动力学预测,可指出厚层粒屑灰岩分布的根据,大多数粒屑灰岩是内源异化颗粒经过古湖泊中风浪及湖流的搬运、分选和再分配的结果,厚层粒屑灰岩主要发育于湖水动能由强转弱的突变区,主要分布在多砂水系入湖区以外,岸线平直的湖盆四角、岸线曲折的湖盆湾口,岛屿的近陆一侧,水下隆起的顶部及斜坡上的凹折带.曾对济阳坳陷第三系厚层粒屑灰岩分布区作了预测,并己为钻探所证实. Kinetic prediction can be based on the distribution of thick-grained litter, most of which are the result of the handling, sorting and redistribution of endogenous alien particles through the waves and lakes of ancient lakes, Limestone mainly develops in the abrupt area where the kinetic energy of the lake weakens from strong to strong, mainly distributed outside the inflow area of ​​the multi-sand water system, the four corners of the lacustrine basin with straight shoreline, the lacustrine bay with tortuous shoreline, the inland side of the island, Lower uplifted tops and dipping belts on slopes. Predictions of the Tertiary thick-bedded granulite limestone distribution in the Jiyang Depression have been predicted and confirmed by drilling.