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Measurement of the left-lateral displacement of ms 8.1 Kunlun earthquake on 14 November 2001 using Landsat-7 ETM+ imagery / J.G. Liu in International Journal of Remote Sensing IJRS, vol 27 n°9-10 (May 2006)  

Public [article]  inInternational Journal of Remote Sensing IJRS > vol 27 n°9-10 (May 2006) . - pp 1875 - 1891 Titre : Measurement of the left-lateral displacement of ms 8.1 Kunlun earthquake on 14 November 2001 using Landsat-7 ETM+ imagery Type de document : Article/Communication Auteurs : J.G. Liu, Auteur ; P.J. Mason, Auteur ; J. Ma, Auteur Année de publication : 2006 Article en page(s) : pp 1875 - 1891 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de télédétection [Termes IGN] analyse diachronique [Termes IGN] analyse infrapixellaire [Termes IGN] appariement d'images [Termes IGN] corrélation croisée normalisée [Termes IGN] déformation de la croute terrestre [Termes IGN] faille géologique [Termes IGN] géoréférencement direct [Termes IGN] image Landsat-ETM+ [Termes IGN] mesurage de distances [Termes IGN] mouvement de terrain [Termes IGN] séisme Résumé : (Auteur) An geodesy study bas been carried out, using pre- and post-event Landsat-7 Enhanced Thematic Mapper Plus (ETM +) images, to reveal regional co-seismic displacement caused by the Ms 8.1 Kunlun earthquake in November 2001. The two Landsat scenes, Kusai Lake and Buka Daban, cover an area of some 57600km (320km W-E and about 180km N-S), which includes most of the fault rupture zone. The co-seismic displacement measured in the Kusai Lake scene shows that the average left-lateral shift along the Kunlun fault is 4.8m (ranging from 1.5 to 8.1 m) and the maximum shift appears west of the Kusai Lake. The splayed nature of the fault to the west of Buka Daban, where the fault splits into three branches, causes the displacement pattern to become complicated. Here the average left-lateral shift, between the south side of the southern branch and the north side of the northern branch, is 4.6m (ranging from 1.0 to 8.2m). Our results also illustrate that the south side of the fault is the 'active' block, moving significantly in an east-south-easterly direction, relative to the largely 'stable' northern block. Numéro de notice : A2006-223 Affiliation des auteurs : non IGN Thématique : IMAGERIE Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1080/01431160500292023 En ligne : https://doi.org/10.1080/01431160500292023 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=27950 [article]

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