W2886983297 @default.
• W4310010382 cites W3126386170 @default.
• W4310010382 cites W3215013633 @default.
• W4310010382 cites W4250303119 @default.
• W4310010382 doi "https://doi.org/10.1080/19475705.2022.2149355" @default.
• W4310010382 hasPublicationYear "2022" @default.
• W4310010382 type Work @default.
• W4310010382 citedByCount "1" @default.
• W4310010382 countsByYear W43100103822023 @default.
• W4310010382 crossrefType "journal-article" @default.
• W4310010382 hasAuthorship W4310010382A5004821840 @default.
• W4310010382 hasAuthorship W4310010382A5046192421 @default.
• W4310010382 hasBestOaLocation W43100103821 @default.
• W4310010382 hasConcept C119217923 @default.
• W4310010382 hasConcept C120447056 @default.
• W4310010382 hasConcept C120806208 @default.
• W4310010382 hasConcept C121332964 @default.
• W4310010382 hasConcept C126691448 @default.
• W4310010382 hasConcept C127313418 @default.

• next