Abstract
Comparative study of schreibersite and rhabdite extracted from Sikhote–Alin (IIAB) iron meteorite using Mossbauer spectroscopy, X-ray diffraction and magnetic measurements was carried out. Mossbauer spectra of bulk meteorite sample and extracted phosphides were recorded in 4,096 channels and then presented in 1,024 channels. Differences of the unit cell structure, the Fe, Ni and Co content, the room temperature Mossbauer spectra and Curie temperature for rhabdite and schreibersite were found.
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