Physics
Scientific paper
Oct 1997
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997jmmm..174..321c&link_type=abstract
Journal of Magnetism and Magnetic Materials, Volume 174, Issue 3, p. 321-323.
Physics
Elsevier: Taenite, Antitaenite, Meteorites, Ultrafine Particles, Mössbauer Spectroscopy
Scientific paper
The author responds to suggestions that a low-spin iron-nickel phase noticed in the Mössbauer spectra of meteorites should be classified as a new mineral called antitaenite. Experimental results do not unambiguously confirm the proposed characteristics of the phase. Reference to the literature reveals that, contrary to an early assumption, the phase is consistent with ferromagnetic and paramagnetic order. Its resistance to the martensitic transformation, claimed to be an intrinsic characteristic, is likely to be caused by contact with tetrataenite. Furthermore, the low-spin phase in meteorites does not appear to be a distinct mineral because it has only been observed as an intergrowth with tetrataenite.
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