Active fold deformation and crustal shortening rates of the Qilian Shan Foreland Thrust Belt, NE Tibet, since the Late Pleistocene

Quantification of crustal shortening rates across foreland fold-and-thrust belts is essential for evaluating how convergence is accommodated throughout the orogenic belt and analyzing seismic hazard in neighboring cities. In this study, we focused on active fold along the western portion of the Qili...

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