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The Qianlishan Complex is a multiply deformed granulite terrane of the Khondalite Belt that represents a Paleoproterozoic continent-continent collisional orogen in the Western Block of the North China Craton. Two major stages of deformation (D 1 and D 2) were identified in the Qianlishan Complex. D 1 mainly produced NWW-trending overturned to recumbent intrafolial isoclinal folds F 1 , sub-horizontal penetrative foliations S 1 , NNE-SSW mineral lineations L 1 associated with top-to-the-SSW thrust shear, reflecting crustal thickening due to the NNE-SSW compression. D 1 was developed with the prograde (M 1) and peak (M 2) granulite-facies metamorphism. D 2 successively superposed the D 1 structures and was characterized by NWW-SEE-trending doubly plunging open to tight upright folds F 2 and minor sub-vertical axial planar foliations/cleavages S 2. D 2 was accompanied by post-peak near-isothermal decompression (M 3), probably related to exhumation following the crustal thickening. SIMS U–Pb zircon ages of deformation-related leucocratic dykes demonstrate that D 1 broadly occurred at 1976–1936 Ma and D 2 subsequently happened at 1936–1854 Ma. These results indicate that the Khondalite Belt underwent long-term (~100 Myr) polyphase deformation and high-grade metamorphism associated with magmatism. Timing constraints and kinematic compatibility suggest that the deformation sequence resulted from the NNE-SSW collision between the Yinshan and Ordos Blocks to form the Western Block at ~1.95 Ga. fx1 [ABSTRACT FROM AUTHOR]