% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Kasama:201629,
      author       = {Kasama, Takeshi and Harrison, Richard J. and Church, Nathan
                      S. and Nagao, Masahiro and Feinberg, Joshua M. and
                      Dunin-Borkowski, Rafal},
      title        = {{F}errimagnetic/ferroelastic domain interactions in
                      magnetite below the {V}erwey transition. {P}art {I}:
                      electron holography and {L}orentz microscopy},
      journal      = {Phase transitions},
      volume       = {86},
      number       = {1},
      issn         = {1029-0338},
      address      = {London [u.a.]},
      publisher    = {Taylor $\&$ Francis},
      reportid     = {FZJ-2015-03923},
      pages        = {67 - 87},
      year         = {2013},
      abstract     = {The crystallographic and magnetic microstructure of
                      magnetite (Fe3O4) below the Verwey transition (∼120 K)
                      is studied using transmission electron microscopy. The low
                      temperature phase is found to have a monoclinic C-centered
                      lattice with a c-glide plane perpendicular to the b-axis,
                      which allows twin-related crystal orientations to be
                      distinguished. Off-axis electron holography and Lorentz
                      electron microscopy are used to show that magnetic domains
                      present at room temperature become subdivided into
                      sub-micron-sized magnetic domains below the Verwey
                      transition, with the magnetization direction in each
                      magnetic domain oriented along the monoclinic [001] axis.
                      The nature of the interactions between the magnetic domain
                      walls and the ferroelastic twin walls is investigated.
                      Cooling and warming cycles through the transition
                      temperature are used to show that a memory effect is likely
                      to exist between the magnetic states that form above and
                      below the transition. Our results suggest that ferroelastic
                      twin walls have a strong influence on the low temperature
                      magnetic properties of magnetite.},
      cin          = {PGI-5},
      ddc          = {540},
      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:000312586700007},
      doi          = {10.1080/01411594.2012.695373},
      url          = {https://juser.fz-juelich.de/record/201629},
}