Summary
The main features of the fold and fault geometry of the Helvetic nappes and Chaînes Subalpines of Switzerland and France have been determined by the construction of tie lines between outcropping hinge points of folds and cut-off points of strata against thrusts. Longitudinal correlation of these structures is now possible. Folds are very persistent along their hinge lines and can often be followed for tens of kilometres. Fold hinges and thrust plane cut-off lines are extremely regularly oriented. The Alpine structures developed in the external massifs are obliquely superposed on previously emplaced nappes. The overall structural pattern is attributed to a progressive change of the relative displacement directions between the northern (European) plate and southern (Apulian) plate from N-S, through NW-SE, concluding with movements in an E-W sense. The well known structural culminations and depressions are interpreted as the result of the latest shortening in an E-W direction and not to complex ramp geometry or to duplex stacking.
- © 1989 The Geological Society