FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2026020959> ?p ?o ?g. }

• W2026020959 endingPage "12455" @default.
• W2026020959 startingPage "12437" @default.
• W2026020959 abstract "A Global Positioning System (GPS) fixed‐point network has been operating in the Kanto and Tokai districts of central Japan since April 1988 to detect crustal deformation associated with the convergence of the Eurasian, Pacific, North American, and Philippine Sea plates and to monitor the deformation cycles of frequent large interplate and intraplate earthquakes. This 10‐station network established by the National Research Institute for Earth Science and Disaster Prevention (NIED) is the first continuously monitoring network of its kind. We determine deformation within the network using two consecutive days of data every 2 weeks for the first 17 months of operations. We use a station and orbit relaxation method which relies exclusively on data collected within the NIED network, except for 1 week of global GPS tracking data which is used to determine initial station positions with respect to the global reference frame. We detect, relative to a station on the Eurasian plate in central Japan, significant westward motion of 28 mm/yr of the northern tip of the Philippine Sea plate, which is subducting beneath the Eurasian plate at the Suruga trough. Our results support finite element models of collision of the Izu Block with the Eurasian plate based on earthquake focal mechanisms and plate block motions of the Japanese archipelago determined from conventional geodetic measurements over the last century. We detect southwestward motion of 18 mm/yr of the southeastern tip of the Eurasian plate, confirming expected surface extension of the subducted plate parallel to the Suruga trough axis. Significant vertical uplift with a velocity of 20 mm/yr is suggested at a site inland of the Tokai district located in the Akaishi uplift zone and at a site on Hatsushima Island in Sagami Bay. The general tendency of vertical movements of the other sites agrees with vertical velocities obtained from 70 years of geodetic leveling and with Quaternary vertical displacements determined from geomorphological and other geological evidence. We detect no significant crustal motion across the Fossa Magna tectonic zone in central Japan (often considered a plate boundary), across the Tokyo metropolitan area, nor across the Sagami trough associated with the subduction of the Philippine Sea plate beneath northeast Japan. Our results demonstrate the power of regionally based, continuously monitoring GPS networks for obtaining temporally dense measurements of small horizontal and vertical crustal movements across plate boundary zones." @default.
• W2026020959 created "2016-06-24" @default.
• W2026020959 creator A5001535652 @default.
• W2026020959 creator A5075643989 @default.
• W2026020959 date "1992-08-10" @default.
• W2026020959 modified "2023-10-14" @default.
• W2026020959 title "Crustal deformation measurements in central Japan determined by a Global Positioning System Fixed-Point Network" @default.
• W2026020959 cites W1482656233 @default.
• W2026020959 cites W153430466 @default.
• W2026020959 cites W1535176033 @default.
• W2026020959 cites W1557757940 @default.
• W2026020959 cites W1581277002 @default.
• W2026020959 cites W1968624392 @default.
• W2026020959 cites W1974437027 @default.
• W2026020959 cites W1978031872 @default.
• W2026020959 cites W1981434941 @default.
• W2026020959 cites W1984984876 @default.
• W2026020959 cites W1994390074 @default.
• W2026020959 cites W1999138223 @default.
• W2026020959 cites W2002557257 @default.
• W2026020959 cites W2003342124 @default.
• W2026020959 cites W2005711414 @default.
• W2026020959 cites W2011868168 @default.
• W2026020959 cites W2016925785 @default.
• W2026020959 cites W2024930506 @default.
• W2026020959 cites W2030653222 @default.
• W2026020959 cites W2034344709 @default.
• W2026020959 cites W2042559327 @default.
• W2026020959 cites W2058214451 @default.
• W2026020959 cites W2059243396 @default.
• W2026020959 cites W2061192341 @default.
• W2026020959 cites W2072834938 @default.
• W2026020959 cites W2073343424 @default.
• W2026020959 cites W2075063784 @default.
• W2026020959 cites W2078401172 @default.
• W2026020959 cites W2081524105 @default.
• W2026020959 cites W2085008024 @default.
• W2026020959 cites W2086388914 @default.
• W2026020959 cites W2086619209 @default.
• W2026020959 cites W2087028515 @default.
• W2026020959 cites W2088171772 @default.
• W2026020959 cites W2098328952 @default.
• W2026020959 cites W2104309496 @default.
• W2026020959 cites W2119486063 @default.
• W2026020959 cites W2135494568 @default.
• W2026020959 cites W2142536098 @default.
• W2026020959 cites W2154869018 @default.
• W2026020959 cites W2250096065 @default.
• W2026020959 cites W2330879602 @default.
• W2026020959 cites W2331350453 @default.
• W2026020959 cites W2509714098 @default.
• W2026020959 cites W2549153544 @default.
• W2026020959 cites W2605377780 @default.
• W2026020959 cites W2605479932 @default.
• W2026020959 cites W2605779101 @default.
• W2026020959 cites W71396898 @default.
• W2026020959 doi "https://doi.org/10.1029/92jb00809" @default.
• W2026020959 hasPublicationYear "1992" @default.
• W2026020959 type Work @default.
• W2026020959 sameAs 2026020959 @default.
• W2026020959 citedByCount "44" @default.
• W2026020959 countsByYear W20260209592013 @default.
• W2026020959 countsByYear W20260209592014 @default.
• W2026020959 countsByYear W20260209592017 @default.
• W2026020959 countsByYear W20260209592020 @default.
• W2026020959 countsByYear W20260209592021 @default.
• W2026020959 crossrefType "journal-article" @default.
• W2026020959 hasAuthorship W2026020959A5001535652 @default.
• W2026020959 hasAuthorship W2026020959A5075643989 @default.
• W2026020959 hasConcept C111368507 @default.
• W2026020959 hasConcept C119477230 @default.
• W2026020959 hasConcept C127313418 @default.
• W2026020959 hasConcept C13280743 @default.
• W2026020959 hasConcept C139719470 @default.
• W2026020959 hasConcept C14279187 @default.
• W2026020959 hasConcept C154839486 @default.
• W2026020959 hasConcept C162324750 @default.
• W2026020959 hasConcept C165205528 @default.
• W2026020959 hasConcept C202511199 @default.
• W2026020959 hasConcept C204207459 @default.
• W2026020959 hasConcept C204366326 @default.
• W2026020959 hasConcept C2777992645 @default.
• W2026020959 hasConcept C2777994876 @default.
• W2026020959 hasConcept C2778261408 @default.
• W2026020959 hasConcept C32239851 @default.
• W2026020959 hasConcept C41008148 @default.
• W2026020959 hasConcept C58097730 @default.
• W2026020959 hasConcept C58754882 @default.
• W2026020959 hasConcept C60229501 @default.
• W2026020959 hasConcept C76155785 @default.
• W2026020959 hasConcept C77928131 @default.
• W2026020959 hasConcept C84786313 @default.
• W2026020959 hasConceptScore W2026020959C111368507 @default.
• W2026020959 hasConceptScore W2026020959C119477230 @default.
• W2026020959 hasConceptScore W2026020959C127313418 @default.
• W2026020959 hasConceptScore W2026020959C13280743 @default.
• W2026020959 hasConceptScore W2026020959C139719470 @default.
• W2026020959 hasConceptScore W2026020959C14279187 @default.

• next