In the late early Cretaceous, the NCC turned into contraction stage again by the influence of the subduction of Pacific plate and Indian plate.

• 早白垩世晚期该区受太平洋板块和印度洋板块俯冲作用影响,华北板块再次转入挤压作用阶段,开始了滨太平洋域的演化。