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

Abstract 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 identify and characterize biogenic magnetic mineral remains (magnetofossils) in sediments. Recent stud...

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Hlavní autoři:	David Heslop, Andrew P. Roberts, Liao Chang
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2014-06-01
Edice:	Geochemistry, Geophysics, Geosystems
Témata:	First‐order reversal curves magnetofossils sedimentary magnetism
On-line přístup:	https://doi.org/10.1002/2014GC005291
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