Počet záznamů: 1  

Spatially varying crustal stress along the Zagros seismic belt inferred from earthquake focal mechanisms

  1. 1.
    SYSNO ASEP0567607
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevSpatially varying crustal stress along the Zagros seismic belt inferred from earthquake focal mechanisms
    Tvůrce(i) Nouri, A. (IR)
    Rahimi, B. (IR)
    Vavryčuk, Václav (GLU-S)
    Ghaemi, F. (IR)
    Číslo článku229653
    Zdroj.dok.Tectonophysics. - : Elsevier - ISSN 0040-1951
    Roč. 846, January (2023)
    Poč.str.9 s.
    Forma vydáníTištěná - P
    Jazyk dok.eng - angličtina
    Země vyd.NL - Nizozemsko
    Klíč. slovaZagros ; Tectonic stress ; Stress inversion ; Earthquake ; Focal mechanism
    Obor OECDEnvironmental and geological engineering, geotechnics
    Způsob publikováníOmezený přístup
    Institucionální podporaGLU-S - RVO:67985831
    UT WOS000909810100001
    EID SCOPUS85144443252
    DOI10.1016/j.tecto.2022.229653
    AnotaceWe determine the stress field of the Zagros fold-and-thrust belt (ZFTB) in the collisional zone between the Arabian and Iranian plates. Using 898 mainshock focal mechanisms, which occurred along the belt between 1956 and 2021, we calculate stress at 32 locations. The results reveal that the crustal stress in the Zagros belt is heterogeneous with variations in the orientation of SHmax as well as in the stress ratio. The interpolation of the Simpson’s index Aϕ points to three distinct domains: northern, central and southern, which are characterized by wrench, compressional, and wrench-compressional to compressional tectonic regimes, respectively. Tectonic stress in the study area is characterized by a horizontal to sub-horizontal maximum compression axis in the ~NESW to ~NNW-SSE direction. The GPS measurements of the strain tensor and the SHmax direction inferred from the stress inversion indicate that both the deformation pattern and the seismicity along the ZFTB zone are primarily affected by convergence of the Arabian and Iranian plates.
    PracovištěGeologický ústav
    KontaktJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Rok sběru2024
    Elektronická adresahttps://www.sciencedirect.com/science/article/pii/S0040195122004474
Počet záznamů: 1  

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