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Relationship Between Parasitic Folds and Tectonic Evolution, Potato Hills, Ouachita Mountains, Oklahoma
Parasitic folds are present in a fault-related anticline in the central Potato Hills. The development of these minor folds indicates an early, overall layer-parallel shortening event occurred in the Potato Hills region before significant folding. This supports the hypothesis that the North Potato Hills thrust is a back thrust indicating a window is nonexistent.
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