FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2030448034> ?p ?o ?g. }

• W2030448034 endingPage "266" @default.
• W2030448034 startingPage "255" @default.
• W2030448034 abstract "An earthquake of Ms=6.1 devastated the town of Dinar (SW Turkey, population 35,000) on October 1, 1995, killing 90 people and destroying 30% of the town. The earthquake generated complex body-waveforms varying with azimuth at teleseismic distances. The method of complex body-waveform inversion developed by Kikuchi and Kanamori (1991)was used to infer a source process for the earthquake. Two subevents were necessary to explain the observed seismic records. The inversion result suggests that the Dinar earthquake initiated at the SE end of the Dinar fault with a subevent of seismic moment Mo=0.5×1018 N m. Six seconds later, the second subevent took place about 10 km to the northwest of the first subevent with a seismic moment a few times larger than the first. The CMT depths of the first and second subevents were found to be 10 and 15 km, respectively. Both subevents had a predominantly normal faulting mechanism with slip-vectors oriented NE–SW, showing good agreement with the velocity-vectors obtained from the recent SLR and GPS studies as well as with the regional stress orientation obtained from geological data. The main shock was preceded by foreshock activity concentrated at the SE end of the Dinar fault where the first subevent took place, while the aftershock activity was concentrated in the vicinity of the second subevent. The spatial distribution of the foreshock and the aftershock activities and the locations of the subevents suggest that the first subevent broke an asperity and the second subevent broke a barrier on the fault, following the definition by Aki (1984)of an asperity and barrier earthquake model. About 10 km of surface ruptures were associated with the earthquake while the estimates yield a rupture length of 25 km. The calculated source parameters of the subevents and their locations suggest that the surface ruptures were probably associated with the first subevent. The estimates also show that the rupture zones of the two subevents overlapped where the maximum vertical displacement was observed." @default.
• W2030448034 created "2016-06-24" @default.
• W2030448034 creator A5068770852 @default.
• W2030448034 date "1998-07-01" @default.
• W2030448034 modified "2023-10-14" @default.
• W2030448034 title "Source inversion of the October 1, 1995, Dinar earthquake (Ms=6.1): a rupture model with implications for seismotectonics in SW Turkey" @default.
• W2030448034 cites W1994553199 @default.
• W2030448034 cites W2003387798 @default.
• W2030448034 cites W2033237879 @default.
• W2030448034 cites W2040016349 @default.
• W2030448034 cites W2062905566 @default.
• W2030448034 cites W2070942674 @default.
• W2030448034 cites W2079224749 @default.
• W2030448034 cites W2086502719 @default.
• W2030448034 cites W2090863471 @default.
• W2030448034 cites W2103102619 @default.
• W2030448034 cites W2122341820 @default.
• W2030448034 cites W2154259004 @default.
• W2030448034 cites W2154476000 @default.
• W2030448034 cites W2166074915 @default.
• W2030448034 cites W2275750751 @default.
• W2030448034 cites W4230141448 @default.
• W2030448034 doi "https://doi.org/10.1016/s0040-1951(98)00056-0" @default.
• W2030448034 hasPublicationYear "1998" @default.
• W2030448034 type Work @default.
• W2030448034 sameAs 2030448034 @default.
• W2030448034 citedByCount "36" @default.
• W2030448034 countsByYear W20304480342013 @default.
• W2030448034 countsByYear W20304480342014 @default.
• W2030448034 countsByYear W20304480342015 @default.
• W2030448034 countsByYear W20304480342016 @default.
• W2030448034 countsByYear W20304480342018 @default.
• W2030448034 countsByYear W20304480342019 @default.
• W2030448034 countsByYear W20304480342021 @default.
• W2030448034 crossrefType "journal-article" @default.
• W2030448034 hasAuthorship W2030448034A5068770852 @default.
• W2030448034 hasConcept C111357193 @default.
• W2030448034 hasConcept C127313418 @default.
• W2030448034 hasConcept C128954607 @default.
• W2030448034 hasConcept C13280743 @default.
• W2030448034 hasConcept C147412999 @default.
• W2030448034 hasConcept C156801008 @default.
• W2030448034 hasConcept C165205528 @default.
• W2030448034 hasConcept C58097730 @default.
• W2030448034 hasConcept C60859754 @default.
• W2030448034 hasConcept C77928131 @default.
• W2030448034 hasConcept C83176761 @default.
• W2030448034 hasConceptScore W2030448034C111357193 @default.
• W2030448034 hasConceptScore W2030448034C127313418 @default.
• W2030448034 hasConceptScore W2030448034C128954607 @default.
• W2030448034 hasConceptScore W2030448034C13280743 @default.
• W2030448034 hasConceptScore W2030448034C147412999 @default.
• W2030448034 hasConceptScore W2030448034C156801008 @default.
• W2030448034 hasConceptScore W2030448034C165205528 @default.
• W2030448034 hasConceptScore W2030448034C58097730 @default.
• W2030448034 hasConceptScore W2030448034C60859754 @default.
• W2030448034 hasConceptScore W2030448034C77928131 @default.
• W2030448034 hasConceptScore W2030448034C83176761 @default.
• W2030448034 hasIssue "3-4" @default.
• W2030448034 hasLocation W20304480341 @default.
• W2030448034 hasOpenAccess W2030448034 @default.
• W2030448034 hasPrimaryLocation W20304480341 @default.
• W2030448034 hasRelatedWork W1186069267 @default.
• W2030448034 hasRelatedWork W1972729006 @default.
• W2030448034 hasRelatedWork W2354361330 @default.
• W2030448034 hasRelatedWork W2383859543 @default.
• W2030448034 hasRelatedWork W2410706959 @default.
• W2030448034 hasRelatedWork W2501006237 @default.
• W2030448034 hasRelatedWork W3154768851 @default.
• W2030448034 hasRelatedWork W4220899651 @default.
• W2030448034 hasRelatedWork W4307201599 @default.
• W2030448034 hasRelatedWork W2224509018 @default.
• W2030448034 hasVolume "292" @default.
• W2030448034 isParatext "false" @default.
• W2030448034 isRetracted "false" @default.
• W2030448034 magId "2030448034" @default.
• W2030448034 workType "article" @default.