Study of iron‐bearing phases in ordinary and carbonaceous chondrites as well as iron meteorite and extracted iron‐nickel phosphides by Mössbauer spectroscopy with improved velocity resolution (measurement in 4096 channels, presentation in 1024 channels) demonstrated new results which were not obtained from Mössbauer spectra measured in 512 channels or less. Fitting of the iron meteorite Mössbauer spectrum measured for the first time with presentation in 4096 channels showed new details probably related to the complicated phase composition.

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