沉积相模式(Sedimentary facies model) 是对沉积环境、沉积作用及其结果(沉积相)三者相互联系的揭示和描述,是对沉积相的成因解释和理论概括。
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Since this sedimentary facies model consists of points in the vector space, zonation can be made according to the principle of "shortest distance" between vector points.
这种沉积相模型为矢量空间上的点,可以按矢量点之间的最短距离原则分层。
At last, according to the palaeogeography characteristic and sedimentary evolution model, the general sedimentary facies model of Jurassic in Qiangtang basin was founded.
根据羌塘盆地侏罗系古地理特征及沉积演化模式,建立了适合于本区的侏罗系综合沉积模式。
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