- 更多网络例句与黄玉岩相关的网络例句 [注：此内容来源于网络，仅供参考]
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Feldspars (including albite and K-feldspar) and amblygonite are the main reserves of the whole-rock phosphorus in the Yashan topaz-lepidolite granite, and the contribution of feldspars to whole-rock phosphorus is related with the crystallization of amblygonite.
长石及磷锂铝石是雅山黄玉锂云母花岗岩中磷的主要贮体，磷锂铝石的出现与否直接影响了长石的磷含量及其对全岩磷的贡献率。
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The presence of REE tetrad effects in apatites and whole rocks of S-type granites has been reported by Sha and Chappell (1999) and Zhao et al.(1999), respectively. The REE tetrad effect in minerals, such as apatite, spessartite, beryl, alkali feldspar and spodumene, from all zones of Altay No. 3 pegmatite has been found remarkable, and the fractionations among isovalent incompatible elements in these minerals are also significant. This paper puts forward that the REE tetrad effect is one of the basic features of peraluminous melts and the origin of REE tetrad effect might be probably related to some processes prior to the formation of pegmatite magma. The immiscibile liquid separation between silicate melt and hydrosaline melt may be responsible for it.
由于阿尔泰3号伟晶岩脉各带磷灰石以及与其共生的石榴石、绿柱石、碱性长石、锂辉石矿物均存在明显的稀土"四重效应"以及相同电价、相似离子半径的不相容元素间存在显著的分异，并结合最近赵振华等(1999)和Sha and Chappell(1999)报道S型花岗岩全岩和单矿物(磷灰石、独居石、长石、黄玉等)均存在稀土"四重效应"这一现象，本文研究提出，稀土"四重效应"是富挥发分过铝质岩浆体系的一个基本特征，其机制既不可能由含稀土的副矿物早期结晶引起残余熔体相中REE含量变化的结果，也不能定性地归因于流体相与熔体相相互作用过程中稀土元素在流体/熔体之间分异的结果，而很可能与伟晶岩岩浆形成之前某些过程密切相关，S型花岗岩岩浆在液相线以上存在硅酸盐熔体与高盐熔体的不混溶液相分离有可能是过铝质岩浆体系产生稀土"四重效应"的主要原因。
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The lithologies of the Al rich rocks under ultra high pressure metamorphism in central China are characterized by kyanite topaz quartzite which has special mineral associations of kyanite, rich topaz,Mg rich chloritoid,coesite and diaspore.
我国中部在超高压条件下形成的高铝质变质岩石，以蓝晶黄玉石英岩为特征，具有以蓝晶石、富水黄玉、富镁硬绿泥石、柯石英、硬水铝石等为代表的高压－超高压变质矿物，矿物组合主要为蓝晶石＋黄玉＋石英、蓝晶石＋蓝刚玉±富镁硬绿泥石等。
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In contrast, the ε(322 Ma) values of five woiframite separates from the topaz-quartz vein ores range from -4.16 to -8.05, much lower than values of the greisen massive ore.
云英岩型钨矿石的形成作用与亏损地幔源岩浆活动有关，而黄玉－石英脉型钨矿石则很可能是壳源岩浆活动的产物。
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The WO3 content of the W-bearing topaz-quartz veins and that of greisen blocks range from 1.23% to 1.86%(1.55% on average) and 0.26% to 0.54%(0.40% on average) respectively.
研究表明，红尖兵山钨矿床的矿化类型大体可划分为云英岩型和黄玉－石英脉型。
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The associated minerals are topaz, lazulite, gorceixite, pyrophyllite, rutile etc. which constitute a suit of mineral assemblage of muddy or muddysandy muscovite schist in high pressure metamorphic belt.
与蓝晶石共生的黄玉、天蓝石、磷钙铝石、叶腊石、金红石等矿物构成高压变质带里原岩为泥质、泥砂质的白片岩或类白片岩的一套矿物组合。
- 更多网络解释与黄玉岩相关的网络解释 [注：此内容来源于网络，仅供参考]
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Stilbite - Maharashtra State, India：辉沸石(岩
93. Stibnite - China辉锑矿(岩55) | 94. Stilbite - Maharashtra State, India 辉沸石(岩179) | 95. Topaz - Thomas Range, Utah, USA黄玉(岩135)
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Vanadinite, Morocco：钒铅矿(岩
97. Topaz - Pakistan黄玉(岩135) | 98. Vanadinite, Morocco钒铅矿(岩131) | 99. Variscite - Utah, USA磷铝石(岩125)
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lamprophyric texture：黄玉 topaz 煌斑结构
黄土塬 loass yuan | 黄玉 topaz 煌斑结构 lamprophyric texture | 煌斑岩 lamprophyre
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rutile plagiaplite：金红斜长细晶岩
金红鈦铁岩 urbainite | 金红斜长细晶岩 rutile plagiaplite | 金黄玉 gold topaz
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topazfels：黄英岩
黄英岩 topaz rock | 黄英岩 topazfels | 黄玉岩,黄英岩 topazite
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topazfels; toprzoseme：黄英岩
黄玉;黄精 topaz | 黄英岩 topazfels; toprzoseme | 黄英岩 topazite; topaz rock
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topazite：黄玉岩
topaz 黄玉 | topazite 黄玉岩 | topazization 黄玉化
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topazite：黄英岩
黄英岩 topazfels | 黄英岩 topazite | 黄玉化作用 topazization
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topazite：黄玉岩,黄英岩
黄英岩 topazfels | 黄玉岩,黄英岩 topazite | 黄玉化作用 topazization
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topazite; topaz rock：黄英岩
黄英岩 topazfels; toprzoseme | 黄英岩 topazite; topaz rock | 黄玉化(作用) topazization