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• W2085883971 startingPage "497" @default.
• W2085883971 abstract "Multilayer folding models provide a framework for evaluating fold kinematics, but have limited applicability for tight folds. A careful analysis of the tight Canyon Range (CR) syncline, a natural, multilayer fold (of alternating competent quartzite and incompetent argillite layers) formed in the elastico-frictional regime, yielded the following results. (1) Fracturing and cataclastic flow occurred at multiple scales. Variations in deformation style across scales are a function of matrix-controlled versus block-controlled cataclastic flow. (2) Competent and incompetent layers switched roles in controlling fold geometry between ∼40° and ∼60° limb dips; models predict this switch at 60°. (3) Parasitic folds formed during later stages of fold-tightening, while most models assume that they form during early stages of folding. (4) During fold-tightening, layer-parallel shortening structures were reoriented to accommodate vertical extension. We use multilayer folding models for initial first-order analysis of the CR syncline's kinematic history. Some of our data stray from model predictions. We use the location and timing of these variations to explain how/why the fold differs from anticipated results; this suggests critical details that may be overlooked and/or oversimplified in established folding models. Thus, kinematic details unraveled from the CR syncline improve our understanding of general multilayer fold models." @default.
• W2085883971 created "2016-06-24" @default.
• W2085883971 creator A5008355047 @default.
• W2085883971 creator A5010227151 @default.
• W2085883971 date "2007-03-01" @default.
• W2085883971 modified "2023-09-27" @default.
• W2085883971 title "Deformation in the core of a fold: Unraveling the kinematic evolution of tight, multilayer folds developed in the upper crust" @default.
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• W2085883971 doi "https://doi.org/10.1016/j.jsg.2006.09.012" @default.
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