Paleogeographic data suggest the first occurrence of the Taihangshan gravity lineament was initially formed during the Early Cretaceous, which is coeval with the peak of Mesozoic magmatism in this region.

• 岩相古地理分析说明太行山重力梯度带的雏形形成于早白垩世，与华北中生代岩浆活动的高峰相吻合。