Abstract

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.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.