Abstract
THE banded character of many of the X-ray ‘lines' from such clay minerals as montmorillonite and halloysite has been attributed to their structures being equivalent to a random stacking of two-dimensional silicate sheets1. The relevant theory has been developed by Warren2, who introduced simplifying assumptions in order to obtain explicit expressions for the intensity distribution. We have sought a more general expression than Warren gives, and have avoided certain of his approximations by expressing the results in a form requiring numerical integration.
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