Several functions have been chosen in order to approximate fold profile geo
metry. Some of them are valid mainly for alloclinal folds (interlimb angle>
0), whereas others are mainly valid for isoclinal folds (interlimb angle =
0). In all cases, a fold profile can be characterised by an aspect ratio (y
(0)/x(0)) between the height and the width of a limb (fold amplitude), and
a shape parameter characteristic of the considered function. The shape para
meters have been mutually linked through the area beneath the fold profile.
The geometrical analysis enables a graphical classification based on a sha
pe-amplitude diagram in which the most common types of folded surfaces are
represented: cuspate, chevron, sinusoidal, parabolic, elliptic and box fold
s. Any of the shape parameters can be used as x-axis of the diagram in orde
r to approximate the geometries commonly exhibited by natural folds. In the
diagram presented in this paper two shape parameters have been combined: t
he exponent n of a power function for alloclinal folds, and a parameter C/y
(0), defined from a function composed of an elliptic part and a line segmen
t of length C for isoclinal folds. In order to show the suitability of the
classification method, it has been applied to some examples of finite-eleme
nt, experimental and natural folds. (C) 1999 Elsevier Science Ltd. All righ
ts reserved.