FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4224999623> ?p ?o ?g. }

• W4224999623 abstract "Abstract Geodetic evidence for slow slip recurrence changed by stress perturbations was rare, especially from afterslip following a nearby large earthquake. The first observed slow slip events in the southernmost Ryukyu subduction had occurred in 2005, 2009, and 2015 following the nearby 2002 March 31 M w 7.1 Hualien offshore earthquake. To investigate whether the M w 7.1 earthquake had influenced the occurrence times of the slow slip, we calculated the coseismic slip distribution and afterslip distribution using the surface displacements from onshore Global Navigation Satellite System observations. The stress perturbation on the slow-slip regions caused by the coseismic slip was quantified using the Coulomb failure criteria. We also examined the aftershock distribution and the evolution with time to clarify the stress perturbations from the afterslip offshore. Our results show that the primary afterslip distribution may have overlapped the 2009 and 2015 slow-slip patch at the downdip of the earthquake. The coseismic stress perturbation may have influenced the SSEs area directly by a Coulomb stress increase of probably 0.10 MPa. However, the 2005 SSE patch in the updip depths had only a little coseismic slip and afterslip with the Coulomb stress increase of approximately 0.06 MPa. We find that most of the aftershocks had occurred in the 2009 and 2015 slow-slip region that evolved into a typical aftershock sequence at least 2.5 years after the earthquake. The surface geodetic displacements reveal that the afterslip may have lasted longer than 4.5 years after the earthquake. The evidence for the afterslip proves that the 2009 and 2015 slow-slip patch was influenced by the afterslip directly for years. We suggest that the ongoing afterslip may have modulated the coseismic stress perturbation. It may explain the delay of the 2009 slow slip occurrence compared with the recurrence interval between the 2009 and 2015 slow slip events. Graphical Abstract" @default.
• W4224999623 created "2022-04-29" @default.
• W4224999623 creator A5022661423 @default.
• W4224999623 creator A5036497451 @default.
• W4224999623 creator A5086357318 @default.
• W4224999623 date "2022-04-26" @default.
• W4224999623 modified "2023-10-18" @default.
• W4224999623 title "Slow slip events following the afterslip of the 2002 Mw 7.1 Hualien offshore earthquake, Taiwan" @default.
• W4224999623 cites W1523600983 @default.
• W4224999623 cites W1602680895 @default.
• W4224999623 cites W1678049551 @default.
• W4224999623 cites W1782121173 @default.
• W4224999623 cites W1902125562 @default.
• W4224999623 cites W1985584663 @default.
• W4224999623 cites W1992363677 @default.
• W4224999623 cites W1997515029 @default.
• W4224999623 cites W1999211958 @default.
• W4224999623 cites W2017911693 @default.
• W4224999623 cites W2023016870 @default.
• W4224999623 cites W2048021555 @default.
• W4224999623 cites W2062811826 @default.
• W4224999623 cites W2066073101 @default.
• W4224999623 cites W2069711545 @default.
• W4224999623 cites W2078249512 @default.
• W4224999623 cites W2095675419 @default.
• W4224999623 cites W2100497023 @default.
• W4224999623 cites W2106567380 @default.
• W4224999623 cites W2108214772 @default.
• W4224999623 cites W2109105024 @default.
• W4224999623 cites W2130014760 @default.
• W4224999623 cites W2132483175 @default.
• W4224999623 cites W2137097669 @default.
• W4224999623 cites W2137433526 @default.
• W4224999623 cites W2142525864 @default.
• W4224999623 cites W2143737258 @default.
• W4224999623 cites W2152730464 @default.
• W4224999623 cites W2164987349 @default.
• W4224999623 cites W2170559182 @default.
• W4224999623 cites W2187891020 @default.
• W4224999623 cites W2278318545 @default.
• W4224999623 cites W2297963167 @default.
• W4224999623 cites W2401769219 @default.
• W4224999623 cites W2463536963 @default.
• W4224999623 cites W2609772108 @default.
• W4224999623 cites W2730539623 @default.
• W4224999623 cites W2754235049 @default.
• W4224999623 cites W2789246872 @default.
• W4224999623 cites W2791989626 @default.
• W4224999623 cites W2794811981 @default.
• W4224999623 cites W2804259338 @default.
• W4224999623 cites W2804276086 @default.
• W4224999623 cites W2894710397 @default.
• W4224999623 cites W2909838346 @default.
• W4224999623 cites W2947998320 @default.
• W4224999623 cites W2963072219 @default.
• W4224999623 cites W2991273975 @default.
• W4224999623 cites W2998259450 @default.
• W4224999623 cites W3016709413 @default.
• W4224999623 cites W3092489454 @default.
• W4224999623 cites W3094457323 @default.
• W4224999623 cites W3128929221 @default.
• W4224999623 cites W3159562292 @default.
• W4224999623 doi "https://doi.org/10.1186/s40623-022-01629-y" @default.
• W4224999623 hasPublicationYear "2022" @default.
• W4224999623 type Work @default.
• W4224999623 citedByCount "1" @default.
• W4224999623 countsByYear W42249996232022 @default.
• W4224999623 crossrefType "journal-article" @default.
• W4224999623 hasAuthorship W4224999623A5022661423 @default.
• W4224999623 hasAuthorship W4224999623A5036497451 @default.
• W4224999623 hasAuthorship W4224999623A5086357318 @default.
• W4224999623 hasBestOaLocation W42249996231 @default.
• W4224999623 hasConcept C121332964 @default.
• W4224999623 hasConcept C127313418 @default.
• W4224999623 hasConcept C13280743 @default.
• W4224999623 hasConcept C156801008 @default.
• W4224999623 hasConcept C162284963 @default.
• W4224999623 hasConcept C165205528 @default.
• W4224999623 hasConcept C187320778 @default.
• W4224999623 hasConcept C195268267 @default.
• W4224999623 hasConcept C58097730 @default.
• W4224999623 hasConcept C58754882 @default.
• W4224999623 hasConcept C63441156 @default.
• W4224999623 hasConcept C77928131 @default.
• W4224999623 hasConcept C97355855 @default.
• W4224999623 hasConceptScore W4224999623C121332964 @default.
• W4224999623 hasConceptScore W4224999623C127313418 @default.
• W4224999623 hasConceptScore W4224999623C13280743 @default.
• W4224999623 hasConceptScore W4224999623C156801008 @default.
• W4224999623 hasConceptScore W4224999623C162284963 @default.
• W4224999623 hasConceptScore W4224999623C165205528 @default.
• W4224999623 hasConceptScore W4224999623C187320778 @default.
• W4224999623 hasConceptScore W4224999623C195268267 @default.
• W4224999623 hasConceptScore W4224999623C58097730 @default.
• W4224999623 hasConceptScore W4224999623C58754882 @default.
• W4224999623 hasConceptScore W4224999623C63441156 @default.
• W4224999623 hasConceptScore W4224999623C77928131 @default.
• W4224999623 hasConceptScore W4224999623C97355855 @default.
• W4224999623 hasFunder F4320322795 @default.
• W4224999623 hasIssue "1" @default.

• next