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Working from outside the basin in to the Mare Basalts, they find the surface composition changes from Feldspathic breccias (Feldspar is a rock that crystallizes from magma) to shocked Anorthosite (a type of feldspar that makes up the light areas of the moon), to unshocked crystalline anorthosite, to high Calcium pyroxene (a rock made of silicate minerals) and pyroclastic rocks in the center.

研究发现:从盆地外边到盆地内部的玄武岩海(盆地内部的熔岩形成的地质结构),月球表面的地质结构依次是:长石质的角砾岩(长石是火山熔岩结晶形成的岩石)、经过冲击的粒状火成岩(构成月球阳面的一种长石)、没有经过冲击的粒状火成岩结晶体、高钙辉石(一种由硅酸盐构成的岩石),最中心的位置是分裂状的火山岩石。

Parisite is associated with secondary minerals, such as quartz, carbonate minerals, arfvedsonite, albite, chlorite, epidote and clay minerals and has intrinsic relation with reservoir.

氟碳钙铈矿常与石英、碳酸盐、钠铁闪石、钠长石、绿泥石、绿帘石、粘土矿物等次生矿物共生,并与天然气储层有着一种内在的联系。

Any of a group of abundant rock-forming minerals occurring principally in igneous, plutonic, and some metamorphic rocks, and consisting of silicates of aluminum with potassium, sodium, calcium, and, rarely, barium.

长石任何一组由大量岩石形成的矿物,主要存在于火成岩、深成岩以及一些变性的岩石中,含有钾、钠、钙及极少的钠的铝硅酸盐,地球的外层地壳中约百分之六十是长石

Any of a group of abundant rock - forming minerals occurring principally in igneous,plutonic,and some metamorphic rocks,and consisting of silicate s of aluminum with potassium,sodium,calcium,and,rarely,barium.

长石任何一组由大量岩石形成的矿物,主要存在于火成岩、深成岩以及一些变性的岩石中,含有钾、钠、钙及极少的钠的铝硅酸盐,地球的外层地壳中约百分之六十是长石

The molten salt leaching method to extract potassium from potash feldspar is studied in this paper.

研究采用熔盐浸取法从钾长石中提取钾的工艺,分别选用不同阴离子的钙盐,比较出选择不同助熔剂时其阴离子对钾长石中钾溶出率的影响,确定了最佳助熔剂为CaC l2。

Any of a common rock-forming series of triclinic feldspars, consisting of mixtures of sodium and calcium aluminum silicates.

斜长岩三斜晶长石系列中一种普通的成岩石,由钠和钙铝硅酸盐组成

For example, to CaSiO〓, wallastonite and cyclowallastonite could be found simultaneously in glazes between the temperature range of 1125℃±10℃, only wallastonite came out below the range, and only cyclowallastonite appeared above the range. Similarly, melilite structure and clinopyroxene structure connected with crystallization temperature. Usually, higher crystallization temperature contributes to forming melilite with simple structure and lower crystallization temperature contributes to clinopyroxene with complex structure.

如钙的偏硅酸盐,硅灰石、环硅灰石的转变温度区域为1125℃±10℃,组分适当的特定釉熔体,高于此温度出现环硅灰石,低于此温度出现硅灰石晶体结构;同样的,黄长石、辉石的出现也与温度有密切的联系,通常,晶体生长的温度较高有利于晶体结构简单的黄长石出现,晶体生长时温度较低有利于稍复杂的辉石结构的出现。

The hydrates of plain CAS glass are mainly gehlenite hydrate and CSH gel:and the preponderant hydrates or the mixture of CAS glass and gypsum are ettringite and CSH gel.

纯CAS玻璃相的水化产物主要为水化钙铝黄长石晶体和CSH凝胶:而掺有适量石膏的CAS玻璃相的水化产物则为钙矾石晶体和CSH凝胶。

Crystal structure of melilite is limited by MgO content of glazes, also restricted by O/Si ratio. Because of differences of ionic radius and ionic polarization capacity between Ca〓 and Mg〓, suitable O/Si ratio for melilite is influenced by content of CaO and MgO to a certain extent.

结晶釉中黄长石结构的出现,除了和MgO含量相关外,还受O/Si比值的限制;而Ca〓和Mg〓离子半径和离子间的极化能力的差异,使钙镁含量对形成黄长石结构的O/Si比值具有一定的影响。

The adsorption behaviour of chemically different superplasticizers, such as melamine formaldehyde sulphite polycondensate,β-naphthalene sulfonate formaldehyde polycondensate and polycarboxylate, on early hydrating cement phases was studied. For this purpose, pure ettringite AF(subscript t, monosulfate AF(subscript m and syngenite were prepared. The adsorbed amount and zeta potential of early hydration products were measured.

制备了钙矾石AF(下标 t、单硫型硫铝酸钙AF(下标 m和钾长石类单矿物,并研究了三聚氰胺磺酸盐甲醛缩聚物、β-萘磺酸盐甲醛缩合物及聚发酸盐等几种化学成分不同的超塑化剂在其早期水化颗粒表面上的吸附行为。

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