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The AAPG/Datapages Combined Publications Database

Journal of Sedimentary Research (SEPM)

Abstract


Journal of Sedimentary Petrology
Vol. 49 (1979)No. 1. (March), Pages 273-280

Empirical Conversion Equations for Thin-Section and Sieve Derived Size Distribution Parameters

J. A. Harrell, K. A. Eriksson

ABSTRACT

Using size analyses of ancient sandstones, thin-section-to-sieve and sieve-to-thin-section empirical conversion equations have been derived, via linear regression analysis, for several graphical size distribution statistics: median, graphic mean, inclusive graphic Previous HitstandardNext Hit Previous HitdeviationNext Hit, graphic Previous HitstandardNext Hit Previous HitdeviationTop, inclusive graphic skewness, graphic skewness, and graphic kurtosis. The correlation coefficients for each of these are respectively .958, .944, .705, .786, .567, .234, and .316. Conversions of high accuracy are possible only for the median and graphic mean. The thin-section-to-sieve conversion equations for these two parameters are,

median: Y(sieve)= .121 4 + 1.030 · X(thin-section)

mean: Y(sieve) = .227 + .973 · X(thin-section)

Thin-section-to-sieve empirical conversion equations, of generally high accuracy, have also been derived for the following cumulative percentiles: 2, 5, 9, 16, 25, 36, 50, 64, 75, 84, 91, 95, and 98. These may be used in the conversion of whole distributions.


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