The development of flanking folds during simple shear and their use as kinematic indicators

We used a numerical finite element simulation to model the formation of fla nking folds around rotating planar structures (e.g. veins, faults or dykes) in a non-linear viscous medium during ideal simple shear. If the planar st ructure is much more viscous than its host it does not deform and flanking folds with no displacement along the structure develop. Their vergence is c onsistent with the overall sense of shear. However, if the planar structure is much less viscous than its host, strain is concentrated within the stru cture and a secondary shear zone is developed in which slip is opposite to the overall sense of shear. Then, flanking folds develop that have a vergen ce, which is incompatible with the drag on structure. If the deflection of markers is not clearly preserved, then such flanking folds can be easily mi sinterpreted as shear bands indicating a wrong shear sense. The deflection of the foliation in flanking folds is very similar to deformed asymmetric p ull-aparts and can therefore help to interpret these otherwise ambiguous sh ear sense criteria. Because our model (ideal simple shear boundary conditio ns) fails to describe back-rotation of planar structures in rocks we specul ate that shear band geometries are indicative for general shear. (C) 2001 E lsevier Science Ltd. All rights reserved.