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All of these were composed of plants adapted to the difficult conditions due to the clayey chalk support composed by the rubble.

所有的这些树林都是由这些适应了不利立地条件的植物组成,不利的立地条件也是那些由废渣碎石产生的粘土状的白垩导致的。

By summarizing the futures of the relative permeability curve in low permeable reservoirs and study of the futures of relative permeability curve in lithic arenite which rock fragments are most come from tuff and lava, it is the reservoirs rock character, the type of detrital minerals, the degree of grains coarse and the lay out of clay mineral that are main influencing factors which influence the relative permeability curve.

本文在总结低渗透油藏油水相对渗透率曲线特征的基础上,对以火山岩、凝灰岩岩屑为主的岩屑砂岩相对渗透率曲线特征进行研究,并分析了其影响因素,研究表明低渗透储层的岩石学特征,碎屑颗粒的成份、结构,其表面的粗糙程度,及其粘土矿物的产状对相对渗透率曲线有明显的影响。

L Slate - Soil type that is the most common found in the Mosel region that is a dark gray, plate like rock that formed when clay, shale, siltstone and other sediments are subjected to pressure.

l 板岩-一种深灰色、扁平状的岩石,由粘土、泥板岩、泥沙岩和其他沉淀物受压力形成。在默塞尔地区非常常见。

A platy, pale green mineral of the mica group of sheet silicates, also considered to be a type of clay mineral, found in sedimentary and low-grade metamorphic rocks.

片状硅酸盐的云母族中的一种板状的浅绿色矿物,成分〔128O2o16〕,也被认为是粘土矿物的一类,见于沉积岩和低级变质岩中。

The results show that mineral compositions of the sediments are smectite, illite, palygorskite and chlorite, and the fibrous or acicular palygorskites are typically authigenic,which grew along the edges or the surfaces of platy smectite, respectively.

结果表明,晚渐新世循化盆地沉积物中粘土矿物组成主要有蒙脱石、伊利石、坡缕石和绿泥石等;坡缕石一般呈纤维状或者针状,沿片状蒙脱石的边缘及表面交代生长,为典型自生成因的坡缕石。

A tunneling machine for producing large tunnels in soft rock or wet, clayey, unconsolidated or bouldery earth by simultaneously detaching the tunnel core by thermal melting a boundary kerf into the tunnel face and forming a supporting excavation wall liner by deflecting the molten materials against the excavation walls to provide, when solidified, a continuous wall supporting liner, and detaching the tunnel face circumscribed by the kerf with powered mechanical earth detachment means and in which the heat required for melting the kerf and liner material is provided by a compact nuclear reactor.

&…一个在软岩石,或湿的、粘土状的、疏松的,或巨砾泥土中挖掘隧道的隧洞掘进机,用先进的以上升暖气流进行隧道核心分离,将边界切口熔入隧道面,同时通过使偏倚在隧道壁上的熔融物料在凝固时提供一个连续墙来支持衬垫,形成一个支持挖掘的墙壁;破碎在切口周围划了界限的隧道核心-用有动力的机械土地分离的方法,在隧道核心中,需要如此操作的热力以及衬垫物料由一个小型的核反应堆提供……&

Pillaring reaction has been well known as one of the significant methods to prepar porous materials and inorganic-organic nanocomposites.

粘土矿物的柱撑反应是制备孔材料、有机一无机纳米复合层状材料的有效方法之一。

Pillaring reaction has been well known as one of the significant methods to prepar porous materials and inorganic-organic nanocomposites.

粘土矿物的柱撑反应是制备孔材料、有机-无机纳米复合层状材料的有效方法之一。

The thermatic fibrous sepiolites are ones of rich Magnesium,richened with Magnesium,silicon and few Aluminum,and the sedimentary clayey sepiolites are ones of rich Aluminum,have lower Magnesium,Silicon and higher Aluminum.

本文通过两种不同成因海泡石化学成分特征的研究发现,热液型海泡石和沉积型海泡石的化学组成有较大差异,热液型纤维状海泡石MgO、SiO2含量高,Al2O3含量低,为富镁海泡石;沉积型粘土状海泡石MgO、SiO2含量低,Al2O3含量高,为富铝海泡石。

Recent developments in the research on the geology and geochemistry of the newly-discovered clayey breccias at the lop of the Xiaochaka Formation in the Juhuashan, Xiaochaka and Shishuihe areas, Qiangtang Basin, northern Tibet have disclosed that mineral compositions, textures and structures, occurrences and sectional architectures of the clayey breccias agree well with those of the paleo-weathering crust in these areas. Compared with the bedrocks, the paleo-weathering crust is characterized by the leaching out of CaO and CO2, and relative enrichment of SiO2, Al2 O3, Fe2O3, K2O, Na2O, MnO and P2O5. The clayey weathered residues in the paleo-weathering crust are characterized by marked enrichment of REEs, much higher contents of LREEs than those of HREEs, markedly positive Ce anomalies and negative Eu anomalies, and a noticeable increase in other element contents besides Mo, Sn and U from the clayey weathered residues.

对最近在藏北羌塘盆地菊花山、肖茶卡、石水河等地区新发现的肖茶卡组顶部的粘土质角砾岩的地质、地球化学特征研究表明:其岩石矿物成分、结构构造、角砾层产状及剖面演化序列等与古风化壳的形成及其特征较为一致;相对于基岩,古风化壳的主量元素表现为CaO、CO2的淋失和SiO2、Al2O3、Fe2O3、K2O、Na2O、MnO、P2O5等不同程度的相对富集;古风化壳中的粘土质风化残积层的稀土元素具有明显的富集,表现为LREE含量远大于HREE的特征,存在明显的Ce的正异常以及Eu的负异常;微量元素除Mo、Sn和U外,粘土质风化残积层的其余元素含量均有明显的增加。

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