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• W2065648625 abstract "Outcrop-scale structures that record a progressive sequence of deformation can be used to clarify the kinematic evolution of an entire fold-and-thrust belt. The temporal progression of the compressional deformation as reconstructed by means of a mesoscopic structural analysis provides a key for unraveling the kinematic history of the Umbria-Marche Apennines (central Italy). Overprinting relationships at outcrop-scale allow for the recognition of three distinct structural stages which are, in sequence: A, layer-parallel shortening; B, folding; C, thrusting. Individual stages are explained in the framework of a progressive deformation model, where shortening of the sedimentary cover was continuous and occurred during a single contractional episode as a consequence of tip-line folding processes. A comparison of this history with those reported from other fold-and-thrust belts shows that layer-parallel shortening, folding and thrusting are sequentially dominant processes in areas which have experienced compressional deformation." @default.
• W2065648625 created "2016-06-24" @default.
• W2065648625 creator A5059917445 @default.
• W2065648625 date "1997-03-01" @default.
• W2065648625 modified "2023-09-24" @default.
• W2065648625 title "Structural evolution of a foreland fold-and-thrust belt: the Umbria-Marche Apennines, Italy" @default.
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• W2065648625 doi "https://doi.org/10.1016/s0191-8141(96)00093-4" @default.
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