fold test The main test in palaeomagnetism for determining the age of the remanent magnetization of rocks. Comparison of the scatter of directions of natural remanence from both sides of a fold, before and after correcting for the tectonic effects of the folding, enable the magnetization to be determined as pre-folding if the scatter is least after correction for folding.
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Folco, Raymonde, B.A., M.A. (Laval –Les Îles) Ed. at Melbourne Univ., Australia (B.A.) and Concordia Univ. (M.A.)