泥质结构

矿石结构主要为泥质结构和显微鳞片泥质结构，构造主要为微层状、板状和致密块状；

The ore has the pelitic and microscale pelitic texture and the micro-bedded , tabular and dense massive structure .

用密度声波时差和自然伽玛测井曲线计算分散泥质结构泥质含量

Calculation of Shaly Content In the Dispersed Shaly Structure from Density , Acoustic Transit Time and Gamma Ray Logs

泥质岩微孔结构及其与扩散系数关系

The micropore structure of argillaceous rock and its correlation with diffusion coefficient

分析发现，泥质板岩的结构以变晶结构为主，包含了由石英晶体形成的颗粒状矿物集合体和由高岭石、白云母和斜绿泥石形成的片状矿物集合体，但以片状集合体为主。

Analysis showed that the main type of structure in argillite was crystalloblastic texture , which contains granular mineral aggregates made of quartz crystal , and schistose mineral aggregates made of the crystals of kaolinite , muscovite and clinochlore .

结合现代土力学原理，系统分析了风化泥质软岩的结构特征，膨胀特性；

From the principles of modern soil mechanics , the structural and swelling characteristics of soft clayey rocks were analyzed systematically .

通过对三肇地区岩石物理资料分析，确定岩性细、泥质重、空隙结构复杂造成是造成不动水饱和度高进而引起低阻油层的主要岩石物理成因。

Heavy mud , complex pore structure is the main causes of rock physics , and it causes of the high immobile water saturation and causes of low resistivity oil layers .