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- They are mainly residue original interganular pore and secondary pore.Residue original intergranular pore has been preserved by the authigenic clay minerals and quartz overgrowth. 剩余原生粒间孔是成岩早期淀粘土及石英加大形成的，它们围绕碎屑边部分布。
- The diagenetic stage and pore-evolution properties of clastic rock can be effectively determined according to the assemblage of authigenic clay mineral. 根据自生粘土矿物的组合特征，可以有效地确定碎屑岩的成岩阶段及其孔隙发育特征。
- It is suggested the authigenic clay mineral in clastic rock be classified into four types,named mixed layer of illite and montmorillonite, illite,chlorite and kaolinite. 得出了碎屑岩中的自生粘土矿物分为伊／蒙混层、伊利石、绿泥石和高岭石4种基本类型；
- An Improved Method for Separation of Authigenic Clay Minerals from Sedimentary Rocks 沉积岩中自生粘土矿物分离提纯方法的改进
- EXTRACTION METHOD AND SIGNIFICANCE OF AUTHIGENIC CLAY MINERALS IN SEDIMENTARY ROCKS FOR K-Ar AGE DATING 油气储层钾氩定年中的自生粘土矿物提纯技术及意义
- authigenic clay minerals 自生粘土矿物
- Identification method of authigenic clay mineral in sedimentary rock by SEM & XEDS GB/T17361-1998沉积岩中自生粘土矿物扫描电子显微镜及X射线能谱鉴定方法
- They are stabilized through absorption by clay minerals. 它们通过粘土矿物的吸收作用而得到稳定。
- Two basic types of clay minerals are present in most soils. 大多数土壤中出现了两类主要的粘土矿物。
- The formation of authigenic clay minoral is related to clastic components of clastic rocks. 自生粘土矿物的形成与碎屑岩的碎屑组分有着密切的关系；
- SEM proves that the form of clay minerals is floccule and sheety. SEM结果显示东太平洋粘土矿物为絮状和片状；
- Clay minerals are the mixture of chlorite and smectite and illite. 粘土矿物主要为绿泥石／蒙脱石混层和伊利石；
- The formation and conversion of authigenic clay mincral were dominated by initial mineral components and diagenetic environment of clastic rock. 自生粘土矿物的形成和转化取决于碎屑岩原始矿物组分及其成岩环境。
- In this paper,the adsorption effect of Zn~(2+) by three clay minerals,i. e. 探讨了在不同矿物投加量、不同振荡时间、不同Zn2+浓度、不同矿物颗粒细度和不同pH条件下,钠基膨润土、膨胀蛭石和沸石三种粘土矿物对Zn2+的吸附效果,并比较了三种粘土矿物对Zn2+的吸附差异性。
- SiO-2, Al-2O-3 and Fe-2O-3 are three main parts in the clay minerals. 红土中粘粒部分的主要化学成分为SiO2 ,Al2 O3和Fe2 O3;
- The main types of clay minerals are illite, smectite, kaolinite and chlorite. 粘土矿物主要由伊利石、蒙皂石、高岭石和绿泥石组成。
- Based on the authigenic and clay mineral assemblage, two types of diagenetic ambient have been recognized in the Meso-Cainozoic detrital rocks in Tarim basin. 根据自生矿物与粘土矿物组合，在塔里木中新生界碎屑岩中可以识别出两种成岩环境。
- The ability of clay minerals to catalyse decarboxylation has long been recognised. 粘土矿物能催化脱羧基是早已认识到的问题。
- The surface area of crystalline clay minerals is highly dependent on the extent of lattice expansion. 结晶粘土矿物的表面积主要依赖于晶格膨胀的程度。
- Specific evidence for coordination complexes between pesticides and clay minerals is quite limited. 关于农药和粘土矿物之间的配位络合的明确证据是十分有限的。
