FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2077961034> ?p ?o ?g. }

• W2077961034 endingPage "8101" @default.
• W2077961034 startingPage "8079" @default.
• W2077961034 abstract "From four years of Global Positioning System (GPS) measurements, we find significant spatial variations in present-day deformation between the eastern and western Kenai Peninsula, Alaska. Sites in the eastern Kenai Peninsula and Prince William Sound move to the NNW relative to North America, in the direction of Pacific-North America relative plate motion. Velocities decrease in magnitude from nearly the full plate rate in southern Prince William Sound to about 30 mm/yr at Seward and to about 5 mm/yr near Anchorage. In contrast, sites in the western Kenai Peninsula move to the SW, in a nearly trenchward direction, with a velocity of about 20 mm/yr. The data are consistent with the shallow plate interface offshore and beneath the eastern Kenai and Prince William Sound being completely locked or nearly so, with elastic strain accumulation resulting in rapid motion in the direction of relative plate motion of sites in the overriding plate. The velocities of sites in the western Kenai, along strike to the southwest, are opposite in sign with those predicted from elastic strain accumulation. These data are incompatible with a significant locked region in this segment of the plate boundary. Trenchward velocities are found also for some sites in the Anchorage area. We interpret the trenchward velocities as being caused by a continuing postseismic transient from the 1964 great Alaska earthquake. There may be significant along-strike differences in the long-term behavior of the plate interface between the western and eastern Kenai, based on roughly coincident boundaries in the coseismic slip distribution, cumulative postseismic uplift, present-day plate coupling, and stress field. The present postseismic response appears to generate purely trenchward motion, suggesting a creep process that is purely dip slip. Our observations suggest that postseismic processes after the largest earthquakes can influence patterns of deformation for decades after the event." @default.
• W2077961034 created "2016-06-24" @default.
• W2077961034 creator A5028443075 @default.
• W2077961034 creator A5073557562 @default.
• W2077961034 creator A5083963054 @default.
• W2077961034 date "2000-04-10" @default.
• W2077961034 modified "2023-09-27" @default.
• W2077961034 title "Spatial variations in present-day deformation, Kenai Peninsula, Alaska, and their implications" @default.
• W2077961034 cites W1481158429 @default.
• W2077961034 cites W1628786483 @default.
• W2077961034 cites W1964948897 @default.
• W2077961034 cites W1966781131 @default.
• W2077961034 cites W1978215130 @default.
• W2077961034 cites W1980158135 @default.
• W2077961034 cites W1988018815 @default.
• W2077961034 cites W1993182720 @default.
• W2077961034 cites W1998395256 @default.
• W2077961034 cites W2002707883 @default.
• W2077961034 cites W2002921523 @default.
• W2077961034 cites W2006915059 @default.
• W2077961034 cites W2009056327 @default.
• W2077961034 cites W2015215934 @default.
• W2077961034 cites W2018137477 @default.
• W2077961034 cites W2018139159 @default.
• W2077961034 cites W2024754990 @default.
• W2077961034 cites W2027748507 @default.
• W2077961034 cites W2034314180 @default.
• W2077961034 cites W2041580614 @default.
• W2077961034 cites W2042109125 @default.
• W2077961034 cites W2042521829 @default.
• W2077961034 cites W2046183170 @default.
• W2077961034 cites W2057371440 @default.
• W2077961034 cites W2059857770 @default.
• W2077961034 cites W2059982963 @default.
• W2077961034 cites W2060803307 @default.
• W2077961034 cites W2085899680 @default.
• W2077961034 cites W2087294328 @default.
• W2077961034 cites W2088119000 @default.
• W2077961034 cites W2088720485 @default.
• W2077961034 cites W2089481299 @default.
• W2077961034 cites W2091141572 @default.
• W2077961034 cites W2093338977 @default.
• W2077961034 cites W2093983895 @default.
• W2077961034 cites W2100345004 @default.
• W2077961034 cites W2105753666 @default.
• W2077961034 cites W2108053734 @default.
• W2077961034 cites W2118887722 @default.
• W2077961034 cites W2124288810 @default.
• W2077961034 cites W2124799255 @default.
• W2077961034 cites W2125030808 @default.
• W2077961034 cites W2127150969 @default.
• W2077961034 cites W2127972904 @default.
• W2077961034 cites W2130014760 @default.
• W2077961034 cites W2130833734 @default.
• W2077961034 cites W2146799928 @default.
• W2077961034 cites W2151580336 @default.
• W2077961034 cites W2164476182 @default.
• W2077961034 cites W2268723567 @default.
• W2077961034 cites W4246266861 @default.
• W2077961034 cites W4251074303 @default.
• W2077961034 cites W4252074023 @default.
• W2077961034 cites W966372214 @default.
• W2077961034 doi "https://doi.org/10.1029/1999jb900388" @default.
• W2077961034 hasPublicationYear "2000" @default.
• W2077961034 type Work @default.
• W2077961034 sameAs 2077961034 @default.
• W2077961034 citedByCount "102" @default.
• W2077961034 countsByYear W20779610342012 @default.
• W2077961034 countsByYear W20779610342013 @default.
• W2077961034 countsByYear W20779610342014 @default.
• W2077961034 countsByYear W20779610342015 @default.
• W2077961034 countsByYear W20779610342017 @default.
• W2077961034 countsByYear W20779610342018 @default.
• W2077961034 countsByYear W20779610342020 @default.
• W2077961034 countsByYear W20779610342021 @default.
• W2077961034 countsByYear W20779610342022 @default.
• W2077961034 countsByYear W20779610342023 @default.
• W2077961034 crossrefType "journal-article" @default.
• W2077961034 hasAuthorship W2077961034A5028443075 @default.
• W2077961034 hasAuthorship W2077961034A5073557562 @default.
• W2077961034 hasAuthorship W2077961034A5083963054 @default.
• W2077961034 hasBestOaLocation W20779610341 @default.
• W2077961034 hasConcept C111368507 @default.
• W2077961034 hasConcept C119477230 @default.
• W2077961034 hasConcept C123588078 @default.
• W2077961034 hasConcept C127313418 @default.
• W2077961034 hasConcept C13280743 @default.
• W2077961034 hasConcept C162284963 @default.
• W2077961034 hasConcept C165205528 @default.
• W2077961034 hasConcept C166957645 @default.
• W2077961034 hasConcept C205649164 @default.
• W2077961034 hasConcept C2777992645 @default.
• W2077961034 hasConcept C77928131 @default.
• W2077961034 hasConceptScore W2077961034C111368507 @default.
• W2077961034 hasConceptScore W2077961034C119477230 @default.
• W2077961034 hasConceptScore W2077961034C123588078 @default.
• W2077961034 hasConceptScore W2077961034C127313418 @default.
• W2077961034 hasConceptScore W2077961034C13280743 @default.

• next