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Effect of pressure on 3D distribution of P-wave velocity and attenuation in antigorite serpentinite

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F17%3A00475899" target="_blank" >RIV/67985530:_____/17:00475899 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985831:_____/17:00475899

  • Result on the web

    <a href="http://dx.doi.org/10.1190/GEO2017-0006.1" target="_blank" >http://dx.doi.org/10.1190/GEO2017-0006.1</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1190/GEO2017-0006.1" target="_blank" >10.1190/GEO2017-0006.1</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Effect of pressure on 3D distribution of P-wave velocity and attenuation in antigorite serpentinite

  • Original language description

    We have developed a detailed study on the pressure dependence of P-wave velocities and amplitudes on a spherical sample of antigorite serpentinite from Val Malenco, Northern Italy. Measurements were done at room temperature and hydrostatic pressures up to 400 MPa in a pressure vessel with oil as a pressure medium. The transducer/sample assembly allows simultaneous velocity and amplitude measurements on the spherical sample in 132 independent directions.nThree significant directions of the foliated sample were selected to study changes of the directional dependence (anisotropy) of velocity, amplitude, and Q-factor with increasing pressure. Remarkable differences are observed between the changes of velocity and attenuation anisotropy as pressure is increased. Although the velocity anisotropy is quite stable through all pressure levels, the attenuation anisotropy and the Q-factor vary significantly in magnitude and orientation. The variations are probably caused by the closing of microcracks due to acting hydrostatic pressure, so the contact conditions between individual minerals consolidatenand the transmitting energy is less attenuating.

  • 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

    10505 - Geology

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

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

    Geophysics

  • ISSN

    0016-8033

  • e-ISSN

  • Volume of the periodical

    82

  • Issue of the periodical within the volume

    4

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    11

  • Pages from-to

    "WA33"-"WA43"

  • UT code for WoS article

    000408628900063

  • EID of the result in the Scopus database

    2-s2.0-85021686895