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Assessing the effectiveness of the shear-tensile-compressive model in earthquake source inversions: synthetic experiments and field application

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F24%3A00583510" target="_blank" >RIV/67985530:_____/24:00583510 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985831:_____/24:00579689

  • Result on the web

    <a href="https://academic.oup.com/gji/article/236/1/161/7333972?login=true" target="_blank" >https://academic.oup.com/gji/article/236/1/161/7333972?login=true</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1093/gji/ggad425" target="_blank" >10.1093/gji/ggad425</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Assessing the effectiveness of the shear-tensile-compressive model in earthquake source inversions: synthetic experiments and field application

  • Original language description

    As an alternative to the moment tensor (MT) model for earthquake sources, the shear-tensile- compressi ve (STC) model of fers a kinematic description of the source mechanism and leads to a more robust inversion problem. However, the premise of the source inversion based on STC is to ensure the accuracy of parameternκdefined as the ratio of the Lam ´e constants, κ= λ/μ, in a fault zone. In this study, we carry out a series of synthetic experiments using P -wave amplitudes in source mechanism inversions based on both the STC and MT models, and consider the influence of noise, the uncertainties in source locations and in the velocity model. We show that the nonlinear STC inversion with an appropriate value of κleads to more accurate result compared to the linear MT inversion. We also propose a new joint-STC inversion method to jointly invert for parameter κand the remaining parameters of the STC model (magnitude and the strik e, dip, rak e and slope angles). The results indicate that our proposed method yields robust results for both the parameter κand focal mechanisms. We apply our joint-STC inversion method to field microearthquake data observed in the West Bohemia region to validate some of the conclusions drawn from the synthetic experiments.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10507 - Volcanology

Result continuities

  • Project

    <a href="/en/project/GA22-10747S" target="_blank" >GA22-10747S: Inversion of focal mechanisms and seismic moment tensors for stress and its spatiotemporal variation</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Geophysical Journal International

  • ISSN

    0956-540X

  • e-ISSN

    1365-246X

  • Volume of the periodical

    236

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    13

  • Pages from-to

    161-173

  • UT code for WoS article

    001098988900002

  • EID of the result in the Scopus database

    2-s2.0-85177767882