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Using neutron diffraction under pressure at room temperature, we observed that pyrrhotite undergoes a ferrimagnetic to paramagnetic transition at about 2.8 GPa. Complete demagnetization of remanence at the same pressure is confirmed in an independent
Externí odkaz:
http://hdl.handle.net/10150/623401
http://arizona.openrepository.com/arizona/handle/10150/623401
http://arizona.openrepository.com/arizona/handle/10150/623401
Publikováno v:
In Journal of Magnetism and Magnetic Materials 1 February 2015 375:234-241
Publikováno v:
In Journal of Magnetism and Magnetic Materials 1 January 2015 373:188-194
Publikováno v:
In Journal of Physics and Chemistry of Solids October 2013 74(10):1414-1418
Publikováno v:
In Physics Procedia November 2009 2(3):665-671
Publikováno v:
In Journal of Alloys and Compounds 2009 482(1):86-89
Autor:
Joumard, I. a, Klein, T. a, *, Samuely, P. b, Szabo, P. b, Jansen, A.G.M. c, Fillion, G. d, Rakoto, H. e, Broto, J.M. e, Marcus, J. a
Publikováno v:
In Physica C: Superconductivity and its applications 1999 317:436-440
Publikováno v:
Journal of Applied Physics; 5/1/1986, Vol. 59 Issue 9, p3208, 16p, 1 Chart, 20 Graphs
Publikováno v:
Journal of Applied Physics; Mar1980, Vol. 51 Issue 3, p1692-1701, 10p
Publikováno v:
The IRM Quarterly, 21(1), 1, 7
Use of low temperature (LT) magnetic transitions to identify magnetic minerals that carry a remanence – either natural or laboratory-induced – at room temperature, is a classic tool in rock magnetism (e.g. Nagata et al., 1964; Kosterov, 2007). Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::5610538a8164a0a17ace0629ca6d872d
https://dspace.library.uu.nl/handle/1874/206792
https://dspace.library.uu.nl/handle/1874/206792