@ARTICLE{Osuch_W._Evolution_2020,
 author={Osuch, W. and Błoniarz, R. and Michta, G. and Suliga, I.},
 volume={vol. 65},
 number={No 1},
 journal={Archives of Metallurgy and Materials},
 pages={485-492},
 howpublished={online},
 year={2020},
 publisher={Institute of Metallurgy and Materials Science of Polish Academy of Sciences},
 publisher={Committee of Materials Engineering and Metallurgy of Polish Academy of Sciences},
 abstract={The state of the dislocation substructure of meteorite in which the history of phenomena accompanying the meteorite during its passage through the Earth’s atmosphere is recorded remains unused. The main goal of the presented work is a comprehensive analysis of the dislocation structure of the iron meteorite from the Morasko reserve (Poland, Wielkopolska Voivodeship) by TEM methods to determine the conditions and mechanism of its formation. The work is cognitive in the field of phenomena related to the destruction and deformation of the material in extreme conditions: space and terrestrial space. It can also be useful in the research on the creation of the material with specific mechanical properties, as well as a unique reference material for earth experiments with low-temperature deformation, high-speed deformation, recrystallization processes with short thermal pulses and structure relaxation in conditions of very long time periods.},
 type={Article},
 title={Evolution of the Dislocation Structure of Iron Meteorite},
 URL={http://journals.pan.pl/Content/115082/PDF/AMM-2020-1-58-Bloniarz.pdf},
 doi={10.24425/amm.2020.131751},
 keywords={iron meteorite, Morasko, TEM study, dislocation structure, Neumann’s bands},
}