Skip navigation
Skip navigation

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

Heslop, David; Roberts, Andrew; Chang, Liao

Description

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 studies have shown that magnetofossils are widespread in the geological record and that they carry useful environmental information and contribute to paleomagnetic recording, which makes it essential to quantify...[Show more]

CollectionsANU Research Publications
Date published: 2014
Type: Journal article
URI: http://hdl.handle.net/1885/74323
Source: Geochemistry, Geophysics, Geosystems. G3
DOI: 10.1002/2014GC005291

Download

File Description SizeFormat Image
01_Heslop_Characterizing_magnetofossils_2014.pdf5.79 MBAdobe PDF


Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.

Updated:  20 July 2017/ Responsible Officer:  University Librarian/ Page Contact:  Library Systems & Web Coordinator