据堆积过程，把自然泥石流堆积地貌分为古泥石流台地、老泥石流台地和近代泥石流长柄扇。
According to the genesis, the accumulational landform of debris flow may be classified into natural and man-made ones.
东达村组自下而上为冲积扇泥石流沉积、无障壁碎屑滨岸沉积和浅水碳酸盐台地潮坪沉积。
The Dongdacun Formation consists in ascending order of alluvial fan debris flow deposits, barrier-free clastic littoral deposits and shallow-water carbonate platform tidal-flat deposits.
松辽盆地东南缘六台地区营城组二段发育一套冲积扇砾岩层。
A set of conglomerates of alluvial fan occurred in the second member of Yingcheng Formation of Liutai, southeast margin of Songliao Basin.
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