FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2031131776> ?p ?o ?g. }

• W2031131776 endingPage "76" @default.
• W2031131776 startingPage "63" @default.
• W2031131776 abstract "Ground-rupturing earthquakes can generate tectonic knickpoints within upstream reaches of streams across active fault zones. These knickpoints are characteristic of upstream propagation of time-related process once generated by an earthquake, so analysis of knickpoint series in streams which cross fault zones can be used to infer paleoearthquake events. We studied the knickpoints along the Huoshan Piedmont Fault (HPF), which is an active normal fault in the Shanxi Faulted Basin zone, China, and demonstrate that analysis of knickpoints shows evidence for two paleoearthquakes in the HPF. First, we identified knickpoints in bedrock reaches upstream of the HPF using high-resolution DEMs derived from IRS-P5 stereo images and the stream-gradient method. After excluding non-faulting knickpoints, 47 knickpoints were identified in 23 bedrock reaches upstream from the HPF. Analysis of the most recent knickpoints caused by the 1303 CE Hongdong Earthquake allowed for local calibration of the retreat rates. Applying these retreat rates across the study area allows for the estimation of the age of other knickpoints, and constrains the age ranges of two knickpoint groups to be 2269–3336 a BP and 4504–5618 a BP. These ages constrain the ages of two paleoearthquake events at 2710 ± 102 and 4980 ± 646 a BP. The knickpoints along the HPF obey the parallel retreating model in which knickpoint morphology was roughly maintained during retreat, so the heights of knickpoints represent the coseismic vertical displacements generated by the earthquakes along the HPF. The vertical offsets for these three earthquake events are similar and are approximately 4 m, which indicates that the ruptures on the HPF obey a characteristic slip model with a similar slip distribution for several successive earthquakes. These results provide additional evidence of paleoearthquakes on the HPF and show that analysis of knickpoint recession along an active fault is a valuable tool for paleoseismology." @default.
• W2031131776 created "2016-06-24" @default.
• W2031131776 creator A5006374777 @default.
• W2031131776 creator A5009950031 @default.
• W2031131776 creator A5028701570 @default.
• W2031131776 creator A5089154798 @default.
• W2031131776 date "2015-04-01" @default.
• W2031131776 modified "2023-10-14" @default.
• W2031131776 title "Evaluating knickpoint recession along an active fault for paleoseismological analysis: The Huoshan Piedmont, Eastern China" @default.
• W2031131776 cites W1484043399 @default.
• W2031131776 cites W1967502633 @default.
• W2031131776 cites W1971955535 @default.
• W2031131776 cites W1976793706 @default.
• W2031131776 cites W1976822911 @default.
• W2031131776 cites W1986082054 @default.
• W2031131776 cites W1993999355 @default.
• W2031131776 cites W2002298668 @default.
• W2031131776 cites W2008507930 @default.
• W2031131776 cites W2016784021 @default.
• W2031131776 cites W2020364089 @default.
• W2031131776 cites W2024543196 @default.
• W2031131776 cites W2037197962 @default.
• W2031131776 cites W2043826213 @default.
• W2031131776 cites W2058460811 @default.
• W2031131776 cites W2066166725 @default.
• W2031131776 cites W2071237400 @default.
• W2031131776 cites W2076062906 @default.
• W2031131776 cites W2077375337 @default.
• W2031131776 cites W2088349978 @default.
• W2031131776 cites W2094475308 @default.
• W2031131776 cites W2095533311 @default.
• W2031131776 cites W2104300819 @default.
• W2031131776 cites W2106776897 @default.
• W2031131776 cites W2113148021 @default.
• W2031131776 cites W2113482505 @default.
• W2031131776 cites W2123112468 @default.
• W2031131776 cites W2140403093 @default.
• W2031131776 cites W2140709557 @default.
• W2031131776 cites W2146098810 @default.
• W2031131776 cites W2155880045 @default.
• W2031131776 cites W2157352574 @default.
• W2031131776 cites W2160189413 @default.
• W2031131776 cites W2161634485 @default.
• W2031131776 cites W2162495231 @default.
• W2031131776 cites W2162798797 @default.
• W2031131776 cites W2331643441 @default.
• W2031131776 cites W2335732884 @default.
• W2031131776 doi "https://doi.org/10.1016/j.geomorph.2015.01.013" @default.
• W2031131776 hasPublicationYear "2015" @default.
• W2031131776 type Work @default.
• W2031131776 sameAs 2031131776 @default.
• W2031131776 citedByCount "16" @default.
• W2031131776 countsByYear W20311317762016 @default.
• W2031131776 countsByYear W20311317762017 @default.
• W2031131776 countsByYear W20311317762018 @default.
• W2031131776 countsByYear W20311317762019 @default.
• W2031131776 countsByYear W20311317762020 @default.
• W2031131776 countsByYear W20311317762021 @default.
• W2031131776 countsByYear W20311317762022 @default.
• W2031131776 crossrefType "journal-article" @default.
• W2031131776 hasAuthorship W2031131776A5006374777 @default.
• W2031131776 hasAuthorship W2031131776A5009950031 @default.
• W2031131776 hasAuthorship W2031131776A5028701570 @default.
• W2031131776 hasAuthorship W2031131776A5089154798 @default.
• W2031131776 hasConcept C114793014 @default.
• W2031131776 hasConcept C127313418 @default.
• W2031131776 hasConcept C137527640 @default.
• W2031131776 hasConcept C165205528 @default.
• W2031131776 hasConcept C175551986 @default.
• W2031131776 hasConcept C26001220 @default.
• W2031131776 hasConcept C2777322221 @default.
• W2031131776 hasConcept C31258907 @default.
• W2031131776 hasConcept C41008148 @default.
• W2031131776 hasConcept C42090638 @default.
• W2031131776 hasConcept C77928131 @default.
• W2031131776 hasConceptScore W2031131776C114793014 @default.
• W2031131776 hasConceptScore W2031131776C127313418 @default.
• W2031131776 hasConceptScore W2031131776C137527640 @default.
• W2031131776 hasConceptScore W2031131776C165205528 @default.
• W2031131776 hasConceptScore W2031131776C175551986 @default.
• W2031131776 hasConceptScore W2031131776C26001220 @default.
• W2031131776 hasConceptScore W2031131776C2777322221 @default.
• W2031131776 hasConceptScore W2031131776C31258907 @default.
• W2031131776 hasConceptScore W2031131776C41008148 @default.
• W2031131776 hasConceptScore W2031131776C42090638 @default.
• W2031131776 hasConceptScore W2031131776C77928131 @default.
• W2031131776 hasFunder F4320321001 @default.
• W2031131776 hasLocation W20311317761 @default.
• W2031131776 hasOpenAccess W2031131776 @default.
• W2031131776 hasPrimaryLocation W20311317761 @default.
• W2031131776 hasRelatedWork W1980641233 @default.
• W2031131776 hasRelatedWork W2008590108 @default.
• W2031131776 hasRelatedWork W2020535921 @default.
• W2031131776 hasRelatedWork W2035860361 @default.
• W2031131776 hasRelatedWork W2314337543 @default.
• W2031131776 hasRelatedWork W2314502293 @default.
• W2031131776 hasRelatedWork W2361882407 @default.
• W2031131776 hasRelatedWork W2733843701 @default.

• next