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synthetic forsterite
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  “synthetic forsterite”译为未确定词的双语例句
     The unit cell parameters of the forsterite in the study area are the same as those of the synthetic forsterite.
     测试出的晶胞参数与人工合成镁橄榄石的一致。
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  相似匹配句对
     Synthetic product T.
     作者将合成的T.
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     Synthetic of SAP
     高吸水树脂SAP的合成
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     The unit cell parameters of the forsterite in the study area are the same as those of the synthetic forsterite.
     测试出的晶胞参数与人工合成镁橄榄石的一致。
短句来源
     Development of forsterite refractorier
     镁橄揽石耐火材料的发展
短句来源
     Investigation on tunable forsterite laser
     镁橄榄石可调谐激光的研究
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  synthetic forsterite
The results of studying the structure of the paramagnetic centers formed by impurity Ho3+ ions in synthetic forsterite (Mg2SiO4), obtained by the method of tunable high-frequency EPR spectroscopy, are reported.
      
The CL spectrum of the grain-boundary silicate was found to differ from that of pure synthetic forsterite suggesting the presence of modifiers.
      
Solubility and partitioning of water in synthetic forsterite and enstatite in the system MgO-SiO2-H2O±Al2O3
      
The solubility of hydrogen in Mg-Fe olivines as a function of temperature and iron concentration was investigated by hydrothermally annealing single crystals of synthetic forsterite and San Carlos olivine.
      
The effect of silica activity on the incorporation mechanisms of water in synthetic forsterite: a polarised infrared spectroscop
      
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The forsterite mineral inclusions in chromite of podiform chromitite occur in mantle peridotite of Luobusa ophiolite in the Indo_Yarlung Zangbo tectonic unit. The forsterite inclusions from chromite grains have Fo number of 97~99 and assume the form of colorless, transparent and euhedral grains with abundant small faces. The crystal of forsterite used for X_ray analysis was measured to be approximately 0.15 mm×0.15 mm×0.15 mm. Crystal system of this forsterite is orthorhombic, space group Pbnm , α, β and...

The forsterite mineral inclusions in chromite of podiform chromitite occur in mantle peridotite of Luobusa ophiolite in the Indo_Yarlung Zangbo tectonic unit. The forsterite inclusions from chromite grains have Fo number of 97~99 and assume the form of colorless, transparent and euhedral grains with abundant small faces. The crystal of forsterite used for X_ray analysis was measured to be approximately 0.15 mm×0.15 mm×0.15 mm. Crystal system of this forsterite is orthorhombic, space group Pbnm , α, β and γ is 90°, a =4.7597, b =10.205, c = 5.9831. The unit cell parameters of forsterite, a , b , c as well as M1—O and M2—O bond lengths are smaller than those of some olivines from mantle xenolith and mantle peridotites. The unit cell parameters of the forsterite in the study area are the same as those of the synthetic forsterite. According to experimental study cited in the literature, the small unit cell andcation_oxygen bond distances of olivine suggest a high pressure of its crystallization.

在西藏罗布莎蛇绿岩块的豆荚状铬铁矿中 ,存在包裹体矿物镁橄榄石。这些镁橄榄石为无色透明多晶面组成的自形晶 ,Fo值可达到 97~ 98,具富镁端员组分。选取一代表性颗粒的单晶进行X单晶衍射分析 ,表明其为斜方晶系 ,空间群Pbnm ,镁橄榄石晶胞参数a、b、c以及M 1— 0和M 2— 0键长均小于地幔包裹体和一般地幔岩中橄榄石的对应值。测试出的晶胞参数与人工合成镁橄榄石的一致。镁橄榄石具有橄榄石族中已知最小的晶胞参数 ,据此推断它是在超高压环境下结晶的

 
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