“…Over the past 15 years, a number of papers have described the distribution and abundance of clay minerals within major ocean basins (Biscaye, 1965;Gorbunova, 1963;Griffin and Goldberg, 1963;KoUa et al, 1976;Venkatarathnam and Biscaye, 1973;YeroshchevShak, 1962) and even the world ocean (Griffin et al, 1968;Rateev et al, 1969). In all cases, however, the abundance values were derived from the assumptions that peak-area ratios from X-ray powder diffractograms are related to the corresponding weight ratios of clay minerals by known simple factors (Biscaye, 1965;modified from Johns et al, 1954), and that clay minerals constitute 100% of the fine fraction of deep-sea sediments.…”