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Orogenic collapse and stress adjustments revealed by an intense seismic swarm following the 2015 Gorkha earthquake in Nepal / Lok Bijaya Adhikari in Frontiers in Earth Science, vol 9 (2021)
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Titre : Orogenic collapse and stress adjustments revealed by an intense seismic swarm following the 2015 Gorkha earthquake in Nepal Type de document : Article/Communication Auteurs : Lok Bijaya Adhikari, Auteur ; Laurent Bollinger, Auteur ; Jérôme Vergne, Auteur ; Sophie Lambotte, Auteur ; Kristel Chanard , Auteur ; Marine Laporte, Auteur ; Lily Li, Auteur ; Bharat Koirala, Auteur ; Mukunda Bhattarai, Auteur ; Chintan Timsina, Auteur ; Nabina Bishwokarma, Auteur ; Nicolas Wendling-Vazquez, Auteur ; Frédéric Girault, Auteur ; Frédéric Perrier, Auteur
Année de publication : 2021 Projets : 1-Pas de projet / Article en page(s) : n° 659937 Note générale : bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Géophysique interne
[Termes IGN] effondrement de terrain
[Termes IGN] Himalaya
[Termes IGN] Népal
[Termes IGN] séisme
[Termes IGN] variation saisonnièreRésumé : (auteur) The April 25, 2015 Mw 7.9 Gorkha earthquake in Nepal was characterized by a peak slip of several meters and persisting aftershocks. We report here that, in addition, a dense seismic swarm initiated abruptly in August 2017 at the western edge of the afterslip region, below the high Himalchuli-Manaslu range culminating at 8156 m, a region seismically inactive during the past 35 years. Over 6500 events were recorded by the Nepal National Seismological Network with local magnitude ranging between 1.8 and 3.7 until November 2017. This swarm was reactivated between April and July 2018, with about 10 times less events than in 2017, and in 2019 with only sporadic events. The relocation of swarm earthquakes using proximal temporary stations ascertains a shallow depth of hypocenters between the surface and 20 km depth in the High Himalayan Crystalline slab. This swarm reveals an intriguing localized interplay between orogenic collapse and stress adjustments, involving possibly CO2-rich fluid migration, more likely post-seismic slip and seasonal enhancements. Numéro de notice : A2021-788 Affiliation des auteurs : UMR IPGP-Géod+Ext (2020- ) Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.3389/feart.2021.659937 Date de publication en ligne : 22/07/2021 En ligne : https://doi.org/10.3389/feart.2021.659937 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=98985
in Frontiers in Earth Science > vol 9 (2021) . - n° 659937[article]