The structure of a glauberite crystal from Imperial County, California has been determined and refined from three-dimensional diffractometer intensities obtained with a double-filter technique. The model refined by successive Fourier syntheses and least-squares techniques confirms that published by Cocco et al. (1965) at the time when this investigation was approaching completion. Anisotropic temperature factors and interatomic distances were calculated and a final R factor of 6.4% was obtained.

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