Seismicity in far western Nepal reveals flats and ramps along the Main Himalayan Thrust
Autor: | Magali Riesner, Chintan Timsina, M. Laporte, Bharat Prasad Koirala, C Duverger, T. Kandel, Mukunda Bhattarai, Hélène Lyon-Caen, Laurent Bollinger, L. B. Adhikari, R. Hoste-Colomer, Jean Letort |
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Přispěvatelé: | Laboratoire de géologie de l'ENS (LGENS), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Laboratoire de Détection et de Géophysique (CEA) (LDG), DAM Île-de-France (DAM/DIF), Direction des Applications Militaires (DAM), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Direction des Applications Militaires (DAM), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Bureau de Recherches Géologiques et Minières (BRGM) (BRGM), Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France, Department of Mines and Geology, Lainchaur, Kathmandu |
Jazyk: | angličtina |
Rok vydání: | 2021 |
Předmět: |
geography
geography.geographical_feature_category 010504 meteorology & atmospheric sciences Front (oceanography) [SDU.STU]Sciences of the Universe [physics]/Earth Sciences Thrust Induced seismicity Fault (geology) 010502 geochemistry & geophysics 01 natural sciences Tectonics Geophysics 13. Climate action Geochemistry and Petrology Regional studies Period (geology) Seismic cycle Seismology Geology 0105 earth and related environmental sciences |
Zdroj: | Geophysical Journal International Geophysical Journal International, Oxford University Press (OUP), 2021, 226 (3), pp.1747-1763. ⟨10.1093/gji/ggab159⟩ Geophysical Journal International, 2021, 226 (3), pp.1747-1763. ⟨10.1093/gji/ggab159⟩ |
ISSN: | 0956-540X 1365-246X |
Popis: | SUMMARYUnravelling relations between lateral variations of mid-crustal seismicity and the geometry of the Main Himalayan Thrust (MHT) system at depth is a key issue in seismotectonic studies of the Himalayan range. These relations can reveal along strike changes in the behaviour of the fault at depth related to fluids or the local ramp-flat geometry and more generally of the stress build-up along the fault. Some of these variations may control the rupture extension of intermediate, large or great earthquakes, the last of which dates back from 1505 CE in far western Nepal. The region is also associated to lateral spatio-temporal variations of the mid-crustal seismicity monitored by the Regional Seismic Network of Surkhet–Birendranagar. This network was supplemented between 2014 and 2016 by 15 temporary stations deployed above the main seismic clusters giving new potential to regional studies. Both absolute and relative locations together with focal mechanisms are determined to gain insight on the fault behaviour at depth. We find more than 4000 earthquakes within 5 and 20 km-depth clustered in three belts parallel to the front of the Himalayan range. Finest locations reveal close relationships between seismic clusters and fault segments at depth among which mid-crustal ramps and reactivated tectonic slivers. Our results support a geometry of the MHT involving several fault patches at depth separated by ramps and tear faults. This geometry most probably affects the pattern of the coseismic ruptures breaking partially or totally the locked fault zone as well as eventual along strike variations of seismic coupling during interseismic period. |
Databáze: | OpenAIRE |
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