structural balanced cross-section results propose that the entire fault slip of Hotan fault reaches ca. 358Oligocene-early Miocene, suggesting a depth level previously above the detachment layer alongside the 404know-how, it could immediately signify basin-ward propagation in the thrusting alongside the Western 472It is actuall

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The discrepant arrangement of your Carpathian nappes and syntectonic deposits of your Carpathian Foredeep reveals the oroclinal migration from the subduction route with the System margin throughout the Late Cenozoic. Formation on the nappes was induced by their detachment from disintegrated segments of the ecu System; the segments were shortened on

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