Multifractal analysis, the box counting technique and sliding window correl
ation dimension analysis are methods for the detection and description of n
onlinear variations in sedimentary time/depth series measurements such as w
ell-log data. Combinations of these methods allow the detection of sediment
ary discontinuities and fractal clustering of events such as bentonite laye
rs or fossils horizons in sedimentary sections. The methods are used to ana
lyze linear, periodic, fractal and random patterns with different sampling
intervals and after setting distinctive measurement thresholds. Application
of the methods iis illustrated by means of computer simulation models and
on the gamma-ray log from a Mid-Cretaceous sedimentary time series. (C) 199
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