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The peak frequency of direct waves for microseismic events

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F13%3A00421143" target="_blank" >RIV/67985891:_____/13:00421143 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1190/GEO2013-0197.1" target="_blank" >http://dx.doi.org/10.1190/GEO2013-0197.1</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1190/GEO2013-0197.1" target="_blank" >10.1190/GEO2013-0197.1</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    The peak frequency of direct waves for microseismic events

  • Original language description

    Direct seismic waves (P- or S-waves) are used to locate and further characterize microseismic events. The resolution of information obtained from direct waves depends on the peak frequencies of the waveforms. The peak frequency results from combination of the source, propagation, and the receiver effects. For frequencies below the corner frequency, propagation effects control the peak frequency in observed seismograms of microseismic events. The frequency dependence of direct body waves can be modeled by attenuation, specifically the global attenuation factor. This model is consistent with observed data along surface profiles explaining the difference between the peak frequencies of P- and S-waves. In addition, the model is consistent with the peak frequencies observed on downhole monitoring arrays. This can be used to invert effective attenuation providing additional unique measurement from microseismic events. The corner frequency can be estimated from the average stress drop and ana

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DC - Seismology, volcanology and Earth structure

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GAP210%2F12%2F2451" target="_blank" >GAP210/12/2451: Seismicity driven by fluids injection</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2013

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Geophysics

  • ISSN

    0016-8033

  • e-ISSN

  • Volume of the periodical

    78

  • Issue of the periodical within the volume

    6

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    5

  • Pages from-to

    "A45"-"A49"

  • UT code for WoS article

    000330223800001

  • EID of the result in the Scopus database