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沉积盆地构造热演化模拟建立在盆地成因的地质地球物理模型基础之上 ,其中包括运动学模型、运动学—流变学模型和动力学模型。运动学模型在预测盆地热流演化方面具有优势 ,但在预测构造沉降等几何形态方面存在一定的缺陷 ;运动学—流变学模型的优势在于构造演化模拟 ,在热演化方面类似于运动学模型 ;动力学模型蕴含着潜在的巨大优势 ,只是目前还存在一些阻碍因素。构造热演化正演模型的进一步完善及正、反演模型的匹配将是未来构造热演化模拟的发展趋势
The tectonic thermal evolution modeling of the sedimentary basin is based on the geological geophysical model of the genesis of the basin, including the kinematics model, the kinematic-rheological model and the kinetic model. The kinematic model has some advantages in predicting the evolution of basin heat flux, but it has certain defects in predicting the geometry of structural subsidence. The kinematic-rheological model has the advantages of tectonic evolution simulation and similar kinematic model in terms of thermal evolution. Kinetic model contains great potential advantages, but there are still some obstacles. The further perfection of forward modeling of thermal evolution and the matching of forward and inverse models will be the trend of future tectonic thermal evolution simulation