FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2071613527> ?p ?o ?g. }

• W2071613527 endingPage "15349" @default.
• W2071613527 startingPage "15333" @default.
• W2071613527 abstract "It is found that the initial rise of far-field P wave velocity pulses generated by microearthquakes is not well represented by a ramp function but exhibits a gradual increase according to the function tn (2 < n < 4), where t is the time measured from the onset of the P wave. This slow rise, termed the slow initial phase, is detected in all 69 earthquakes analyzed here. Their seismic moments range between 108 and 1013 N m. No ramplike onsets are observed, suggesting that the slow rise is not an anomalous feature but is always generated by earthquakes of this size. The slow initial phase is not due to the transient response of the recording system. Analyses and simulations suggest that the slow initial phase is also not likely to result from an inhomogenuous velocity structure but that it may be partly due to anelastic attenuation. The slow initial phase likely results from the source process of the microearthquakes, especially those instances of the phase with a longer duration. The slow initial phase can not be explained by theoretical source models which assume constant dynamic friction and rupture velocity in an expanding fault. This is because these models predict a ramplike behavior in the initial rise of the far-field P wave velocity pulse. Only the observed ramplike waveform following the slow initial phase can be explained by these models. The slow initial phase can be explained by models which predict slow slip velocities and/or rupture velocities immediately after rupture initiation, such as the slip-weakening crack model. The duration of the slow initial phase is proportional to the rise time of the P wave velocity pulse. This dependence implies that longer, slow initial phases are generated by larger earthquakes, the duration of the slow initial phase being a measure of the earthquake size." @default.
• W2071613527 created "2016-06-24" @default.
• W2071613527 creator A5091910194 @default.
• W2071613527 date "1995-08-10" @default.
• W2071613527 modified "2023-10-18" @default.
• W2071613527 title "Observations of the slow initial phase generated by microearthquakes: Implications for earthquake nucleation and propagation" @default.
• W2071613527 cites W1602744129 @default.
• W2071613527 cites W1963519252 @default.
• W2071613527 cites W1972009047 @default.
• W2071613527 cites W1986162310 @default.
• W2071613527 cites W1990660369 @default.
• W2071613527 cites W2013185482 @default.
• W2071613527 cites W2014390878 @default.
• W2071613527 cites W2015939216 @default.
• W2071613527 cites W2017431651 @default.
• W2071613527 cites W2019549988 @default.
• W2071613527 cites W2019935798 @default.
• W2071613527 cites W2037168657 @default.
• W2071613527 cites W2058413866 @default.
• W2071613527 cites W2059727200 @default.
• W2071613527 cites W2067875830 @default.
• W2071613527 cites W2071666675 @default.
• W2071613527 cites W2072471924 @default.
• W2071613527 cites W2073182257 @default.
• W2071613527 cites W2077011746 @default.
• W2071613527 cites W2087000113 @default.
• W2071613527 cites W2093509339 @default.
• W2071613527 cites W2106919751 @default.
• W2071613527 cites W2110574886 @default.
• W2071613527 cites W2170362286 @default.
• W2071613527 doi "https://doi.org/10.1029/95jb01150" @default.
• W2071613527 hasPublicationYear "1995" @default.
• W2071613527 type Work @default.
• W2071613527 sameAs 2071613527 @default.
• W2071613527 citedByCount "107" @default.
• W2071613527 countsByYear W20716135272013 @default.
• W2071613527 countsByYear W20716135272014 @default.
• W2071613527 countsByYear W20716135272015 @default.
• W2071613527 countsByYear W20716135272016 @default.
• W2071613527 countsByYear W20716135272017 @default.
• W2071613527 countsByYear W20716135272018 @default.
• W2071613527 countsByYear W20716135272019 @default.
• W2071613527 countsByYear W20716135272020 @default.
• W2071613527 countsByYear W20716135272021 @default.
• W2071613527 countsByYear W20716135272022 @default.
• W2071613527 countsByYear W20716135272023 @default.
• W2071613527 crossrefType "journal-article" @default.
• W2071613527 hasAuthorship W2071613527A5091910194 @default.
• W2071613527 hasConcept C121332964 @default.
• W2071613527 hasConcept C127313418 @default.
• W2071613527 hasConcept C147412999 @default.
• W2071613527 hasConcept C156801008 @default.
• W2071613527 hasConcept C165205528 @default.
• W2071613527 hasConcept C44280652 @default.
• W2071613527 hasConcept C61048295 @default.
• W2071613527 hasConcept C62520636 @default.
• W2071613527 hasConcept C8058405 @default.
• W2071613527 hasConcept C97355855 @default.
• W2071613527 hasConceptScore W2071613527C121332964 @default.
• W2071613527 hasConceptScore W2071613527C127313418 @default.
• W2071613527 hasConceptScore W2071613527C147412999 @default.
• W2071613527 hasConceptScore W2071613527C156801008 @default.
• W2071613527 hasConceptScore W2071613527C165205528 @default.
• W2071613527 hasConceptScore W2071613527C44280652 @default.
• W2071613527 hasConceptScore W2071613527C61048295 @default.
• W2071613527 hasConceptScore W2071613527C62520636 @default.
• W2071613527 hasConceptScore W2071613527C8058405 @default.
• W2071613527 hasConceptScore W2071613527C97355855 @default.
• W2071613527 hasIssue "B8" @default.
• W2071613527 hasLocation W20716135271 @default.
• W2071613527 hasOpenAccess W2071613527 @default.
• W2071613527 hasPrimaryLocation W20716135271 @default.
• W2071613527 hasRelatedWork W1968107979 @default.
• W2071613527 hasRelatedWork W1969245073 @default.
• W2071613527 hasRelatedWork W1970193186 @default.
• W2071613527 hasRelatedWork W2069039421 @default.
• W2071613527 hasRelatedWork W2344103485 @default.
• W2071613527 hasRelatedWork W2371527909 @default.
• W2071613527 hasRelatedWork W2376149826 @default.
• W2071613527 hasRelatedWork W2626964047 @default.
• W2071613527 hasRelatedWork W2904667922 @default.
• W2071613527 hasRelatedWork W3036113227 @default.
• W2071613527 hasVolume "100" @default.
• W2071613527 isParatext "false" @default.
• W2071613527 isRetracted "false" @default.
• W2071613527 magId "2071613527" @default.
• W2071613527 workType "article" @default.