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...

Descripció completa

Dades bibliogràfiques

Autors principals:	David Heslop, Andrew P. Roberts, Liao Chang
Format:	Artigo
Idioma:	Inglês
Publicat:	Wiley 2014-06-01
Col·lecció:	Geochemistry, Geophysics, Geosystems
Matèries:	First‐order reversal curves magnetofossils sedimentary magnetism
Accés en línia:	https://doi.org/10.1002/2014GC005291
Etiquetes:	Afegir etiqueta Sense etiquetes, Sigues el primer a etiquetar aquest registre!