Lithotectonic elements of Precambrian basement in the North China Craton: Review and tectonic implications

► Neoarchean basement in the NCC was formed at two distinct periods: 2.8-2.7 Ga and 2.6-2.5 Ga. ► The 2.8-2.7 Ga is considered as a major period of juvenile crustal growth in the NCC. ► The formation of the 2.6-2.5 Ga basement in the NCC was most likely related to mantle plume activities. ► Paleoproterozoic basement rocks in the NCC are mainly restricted to three linear tectonic belts. ► Subduction/collision was involved in the development of the Paleoproterozoic belts in the NCC.