The effects of dislocations on crystallographic twins and domain wall motion in magnetite at the Verwey transition.

The Institute for Rock Magnetism and LacCore are supported by the NSF EAR Instrumentation and Facilities Program and by the University of Minnesota, Earth Sciences Division, National Science Foundation. This work was funded by EAR-0810085 to JMF, by EAR-0810252 to AJN, and by a Geological Society of America grant to AKL. The research leading to these results has received funding from the European Research Council under the European Union’s Seventh Framework Programme (FP/2007-2013) / ERC Grant Agreement No. 320750. JCL was funded by the Royal Society, UK.