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Characterizing magnetofossils from first‐order reversal curve (FORC) central ridge signatures

D Heslop, AP Roberts, L Chang - Geochemistry, Geophysics …, 2014 - Wiley Online Library
The central ridge structure of a first‐order reversal curve (FORC) distribution is indicative of
uniaxial noninteracting single domain magnetic particles, which provides the opportunity to …
被引用次数：58 相关文章

Characterizing magnetofossils from first-order reversal curve (FORC) central ridge signatures

D Heslop, AP Roberts, L Chang - Geochemistry Geophysics …, 2014 - archimer.ifremer.fr
The central ridge structure of a first-order reversal curve (FORC) distribution is indicative of
uni-axial noninteracting single domain magnetic particles, which provides the opportunity to …
[PDF] core.ac.uk

[PDF][PDF] Characterizing magnetofossils from first-order reversal curve (FORC) central ridge signatures

D Heslop, AP Roberts, L Chang - Geochem. Geophys. Geosyst, 2014 - core.ac.uk
The central ridge structure of a first-order reversal curve (FORC) distribution is indicative of
uniaxial noninteracting single domain magnetic particles, which provides the opportunity to …

Characterizing magnetofossils from first-order reversal curve (FORC) central ridge signatures

D Heslop, AP Roberts, L Chang - Geochemistry, Geophysics …, 2014 - ui.adsabs.harvard.edu
The central ridge structure of a first-order reversal curve (FORC) distribution is indicative of
uniaxial noninteracting single domain magnetic particles, which provides the opportunity to …

[引用][C] Characterizing magnetofossils from first-order reversal curve (FORC) central ridge signatures

D Heslop, AP Roberts, L Chang - Geochemistry, Geophysics …, 2014 - cir.nii.ac.jp
Characterizing magnetofossils from first-order reversal curve (FORC) central ridge signatures |
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