FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3152571856> ?p ?o ?g. }

• W3152571856 endingPage "1598" @default.
• W3152571856 startingPage "1584" @default.
• W3152571856 abstract "SUMMARY This study introduces a novel method for computing post-seismic crustal internal deformation in a layered earth model. The surface dislocation Love number (DLN) calculated by the reciprocity theorem was implemented as the initial value. Furthermore, numerical integration of the value from the Earth's surface to the interior was undertaken to obtain the internal DLN. This method does not require a combination of the general solution and particular solution for the calculation of internal deformation above the seismic source, thus avoiding the loss of precision. When the post-seismic deformation within a certain period is calculated, the particular solutions at the beginning and end of the considered period cancel each other. This simplifies the calculation of post-seismic internal deformation. The numerical results depict that as the degrees increase, the post-seismic DLN reaches stability in a shorter interval of time. Thus, for improved efficiency of the post-seismic internal deformation calculation, the post-seismic DLNs should be calculated within 2000 degree and integrated with the coseismic results. As an application, the post-seismic Coulomb failure stress changes (∆CFS) induced by the 2011 Tohoku-Oki earthquake in the near field around the Japanese archipelagos and two major faults in Northeast China were simulated. The results exhibit that the ∆CFS values in the near field agree well with those simulated by the method in a half-space layered earth model, thus verifying the present method. The coseismic ∆CFS on the Mishan-Dunhua fault in Northeast China, as an example, is only 0.094–0.668 KPa. However, the ∆CFS caused by the viscoelastic relaxation of the mantle within 5 yr following the 2011 Tohoku-Oki event on the same fault exceeds the coseismic results. Therefore, the cumulative effect of the viscoelastic relaxation of the mantle is deserving of attention." @default.
• W3152571856 created "2021-04-26" @default.
• W3152571856 creator A5003944303 @default.
• W3152571856 creator A5010268194 @default.
• W3152571856 creator A5028543289 @default.
• W3152571856 creator A5044264026 @default.
• W3152571856 date "2021-04-20" @default.
• W3152571856 modified "2023-10-17" @default.
• W3152571856 title "Post-seismic crustal internal deformation in a layered earth model" @default.
• W3152571856 cites W1682486987 @default.
• W3152571856 cites W1807213132 @default.
• W3152571856 cites W1852251098 @default.
• W3152571856 cites W1968460897 @default.
• W3152571856 cites W1976815700 @default.
• W3152571856 cites W1987651695 @default.
• W3152571856 cites W1990113089 @default.
• W3152571856 cites W1993648481 @default.
• W3152571856 cites W1994299295 @default.
• W3152571856 cites W1994576411 @default.
• W3152571856 cites W1995307791 @default.
• W3152571856 cites W1995666401 @default.
• W3152571856 cites W2013048085 @default.
• W3152571856 cites W2015109328 @default.
• W3152571856 cites W2015906752 @default.
• W3152571856 cites W2017611649 @default.
• W3152571856 cites W2022029674 @default.
• W3152571856 cites W2023244927 @default.
• W3152571856 cites W2031967575 @default.
• W3152571856 cites W2032693459 @default.
• W3152571856 cites W2046569337 @default.
• W3152571856 cites W2051984084 @default.
• W3152571856 cites W2053570564 @default.
• W3152571856 cites W2062221814 @default.
• W3152571856 cites W2082476880 @default.
• W3152571856 cites W2085424666 @default.
• W3152571856 cites W2095290719 @default.
• W3152571856 cites W2100590912 @default.
• W3152571856 cites W2105347446 @default.
• W3152571856 cites W2112931705 @default.
• W3152571856 cites W2117094675 @default.
• W3152571856 cites W2121551303 @default.
• W3152571856 cites W2135726590 @default.
• W3152571856 cites W2152608994 @default.
• W3152571856 cites W2156721705 @default.
• W3152571856 cites W2157520698 @default.
• W3152571856 cites W2159965811 @default.
• W3152571856 cites W2164416744 @default.
• W3152571856 cites W2207005762 @default.
• W3152571856 cites W2225203902 @default.
• W3152571856 cites W2278318545 @default.
• W3152571856 cites W2327793839 @default.
• W3152571856 cites W2330083913 @default.
• W3152571856 cites W2555095717 @default.
• W3152571856 cites W2593204517 @default.
• W3152571856 cites W2605991614 @default.
• W3152571856 cites W2806792168 @default.
• W3152571856 cites W2807801951 @default.
• W3152571856 cites W2893726365 @default.
• W3152571856 cites W2902994044 @default.
• W3152571856 cites W2920345792 @default.
• W3152571856 cites W2923627075 @default.
• W3152571856 cites W2926465753 @default.
• W3152571856 cites W2944057909 @default.
• W3152571856 cites W2971256678 @default.
• W3152571856 cites W3008090114 @default.
• W3152571856 cites W3037369261 @default.
• W3152571856 doi "https://doi.org/10.1093/gji/ggab156" @default.
• W3152571856 hasPublicationYear "2021" @default.
• W3152571856 type Work @default.
• W3152571856 sameAs 3152571856 @default.
• W3152571856 citedByCount "2" @default.
• W3152571856 countsByYear W31525718562022 @default.
• W3152571856 countsByYear W31525718562023 @default.
• W3152571856 crossrefType "journal-article" @default.
• W3152571856 hasAuthorship W3152571856A5003944303 @default.
• W3152571856 hasAuthorship W3152571856A5010268194 @default.
• W3152571856 hasAuthorship W3152571856A5028543289 @default.
• W3152571856 hasAuthorship W3152571856A5044264026 @default.
• W3152571856 hasConcept C111368507 @default.
• W3152571856 hasConcept C127313418 @default.
• W3152571856 hasConcept C13280743 @default.
• W3152571856 hasConcept C136752280 @default.
• W3152571856 hasConcept C165205528 @default.
• W3152571856 hasConcept C204366326 @default.
• W3152571856 hasConcept C2993668338 @default.
• W3152571856 hasConcept C77928131 @default.
• W3152571856 hasConcept C78542244 @default.
• W3152571856 hasConcept C8058405 @default.
• W3152571856 hasConceptScore W3152571856C111368507 @default.
• W3152571856 hasConceptScore W3152571856C127313418 @default.
• W3152571856 hasConceptScore W3152571856C13280743 @default.
• W3152571856 hasConceptScore W3152571856C136752280 @default.
• W3152571856 hasConceptScore W3152571856C165205528 @default.
• W3152571856 hasConceptScore W3152571856C204366326 @default.
• W3152571856 hasConceptScore W3152571856C2993668338 @default.
• W3152571856 hasConceptScore W3152571856C77928131 @default.
• W3152571856 hasConceptScore W3152571856C78542244 @default.
• W3152571856 hasConceptScore W3152571856C8058405 @default.

• next