陆源碎屑（terrigenous clast）是指陆源区母岩经物理风化或机械破坏而形成的碎屑物质。
对碳酸盐与陆源碎屑的混合沉积的研究具有重要意义。
Sedimentogenic significance of mixed carbonate and siliciclastic sediments is emphasized.
尤以陆源碎屑重力流，沉积厚度大、分布面积广，十分发育。
The terrigenous elastic gravity flow deposits are more significant due to its great thickness and broad distribution extent.
在晚期碎屑沉积阶段，主要表现为陆源碎屑沉积作用，成矿作用相对甚弱。
The extremely poor mineralization occurred in the late clastic sedimentary stage, and corresponds to the sedimentation process of the terrigenous clastics.
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