Direct observation of ferrimagnetic/ferroelastic domain interactions in magnetite below the Verwey transition
Publication: Research - peer-review › Journal article – Annual report year: 2010
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Direct observation of ferrimagnetic/ferroelastic domain interactions in magnetite below the Verwey transition. / Kasama, Takeshi; Church, Nathan S.; Feinberg, Joshua M.; Dunin-Borkowski, Rafal E.; Harrison, Richard J.
In: Earth and Planetary Science Letters, Vol. 297, No. 1-2, 2010, p. 10-17.Publication: Research - peer-review › Journal article – Annual report year: 2010
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TY - JOUR
T1 - Direct observation of ferrimagnetic/ferroelastic domain interactions in magnetite below the Verwey transition
A1 - Kasama,Takeshi
A1 - Church,Nathan S.
A1 - Feinberg,Joshua M.
A1 - Dunin-Borkowski,Rafal E.
A1 - Harrison,Richard J.
AU - Kasama,Takeshi
AU - Church,Nathan S.
AU - Feinberg,Joshua M.
AU - Dunin-Borkowski,Rafal E.
AU - Harrison,Richard J.
PB - Elsevier BV
PY - 2010
Y1 - 2010
N2 - The magnetic behaviour of magnetite at low temperatures is dominated by its transformation to a monoclinic crystal structure that is simultaneously ferrimagnetic, ferroelastic and ferroelectric below similar to 125 K (the Verwey transition). Here we use electron microscopy to reveal the relationship between ferrimagnetic and ferroelastic domain structures in monoclinic magnetite. We present dynamic observations of magnetite during heating and cooling across the Verwey transition, revealing a diversity of unexpected interaction phenomena between crystallographic twins and magnetic domain walls. This study provides a new understanding of the low-temperature magnetic properties of magnetite that will affect a broad range of rock magnetic studies, from the interpretation of magnetic remanence in terrestrial rocks and sediments to the search for biogenic magnetite in extraterrestrial materials.
AB - The magnetic behaviour of magnetite at low temperatures is dominated by its transformation to a monoclinic crystal structure that is simultaneously ferrimagnetic, ferroelastic and ferroelectric below similar to 125 K (the Verwey transition). Here we use electron microscopy to reveal the relationship between ferrimagnetic and ferroelastic domain structures in monoclinic magnetite. We present dynamic observations of magnetite during heating and cooling across the Verwey transition, revealing a diversity of unexpected interaction phenomena between crystallographic twins and magnetic domain walls. This study provides a new understanding of the low-temperature magnetic properties of magnetite that will affect a broad range of rock magnetic studies, from the interpretation of magnetic remanence in terrestrial rocks and sediments to the search for biogenic magnetite in extraterrestrial materials.
KW - TEM
KW - Verwey transition
KW - electron holography
KW - twins
KW - domain walls
KW - magnetite
U2 - 10.1016/j.epsl.2010.05.004
DO - 10.1016/j.epsl.2010.05.004
JO - Earth and Planetary Science Letters
JF - Earth and Planetary Science Letters
SN - 0012-821X
IS - 1-2
VL - 297
SP - 10
EP - 17
ER -