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Bayesian inference and interpretation of centroid moment tensors of the 2016 Kumamoto earthquake sequence, Kyushu, Japan

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F17%3A10366885" target="_blank" >RIV/00216208:11320/17:10366885 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1186/s40623-017-0721-4" target="_blank" >http://dx.doi.org/10.1186/s40623-017-0721-4</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1186/s40623-017-0721-4" target="_blank" >10.1186/s40623-017-0721-4</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Bayesian inference and interpretation of centroid moment tensors of the 2016 Kumamoto earthquake sequence, Kyushu, Japan

  • Original language description

    On April 16, 2016, Kumamoto prefecture in Kyushu region, Japan, was devastated by a shallow MJMA7.3 earthquake. The series of foreshocks started by MJMA6.5 foreshock 28 h before the mainshock. They have originated in Hinagu fault zone intersecting the mainshock Futagawa fault zone; hence, the tectonic background for this earthquake sequence is rather complex. Here we infer centroid moment tensors (CMTs) for 11 events with MJMA between 4.8 and 6.5, using strong motion records of the K-NET, KiK-net and F-net networks. We use upgraded Bayesian full-waveform inversion code ISOLA-ObsPy, which takes into account uncertainty of the velocity model. Such an approach allows us to reliably assess uncertainty of the CMT parameters including the centroid position. The solutions show significant systematic spatial and temporal variations throughout the sequence. Foreshocks are right-lateral steeply dipping strike-slip events connected to the NE-SW shear zone. Those located close to the intersection of the Hinagu and Futagawa fault zones are dipping slightly to ESE, while those in the southern area are dipping to WNW. Contrarily, aftershocks are mostly normal dip-slip events, being related to the N-S extensional tectonic regime. Most of the deviatoric moment tensors contain only minor CLVD component, which can be attributed to the velocity model uncertainty. Nevertheless, two of the CMTs involve a significant CLVD component, which may reflect complex rupture process. Decomposition of those moment tensors into two pure shear moment tensors suggests combined right-lateral strike-slip and normal dip-slip mechanisms, consistent with the tectonic settings of the intersection of the Hinagu and Futagawa fault zones.

  • 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

    10500 - Earth and related environmental sciences

Result continuities

  • Project

  • Continuities

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    EARTH PLANETS AND SPACE

  • ISSN

    1880-5981

  • e-ISSN

  • Volume of the periodical

    69

  • Issue of the periodical within the volume

    September

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    19

  • Pages from-to

  • UT code for WoS article

    000411750200001

  • EID of the result in the Scopus database