The flyschoid-dominated deep-water sediments especially the "glaciofluvial diamictites" are found to be overlain by the formerly Lugu Formation limestones and volcanic horizons.
摘要地层古生物方面，在原鲁谷组灰岩和火山岩层位之下新发
以类复理
沉积为主
沉积物，特别是“冰杂砾岩”；
The flyschoid-dominated deep-water sediments especially the "glaciofluvial diamictites" are found to be overlain by the formerly Lugu Formation limestones and volcanic horizons.
摘要地层古生物方面，在原鲁谷组灰岩和火山岩层位之下新发以类复理沉积为主沉积物，特别是“冰杂砾岩”；
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