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主要概述了伸展背景下砂质沉积物在不同构造样式下的沉积型式的研究进展。近来的研究日益表明特定的沉积型式与所处单元构造样式之间存在特定的联系。沉积盆地边缘—斜坡地区具有不同的构造样式 ,控制了砂质沉积物的沉积型式包括来源区、水流方式、砂体几何形态与分布以及沉积构成等。
The research progress of sedimentary types of sandy sediments under different tectonic styles is mainly summarized. Recent research has increasingly shown that there is a specific connection between a particular sedimentary pattern and the cell’s construction style. Sedimentary basins have different tectonic styles in the margin and slope area and control the sedimentary types of sandy sediments including source area, water flow pattern, geometry and distribution of sand bodies and sedimentary composition.