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
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10302 - Condensed matter physics (including formerly solid state physics, supercond.)
Result continuities
Project
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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