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Inverting for the focal mechanisms of small and microearthquakes using initial P-wave amplitudes

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F25%3A00635665" target="_blank" >RIV/67985530:_____/25:00635665 - isvavai.cz</a>

  • Result on the web

    <a href="http://www.geophy.cn//article/doi/10.6038/cjg2024S0147" target="_blank" >http://www.geophy.cn//article/doi/10.6038/cjg2024S0147</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.6038/cjg2024S0147" target="_blank" >10.6038/cjg2024S0147</a>

Alternative languages

  • Result language

    čínština

  • Original language name

    利用 P 波初动振幅反演小微地震的震源机制

  • Original language description

    摘要 获取准确且数目众多的小微地震的震源机制对研究水力压裂所导致的地下应力场变化具有重要意义. 本研 究基于川南页岩气注采区域密集台阵地震监测数据,分别采用波形反演法和振幅反演法对 5 个中小地震 (5 > ML > 3) 进行震源机制求解,并将两种结果进行比较分析. 以波形反演得到的震源机制解作为参考,结合振幅正演合成理论 计算得到理论初至振幅,将理论初至振幅和用于振幅反演的观测初至振幅进行比较,提出基于震源机制解的振幅 校准系数, 再将校准系数应用于小微地震 (ML ≤ 3) 的振幅反演中,从而获得更加可靠的小微地震震源机制结果. 相 关结果及结论以期对小微地震的震源机制研究提供进一步指导,并为注采诱发地震灾害的防控工作奠定基础.n

  • 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

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION

  • ISSN

    0001-5733

  • e-ISSN

    0001-5733

  • Volume of the periodical

    68

  • Issue of the periodical within the volume

    5

  • Country of publishing house

    CN - CHINA

  • Number of pages

    18

  • Pages from-to

    1808-1825

  • UT code for WoS article

    001492740900006

  • EID of the result in the Scopus database

    2-s2.0-105006744813