1.【地】泥岩
1.a gray sedimentary rock formed from mud, similar to shale but with less developed lamination
1.The graptolites are generally preserved as films in mudstones or muddy siltstones at the depths of thousands meters beneath the surface.
这些笔石标本一般保存成薄膜状于数千米之下的泥岩或泥质粉砂岩之中。
2.Dark mudstones are widely developed in Lindian fault depression, organic matter abundance in marine source rocks is in middle level.
林甸断陷地层的暗色泥岩并不发育，有机质丰度总体上属于中等水平。
3.The geochemical characteristics of inclusion and clay-adsorbed oils correlate well with the lacustrine mudstones.
油气包裹体和粘土吸附油气组分具有明显的湖相泥岩地球化学特征。
4.AVO characteristics were ambiguous in thin-layer interbed sandstones and mudstones of terrestrial facies of Daqing area.
大庆地区陆相砂泥岩薄互层AVO特性不明显，甚至没有显示。
5.terrestrial source rocks deposited under oxic conditions, probably Middle to Late Jurassic mudstones.
陆源岩沉积好氧条件下，可能晚侏罗世泥岩中。
6.The frequent change of water depth resulted in the frequent alternation of dark mudstones and lowlevel salt rock and sandstone.
高水位和低水位的频繁变化导致深水暗色泥岩和低位盐、低位砂的纵向叠加。
7.Mudstones are regional cap rocks, which mainly distributed in K1d2 and strata above it.
高声波时差火山岩盖层主要分布在营一段顶部，为局部盖层。
8.The mudstones provide an effective seal.
此泥岩提供了有效的封闭。
9.Geochemical characteristics of Tertiary mudstones in Kuqa depression and their implications to tectonic setting and provenance attribute
库车坳陷第三系泥岩地球化学特征及其对构造背景和物源属性的指示
10.Comparison of Geochemistry Character between Mudstones from Deep Lacustrine Facies and Coal Measures by Hydrous Pyrolysis
加水热模拟中深湖与煤系泥岩地化特征比较