D. Grujic, THE INFLUENCE OF INITIAL FOLD GEOMETRY ON TYPE-1 AND TYPE-2 INTERFERENCE PATTERNS - AN EXPERIMENTAL APPROACH, Journal of structural geology, 15(3-5), 1993, pp. 293
Experiments on superposed folding were performed in a plane strain-pur
e shear rig using paraffin wax as an analogue for rocks. A series of p
re-formed cylindrical folds were refolded with the compression directi
on acting parallel to the initial fold hinge direction, the intermedia
te axis perpendicular to the first fold axial plane and the extension
direction parallel to the first fold axial plane and perpendicular to
its axis (Type 1 interference geometry). Roundness, tightness and ampl
itude were varied to investigate the influence of first-fold geometry
on the interference patterns. Experimental folding of an initially pla
nar layer oriented parallel to the first-fold envelope provides a refe
rence geometry for comparison. The results suggest that hinge roundnes
s has less influence on the interference pattern than other factors. C
lose initial folds refold into Type 2 interference patterns, which bec
ome even more pronounced as the tightness increases; open folds produc
e Type 1 interference patterns. Folds with the same interlimb angle an
d the same roundness produce different interference patterns depending
on relative amplitude: folds with relatively large amplitude are refo
lded into Type 2 patterns, whereas folds with small amplitude give cle
ar dome and basin structures. In a second set of experiments, the comp
ression direction also acted parallel to the first-fold hinge, but the
orientations of the intermediate and extension axes were interchanged
. The interference patterns obtained are very similar to those in Type
1 interference geometry, suggesting that the major factor in determin
ing whether Type 1 or Type 2 interference patterns develop is the init
ial fold geometry and not the kinematics of the second deformation.