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1)  upper part of No.3 Member of Tongziyan Formation
童子岩组第三段上亚段
1.
Regression Analysis of Coaly Chemical Indieator on upper part of No.3 Member of Tongziyan Formation Coal Measures in ChangfushanMining Area;
童子岩组第三段上亚段各煤层提供了新的对比依据。
2)  first member of Tongziyan formation
童子岩组一段
3)  Upper Submember of the Fourth Member of the Shahejie Formation
沙河街组第四段上亚段
1.
High-resolution sequence stratigraphic framework of the Upper Submember of the Fourth Member of the Shahejie Formation on the southern slope of the Dongying subbasin,northern Shandong,China;
鲁北济阳坳陷东营凹陷南坡沙河街组第四段上亚段高分辨率层序地层格架
4)  Es3~1
沙三上亚段
1.
Physical properties of Es3~1 reservoir of Youyi Oilfield and their control factors;
友谊油田沙三上亚段储层物性特征及控制因素分析
5)  the V-rock member of Yan'an Formation
延安组第Ⅴ岩段
6)  the 3~(rd) Member of Badong Formation
巴东组第三段
1.
Weak intercalated layers in the 3~(rd) Member of Badong Formation(T_2b~3)are the principal structural plane,13 major penetrative weak intercalated layers within 270m thick rock mass were revealled by deep-seated deformation monitoring profiles in Baitupo slope in Badong new town-site of the Three Gorges reservoir.
巴东组第三段中的软弱夹层是白土坡斜坡的主要结构面,巴东新城白土坡深层变形监测钻孔揭露白土坡斜坡巴东组第三段厚度在270m左右,主要贯通性软弱夹层有13层,为泥质灰岩碎块石夹土、黄褐色碎石土,中上部夹层分布较密,软弱夹层的空间分布由沉积环境所决定的岩性变化控制,典型夹层露头构造分析表明夹层由于构造作用发生过层间错动,夹层的存在有利于斜坡深层变形,三峡水库蓄水后水位的抬高将会影响到斜坡岩体的深层蠕变。
补充资料:段成式
      见《酉阳杂俎》。
  

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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