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Strongly Negative Low-Field Variation of Magnetic Susceptibility: Rock Magnetic Character of the Basement-Cover Interface of Northeastern Oklahoma

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F24%3A00597996" target="_blank" >RIV/67985831:_____/24:00597996 - isvavai.cz</a>

  • Result on the web

    <a href="https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2023JB028606" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2023JB028606</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1029/2023JB028606" target="_blank" >10.1029/2023JB028606</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Strongly Negative Low-Field Variation of Magnetic Susceptibility: Rock Magnetic Character of the Basement-Cover Interface of Northeastern Oklahoma

  • Original language description

    Some rock and soil samples exhibit significant loss of magnetic susceptibility (χ) with increasing applied field amplitude even at relatively low (10–100s of A/m) fields, a behavior which remains unexplained. Exceptionally strong negative field-dependence of susceptibility (χHD) is present in sandstones and altered intermediate-felsic igneous rocks in several cores from the northeastern Oklahoma subsurface. These same rocks also show elevated frequency-dependence of susceptibility (χFD), with reasonable correlation of χHD to χFD, and frequency-dependent χHD. Results from multiple characterization methods indicate that strongly negative χHD in these rocks is linked to a yet-unidentified phase which begins the approach to magnetic saturation in low fields (<1 mT/800 A/m), shows elevated χFD to low temperatures, is unstable at high temperatures, possesses significant anisotropy of magnetic susceptibility, and becomes paramagnetic above ∼83°C. Clear associations with fluid alteration features indicate that this material may be highly relevant to rock alteration, diagenetic, and environmental studies.

  • 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

    10302 - Condensed matter physics (including formerly solid state physics, supercond.)

Result continuities

  • Project

  • 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

    Journal of Geophysical Research-Solid Earth

  • ISSN

    2169-9313

  • e-ISSN

    2169-9356

  • Volume of the periodical

    129

  • Issue of the periodical within the volume

    8

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    22

  • Pages from-to

    e2023JB028606

  • UT code for WoS article

    001285336900001

  • EID of the result in the Scopus database

    2-s2.0-85200689423