综合考虑陆源碎屑物供给、内源碳酸盐岩没积、沉积物侵蚀与再沉积、重力流沉积以及构造升降和水平位移等诸多地质因素，建立了一个能够模拟各型盆地的综合数学物理方程式。采用自行研制的定量层序地层模拟系统，以断陷湖盆坡带（泌阳断陷双河～赵凹地区为例），分别模拟了：①湖平面变化过程及其陆相层序响应机制；②基底构造沉降过程及其陆相层序响应机制；③物源供给过程及其陆相层序响应机制。 Considering the geological factors such as terrigenous detritus supply, endogenous carbonate sedimentation, sediment erosion and redeposition, gravity flow deposition and tectonic movements and horizontal displacements, an integrated mathematical physics model equation. Using the quantitative sequence stratigraphic simulation system developed by ourselves, taking the fault zone of the basin (Shuanghe ~ Zhao’ou area in Biyang fault depression as an example), we respectively simulate: ①the change of lake level and the response mechanism of its continental sequence ; ② sedimentation process of the basement and continental facies sequence response mechanism; ③ source supply process and continental sequence response mechanism.