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平衡剖面正演模拟技术可快速、有效地正们盆地或局部构造的形成过程，合理地挪释盆地演化史和局部构造发展史．裂陷盆地构造沉降数值模拟可以估计上地壳与壳下岩石圈的伸展率及岩浆侵入体积．伸展率可用以计算裂陷盆地的古热流史，为预测烃源岩的演化程度提供依据．
Balanced cross-section forward modeling can quickly and effectively form the basin or local structure, and properly interpret the basin evolution history and local structure history. The tectonic subsidence numerical simulation of rifted basins can estimate the extensibility and magma intrusive volume of the upper lithosphere and the lower lithosphere. The extension rate can be used to calculate the history of pale-heat flux in rifted basins, which provides the basis for predicting the evolution of source rocks.