顽火辉石

wán huǒ huī shí
  • enstatite
顽火辉石顽火辉石
顽火辉石[wán huǒ huī shí]
  1. 绢石与顽火辉石光性方位的关系

    A relationship optic orientation between bastite and enstatite

  2. 800℃时,1060cm~(-1)新带的出现标志着顽火辉石的生成。

    At800 ℃, a new band appears at 1060 cm ~ ( - 1 ), indicating the formation of enstatite .

  3. 顽火辉石(Mg(0.92),Fe(0.08))SiO3的冲击相变和高压状态方程及其地球物理意义

    Equation of State and Phase Transition of ( Mg_ ( 0.92 ), Fe_ ( 0.08 )) SiO_3 Enstatite under Shock Compression and Its Geophysical Implications

  4. 冲击压缩下钙钛矿顽火辉石的Grüneisen参数、冲击波温度及相稳定性研究

    Study on Gr ü neisen Parameter , Shock Temperatures and Phase Stability of Shock-compressed Perovskite Enstatite

  5. 根据地球化学热力学原理,组成矿床的主要成分SiO2和MgO,主要来自硅镁质石陨石的镁橄榄石和顽火辉石。

    Based on the principle of geochemistry-thermodynamics , the main component , MgO and SiO_2 that form deposit , originate from forsterite and enstatite of the simatic meteorolite .

  6. 下地幔深部压力条件下顽火辉石Perovskite(MgSiO3)的冲击诱导相变

    Shock & induced Transition of Perovskite ( MgSiO_3 ) under the Pressure of the Low Mantle

  7. 顽火辉石的状态方程和高压相的稳定性研究

    Shock Wave Equation of State and the Stability of High-pressure Phase of Enstatite

  8. 800℃时,晶质顽火辉石生成。

    At 800 ℃, crystalline enstatite is formed .

  9. 非理想热力学混合作用对固溶体矿物热容的影响&以斜方顽火辉石-正铁辉石固溶体为例

    Influence of non-ideal thermodynamic mixing on the heat capacities of solid solution minerals as exemplified by orthoenstatite-orthoferrosilite solution

  10. 清镇顽火辉石球粒陨石及我国新近降落的不同类型陨石宇宙成因核的研究

    A study on cosmogenic nuclides in the Qingzhen enstatite chondrite and various types of meteorites falling recently in China

  11. 普通球粒陨石和碳质球粒陨石中的亲石元素在顽火辉石球粒陨石内显示亲铜或亲铁的性质。

    The lithophile elements in ordinary and carbonaceous chondrite groups may display either chalcophile or siderophile nature in enstatite chondrites .

  12. 温度升高到650℃时,镁橄榄石结晶度增高,并出现顽火辉石新物相;

    When the temperature reaches 650 ℃, the crystallinity of forsterite is improved , then another new mineral phase enstatite appears .

  13. 将计算结果与实验数据比较后表明,在相同压力但不同温度的区域,上述两组相态都可能是顽火辉石的高温高压相态。

    When compared with experimental Hugoniots , the calculations demonstrate that the above mentioned two kinds of phase states are indeed possibly the high pressure phases of enstatite when it is compressed to high pressure but to different temperatures .