Fabric shape is often quantified using the three eigenvalues from the
'orientation tensor' method applied to a sample of directions. Several
studies have used eigenvalues plotted on fabric shape diagrams to dis
tinguish sedimentary facies or strain histories. However, such studies
seldom consider how well the sample eigenvalues represent the true fa
bric shape. In this paper, we use 'bootstrapping' techniques to define
confidence regions for sample eigenvalues, and show that sample and p
opulation eigenvalues may differ substantially. Confidence regions are
often very large for small sample sizes, and we recommend that sample
sizes should be at least 50. (C) 1997 Elsevier Science Ltd.