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000827059 1001_ $$0P:(DE-HGF)0$$aAlmeida, T. P.$$b0$$eCorresponding author
000827059 245__ $$aDirect observation of the thermal demagnetization of a vortex structure held by a non-ideal magnetite recorder
000827059 260__ $$aHoboken, NJ$$bWiley$$c2016
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000827059 520__ $$aThe thermal demagnetization of pseudo-single-domain (PSD) magnetite (Fe3O4) particles, which govern the magnetic signal in many igneous rocks, is examined using off-axis electron holography. Visualization of a vortex structure held by an individual Fe3O4 particle (~250 nm in diameter) during in situ heating is achieved through the construction and examination of magnetic-induction maps. Stepwise demagnetization of the remanence-induced Fe3O4 particle upon heating to above the Curie temperature, performed in a similar fashion to bulk thermal demagnetization measurements, revealed that its vortex state remains stable under heating close to its unblocking temperature and is recovered upon cooling with the same or reversed vorticity. Hence, the PSD Fe3O4 particle exhibits thermomagnetic behavior comparable to a single-domain carrier, and thus, vortex states are considered reliable magnetic recorders for paleomagnetic investigations
000827059 536__ $$0G:(DE-HGF)POF3-143$$a143 - Controlling Configuration-Based Phenomena (POF3-143)$$cPOF3-143$$fPOF III$$x0
000827059 7001_ $$0P:(DE-HGF)0$$aMuxworthy, A. R.$$b1
000827059 7001_ $$0P:(DE-Juel1)144926$$aKovacs, Andras$$b2
000827059 7001_ $$0P:(DE-HGF)0$$aWilliams, W.$$b3
000827059 7001_ $$0P:(DE-HGF)0$$aNagy, L.$$b4
000827059 7001_ $$0P:(DE-HGF)0$$aConbhuí, P.Ò$$b5
000827059 7001_ $$0P:(DE-HGF)0$$aFrandsen, C.$$b6
000827059 7001_ $$0P:(DE-HGF)0$$aSupakulopas, R.$$b7
000827059 7001_ $$0P:(DE-Juel1)144121$$aDunin-Borkowski, Rafal$$b8
000827059 773__ $$0PERI:(DE-600)2021599-X$$a10.1002/2016GL070074$$n16$$p8426 - 8434$$tGeophysical research letters$$v43$$x0094-8276$$y2016
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