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| 001 | 189411 | ||
| 005 | 20240610121205.0 | ||
| 024 | 7 | _ | |a 10.1002/2014GL061432 |2 doi |
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| 037 | _ | _ | |a FZJ-2015-02578 |
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| 100 | 1 | _ | |a Almeida, Trevor P. |0 P:(DE-HGF)0 |b 0 |e Corresponding Author |
| 245 | _ | _ | |a Observing thermomagnetic stability of nonideal magnetite particles: Good paleomagnetic recorders? |
| 260 | _ | _ | |a Hoboken, NJ |c 2014 |b Wiley |
| 336 | 7 | _ | |a article |2 DRIVER |
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| 336 | 7 | _ | |a Journal Article |b journal |m journal |0 PUB:(DE-HGF)16 |s 1429019280_26837 |2 PUB:(DE-HGF) |
| 336 | 7 | _ | |a ARTICLE |2 BibTeX |
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| 336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
| 520 | _ | _ | |a 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 |
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| 700 | 1 | _ | |a Kasama, Takeshi |0 P:(DE-HGF)0 |b 1 |
| 700 | 1 | _ | |a Muxworthy, Adrian R. |0 P:(DE-HGF)0 |b 2 |
| 700 | 1 | _ | |a Williams, Wyn |0 P:(DE-HGF)0 |b 3 |
| 700 | 1 | _ | |a Nagy, Lesleis |0 P:(DE-HGF)0 |b 4 |
| 700 | 1 | _ | |a Dunin-Borkowski, Rafal |0 P:(DE-Juel1)144121 |b 5 |u fzj |
| 773 | _ | _ | |a 10.1002/2014GL061432 |g Vol. 41, no. 20, p. 7041 - 7047 |0 PERI:(DE-600)2021599-X |n 20 |p 7041 - 7047 |t Geophysical research letters |v 41 |y 2014 |x 0094-8276 |
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