ALONG-STRIKE VARIATIONS IN CURVED THRUST BELTS: EXAMPLES FORM THE CENTRAL-NORTHERN APENNINES OF ITALY
The Central-Northern Apennines of Italy developed during Neogene-Quaternary time following the closure of the Alpine Tethys. The orogenic stacking involved Triassic-Miocene carbonate platform-slope-basin sequences deposited on the Adria Mesozoic continental margin and overlying Miocene-Pliocene syn-orogenic siliciclastic sediments. Significant lateral variations in structural style and stratigraphy occur along the strike of the Apennines and are mostly related to the inherited pre-orogenic setting.
Thrust-related folds, spectacularly exposed in the Central-Northern Apennines (Gran Sasso and Olevano-Antrodoco-Sibillini thrust systems) are analyzed with the aim of reconstructing their along-strike variation in thrust-related folding mechanisms and unravelling their interference fold patterns. The Central-Northern Apennines are characterized by curved thrusts and remarkable lateral variations in thrust-related folds occur. Different folding mechanisms involve the same Lower Jurassic-Miocene carbonate slope-basin multilayer and their development has been selectively controlled by contrasting styles of compressional normal-fault reactivation. Pre-thrusting normal-fault transpressive reactivation promoted fault-bend folding along the N-S and NNE-SSW oblique ramps, whereas shortcut-propagating thrusts developed fault-propagation folds along the WNW-ESE and NW-SE frontal ramps. These two laterally changing thrust-related folds interact with a characteristic interference fold pattern produced by their synchronous/in-sequence growth and interaction in the salient apex of the curved thrust system.