Occurrence of both carbonate and siliciclastic sources, active hydrodynamic regimes, alternate dry and wet climates, and the fluctuation of sea level are main factors for forming mixed sediments.
形成混合沉积的条件是具备碳酸盐和硅质碎屑两类物源、活跃的水动力和干湿交替的气候，此外，海平面的相对波动也会造成积极的影响。
Sedimentogenic significance of mixed carbonate and siliciclastic sediments is emphasized.
对碳酸盐与陆源碎屑的混合沉积的研究具有重要意义。
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