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@ARTICLE{Almeida:189411,
author = {Almeida, Trevor P. and Kasama, Takeshi and Muxworthy,
Adrian R. and Williams, Wyn and Nagy, Lesleis and
Dunin-Borkowski, Rafal},
title = {{O}bserving thermomagnetic stability of nonideal magnetite
particles: {G}ood paleomagnetic recorders?},
journal = {Geophysical research letters},
volume = {41},
number = {20},
issn = {0094-8276},
address = {Hoboken, NJ},
publisher = {Wiley},
reportid = {FZJ-2015-02578},
pages = {7041 - 7047},
year = {2014},
abstract = {The thermomagnetic behavior of remanence-induced magnetite
(Fe3O4) particles in the pseudo-single-domain (PSD) size
range (~0.1–10 µm), which dominate the magnetic
signature of many rock lithologies, is investigated using
off-axis electron holography. Construction of magnetic
induction maps allowed for the visualization of the vortex
domain state in an individual Fe3O4 grain (~200 nm in
diameter) as a function of temperature. Acquisition of a
series of electron holograms at 100°C intervals during in
situ heating up to 700°C demonstrates the vortex state of
the Fe3O4 grain, in this instance, remains thermally stable
close to its unblocking temperature and exhibits a similar
in-plane remanent state upon cooling; i.e., the particle is
effectively behaving like a uniaxial single-domain particle
to temperatures near TC. Such particles are thought to be
robust magnetic recorders. It is suggested that evidence for
PSD behavior should therefore not preclude paleomagnetic
investigation},
cin = {PGI-5},
ddc = {550},
cid = {I:(DE-Juel1)PGI-5-20110106},
pnm = {42G - Peter Grünberg-Centre (PG-C) (POF2-42G41)},
pid = {G:(DE-HGF)POF2-42G41},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000345343100008},
doi = {10.1002/2014GL061432},
url = {https://juser.fz-juelich.de/record/189411},
}