Kinematic history of the Tan-Lu fault zone constrained by the Late Mesozoic–Cenozoic tectono-sedimentary evolution of basins in the Luxi Block, eastern North China Craton

•The development of basins in the Luxi Block are closely related to the Tan–Lu Fault Zone.•The basins in the Luxi Block were involved in NE–SW compression (150–145 Ma), NE–SW extension (145–122 Ma) and N–S extension (63–32 Ma).•The Tan–Lu Fault Zone experienced sinistral strike-slip, normal faulting and dextral strike-slip in Late Jurassic–Paleogene.•The change from compression to extension at ∼145 Ma in the Luxi Block represents the initiation of craton destruction.