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Journal Article | FZJ-2016-01480 |
; ; ; ;
2015
IOP Publ.
Bristol
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Please use a persistent id in citations: http://hdl.handle.net/2128/9831 doi:10.1088/1742-6596/644/1/012027
Abstract: The production of a synthetic basalt comprising Fe3O4 grains (~ 50 nm to ~ 500 nm), via a glass ceramic method, has been confirmed using transmission electron microscopy and X-ray diffractometry. Off-axis electron holography combined with in situ heating allowed for the visualisation of non-uniform vortex states present in saturation remanent structures, and their variation approaching the Curie temperature; determined separately by bulk thermomagnetic measurements.
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