Given the fact that Mesozoic magmatism was closely related to the lithospheric thinning, it is proposed that the diachro由于岩浆作用与岩石圈减薄作用密切相关，因此认为华北岩石圈减薄的时空不均一性是形成太行山重力梯度带的重要机制。
The spatial heterogeneity of the lithospheric mantle beneath North China may have resulted from the diachronous thinning华北岩石圈组成的空间不均一性可能与岩石圈减薄过程的时空差异有关。