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
方面，在原鲁谷组灰岩和火山岩层位之
现一套以类复理
为主的深水，特别是“冰水杂砾岩”；
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.
摘要地层古生方面，在原鲁谷组灰岩和火山岩层位之现一套以类复理为主的深水，特别是“冰水杂砾岩”；
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