1) micritic rind
泥晶质壳层
2) properties of shell
壳层性质
3) shell layers
壳质层
1.
Upon careful observation under scann ng electron microscope, it can be found that the shell thicknes is obviously controlled by the varieties of shell layers.
腹足类个体发育中壳质结构的重要特点是壳质层的微观变化，包括原有壳质层的增厚、增生与上覆超微结构相同的壳质层、增生新的超微结构层、壳质层的相互消长与显微结构的演变。
4) mudstone layer
泥质岩层
1.
Water is easily preserved in the pores and forms the undercompaction of the mudstone layer.
泥质岩层中的孔隙水在向外排运的过程中遵循低速非达西流动规律。
5) laminated shale
层状泥质
1.
Based on parallel conductance between laminated shale and dispersed shaly sands, and the assumption under which dispersed shaly sands are described with dual water conductivity model, a new dual water conductivity model for laminated and dispersed shaly sands is established.
基于层状泥质和分散泥质砂岩并联导电,采用双水电导率模型来描述分散泥质砂岩导电规律,建立了混合泥质砂岩双水电导率模型。
2.
Based on the hypothesis that the laminated shale and dispersed shaly sand are parallel conduction,and the conduction theory for 3-dimensional periodic array of charged spheres immersing in electrolyte,a new generalized double layer conductivity model is proposed for laminated and dispersed shale coexisting in shaly sand.
基于层状泥质与分散泥质砂岩并联导电理论,以及悬浮于电解液中三维周期排列带电球体导电理论,建立了分散泥质和层状泥质同时存在的混合泥质砂岩通用双电层电导率理论模型。
3.
Based on the parallel conductance between laminated shale and dispersed shaly sand,and new electric double layer conductivity model for dispersed shaly sand,then a new generalized electric double layer conductivity model is proposed for laminated and dispersed shaly sand interpretation.
基于层状泥质与分散泥质砂岩并联导电的理论,以及新的分散泥质砂岩双电层电导率模型,建立了分散泥质和层状泥质同时存在的混合泥质砂岩通用双电层电导率模型;分析了影响模型的因素。
6) shaly formation
泥质地层
1.
Determination of saturation exponent in shaly formation;
泥质地层中饱和度指数的确定
补充资料：闭壳层离子
分子式：
CAS号：
性质：又称偶电子离子(even-electron ion)。在有机质谱分析中形成的外层电子完全成对的离子，缩写为EE，标志符号为+，如EE+。化学电离所产生的初始离子，主要是EE+离子，如(M十H)+和(M-H)+。
CAS号：
性质：又称偶电子离子(even-electron ion)。在有机质谱分析中形成的外层电子完全成对的离子，缩写为EE，标志符号为+，如EE+。化学电离所产生的初始离子，主要是EE+离子，如(M十H)+和(M-H)+。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条