- 更多网络例句与石榴石相关的网络例句 [注：此内容来源于网络，仅供参考]
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The technology of separating rutile and almandine by flotation and the action mechanism of sodium hexametaphosphate[(NaPO3)6], a regulator, were investigated for realizing an effective separation of rutile and almandine, a main gangue mineral, in non-pollution.
为了实现金红石与主要脉石矿物石榴石在无污染条件下的有效分离，采用浮选方法研究了金红石和石榴石的分离，并采用红外光谱和X光电子能谱分析等手段研究了分离过程中调整剂六偏磷酸钠的作用机理。
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The action mechanism that (NaPO3)6 depresses almandine is two sides: one is that (NaPO3)6 is chemical adsorbed firmly on the surface of almandine and lead to almandine strong hydrophilic. The other is that (NaPO3)6 selectively dissolves Ca(superscript 2+) on almandine surface and makes the surface cations act with the collector lessening.
NaPO36对石榴石的抑制作用存在两种机理：其一，(NaPO3)6与石榴石表面Fe(上标 2+)发生化学键合导致其牢固吸附而使石榴石表面强烈亲水：其二，(NaPO3)6选择性溶解石榴石表面Ca(上标 2+)导致石榴石与捕收剂作用的表面活性质点减少。
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The garnets in Cretaceous sandstones come from blueschist that located in the southwest Tianshan and low-grade metamorphic rocks by lager proportionally. The garnets in Tertiary sandstones enrich almandine, which come from high-grade metamorphic rocks.
白垩系砂岩中的石榴石来自西南大山蓝片岩和低级变质岩的比例较大，而第三系砂岩中的石榴石中富铁铝榴石组分，多来自高级变质岩。
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2The studies on the appearance typomorphism, physical typomorphism, inner structure typomorphism and chemical typomorphism of the zircon and garnet, and the result of U-Pb isotopic age dating of zircon indicate that the zircons are meta-morphogenic genesis but two or three of them are magmatic genesis and most meta-morphogenic zircons have a basic magmatic zircon core which was generated in Stage of Yanshand and Indo-Chinese epoch. The genesis and origin of the garnet is very complicated. The garnets are main almandine with high Fe and Mg content and were proposed their souce rocks are mostly regional mid-degree-metamorphic rocks.
2研究锆石和石榴石的形貌标型、物性标型、内部结构标型以及成分标型特征和锆石U-Pb同位素测年结果表明，锆石除少数几个为岩浆锆石外，绝大多数是变质锆石，且中间多有形成于燕山-印支期的基性岩岩浆锆石残核；石榴石的成因及来源是比较复杂的，以铁铝榴石为主，且铁铝榴石中Fe、Mg的含量较高，推测其源区母岩主要以中级区域变质岩为主。
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The first generation garnet developed before the leucosome and heavily dissovled during the anatexis; the second generation garnet grew after the leucosome.
第一世代石榴石发育在浅色体结晶之前，并因强烈的深熔作用而受到严重溶解；第二世代石榴石在浅色体形成之后生长。
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It was also found that the film of smaller grains corresponded to a smaller lattice constant of the garnet structure, which implied that fewer Bi〓 ions substituted into the dodecahedral sites in the garnet, due to the fact that the smaller grains resulted in more grain boundaries, thus leading to more serious Bi segregation in the grain boundaries.
分析表明，细小的晶粒意味着薄膜中含有更多的晶界，这样将导致Bi组分在晶界上的偏析较显著，而进入石榴石结构中氧十二面体间隙的Bi〓较少，对于Bi，Al∶DyIG来说，石榴石相晶格常数与{Bi〓}〓呈正相关关系，由此可以解释具有细小晶粒的薄膜对应较小的石榴石相晶格常数。
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Andalusite-sillimanite type progressive metamorphic belt composed of chlorite-biotite zone, biotite-garnet zone, garnet-staurolite zone, staurolite-andalusite zone and sillimanite zone in Aletai Xinjiang is studied. According to the component zoning of the garnets, the relationship between metamorphism and deformation, and the paragenetic association evolution of the minerals, etc, the metamorphism is divided into three evolution stages: the stage before peak metamorphism, the peak metamorphism stage and the stage after peak metamorphism.
新疆阿勒泰地区发育了红柱石－矽线石型递增变质带，由绿泥石－黑云母带、黑云母－石榴石带、石榴石－十字石带、十字石－红柱石带和矽线石带组成，根据石榴石成分环带、变质与变形关系、矿物共生组合演化等特征，将变质作用分为峰前期、峰期和峰后期3个演化阶段。
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According to cpx-melt equilibrium pressure, the xenoliths types and simulating calculating of host rock REE partition pattern, source of sodic basalts is garnet lherzolite mantle, and the source of potassic basalt is metasomatic fluid altered phlogopite-containing garnet lherzolite mantle. For the alkaline basalts to sub-alkaline basalts, the melting degrees of the source rocks are 4%～15%.
根据单斜辉石—熔体平衡压力计算、所携带的包体类型及玄武岩稀土元素配分曲线的非实比部分熔融定量模拟表明，钠质玄武岩的来源为石榴石二辉橄榄岩源区，五大连池钾质玄武岩的源区是被交代的含金云母石榴石二辉橄榄岩源区，研究区碱性玄武岩到亚碱性玄武岩是石榴石二辉橄榄岩源区经4％～15％部分熔融程度的产物。
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But in sodium carbonate solution, any form of hydrogarnet can be decomposed into sodium hydrate alumino-silicate.
通过对钠硅渣和水化石榴石反应行为的热力学分析，发现高饱和系数( x ＞1)的水化石榴石不易被苛性碱分解，低饱和系数的水化石榴石易被分解而转化为钠硅渣，且钠硅渣也可以转化为水化石榴石，而在Na2CO3溶液中，任何形式的水化石榴石均能被分解生成钠硅渣。
- 更多网络解释与石榴石相关的网络解释 [注：此内容来源于网络，仅供参考]
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almandite：铁矾石榴石
almandine /铁矾石榴石/ | almandite /铁矾石榴石/ | almestrone /阿美雌酮/
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andradite：钙铁石榴石
常见的石榴石因应其化学成分而确认为六种种类,分别为红榴石(Pyrope)、铁铝石榴子石(Almandine)、锰铝石榴石(Spessartite)、钙铁石榴石(Andradite)、钙铝榴石(Grossular)(变种有沙弗来石(tsavorite)及肉桂石(hessonite))及钙铬榴石(U
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diopside garnetite：透辉石榴石岩
透辉闪长岩 diopside-diorite | 透辉石榴石岩 diopside-garnetite | 透辉花冈岩 diopside-granite
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garnet paper：石榴石砂纸
石榴石 garnet | 石榴石砂纸 garnet paper | 钢刺条(纺织) garnet wire
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garnet：石榴石
(6)非洲产特兰斯瓦尔玉(transvael jade),矿物名钙铝榴石(grossuar),石榴石(garnet)之变种,颜色翠绿,亦称非洲玉. 我国1987年曾有人当翡翠进口过. 透明~不透明. 硬度(h)7~7.5,比重(g)3.45~3.50,折光率n=1.73. (8)我国台湾产翡翠,
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white garnet：白色石榴石
White emerald 白祖母绿 | White garnet 白色石榴石 | White gold 白色金
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Ceylon garnet：锡兰石榴石
Ceylon diamond 锡兰钻石 | Ceylon garnet 锡兰石榴石 | Ceylon hyacinth 锡兰锆石
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scandium garnet：钪石榴石
scanatron 扫描器 | scandium garnet 钪石榴石 | scanistor 固态像扫描器
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brown-green garnet：棕绿石榴石
red garnet 红石榴石 | brown-green garnet 棕绿石榴石 | jade 玉石
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garnet brown：(红棕色)石榴石棕
garment piece ==> 衣片 | garnet brown ==> (红棕色)石榴石棕 | garnet film ==> 石榴石膜