柱晶組 的英文怎麼說

中文拼音 [zhùjīng]
柱晶組 英文
prismatic class
  • : Ⅰ形容詞(光亮) brilliant; glittering Ⅱ名詞1. (水晶) quartz; (rock) crystal 2. (晶體) any crystalline substance
  • : Ⅰ名詞1 (由不多的人員組成的單位) group 2 (姓氏) a surname Ⅱ動詞(組織) organize; form Ⅲ量詞(...
  1. High - mg volcanic rocks approach the primitive mantle compositions, and their magmatic source is close to the composition of bse, derives from the lower mantle and formed by this type - mantle rocks " fractional melting highly ( > 25 % ). high - mg volcanic magma, formed in the axis of the emei mantle plume, underwent the crystallization differentiation of olivines and some pyroxenes ; some olivines reflect fair cumulus crystallization

    高鎂火山巖接近於原始巖漿的成,巖漿源區與地球平均成分bse的成分特徵相近,起源深度為下地幔,為該地幔巖較高程度的部分熔融( 25 )而形成的。高鎂火山巖處于地幔的軸部,經歷了橄欖石及一定程度的輝石分異結,並且橄欖石顯示出一定的堆作用。
  2. Abstract : the crystal structures obtained by static solidification and vibration solidification were compared. it was showed that, in the case of vibration solidification, the orientation growth of the columnar crystal was not obvious, the equiaxial crystal appeared more early. the grains of both types of crystals were quite fine, hardness in the full section was relatively high, and the hardness distribution was uniform. in the former case, the solute segregation in dendritical austenite more severe, and there were lumps of distortion inclusion

    文摘:對球鐵金屬型靜凝固與振動凝固的結織對比表明:後者方向性生長較弱,等軸出現較早,且兩者的粒均較細,全斷面硬度較高且分佈均勻;前者枝奧氏體內溶質偏析大,有畸變夾雜團塊。
  3. A ree partition simulation suggests that the tianzhushan intermediate rocks can be generated by partial melting, in coupling with fractional crystallization, of dioritic gneiss which is similar in chemical compositions to the mafic rocks in the lower crust in north dabie ; partial melting of intermediate grey gneiss which is similar in chemical compositions to the middle crust in north dabie can generate the tianzhushan felsic rocks

    Ree配分的定量模擬計算結果表明,與基性下地殼相似的北大別基性閃長質片麻巖部分熔融並經過結分異能夠形成與天山中性巖類似的稀土元素成,而與中性地殼相似的北大別中性灰色片麻巖部分熔融能夠形成與天山花崗巖類似的稀土元素成。
  4. Ree partition simulation suggests that the tianzhushan intermediate rocks can be generated by partial melting, in coupling with fractional crystallization, of dioritic gneiss which is similar in chemical compositions to the mafic rocks in the lower crust in north dabie ; partial melting of intermediate grey gneiss which is similar in chemical compositions to the middle crust in north dabie can generate the tianzhushan felsic rocks

    Ree配分的定量模擬計算結果表明,與基性下地殼相似的北大別基性閃長質片麻巖部分熔融並經過結分異能夠形成與天山中性巖類似的稀土元素成,而與中性地殼相似的北大別中性灰色片麻巖部分熔融能夠形成與天山花崗巖類似的稀土元素成。
  5. 3. for the component of sub - eutectic, the cu - cr alloys are difficult to form complete eutectic tissue on the condition of non - equilibrium solidification. the general microstructure is of cellular primary a ( cu ) and circumference - distributed eutectic ( a + p ) where the former mainly acts as the conductor and the latter as the reinforce, together to be fibrous eutectic reinforced in - situ composites

    3在非平衡凝固條件下,亞共cu - cr合金凝固織的一般特徵為狀的初生之間分佈著條狀的cu - cr共體,前者主要起導電作用,後者作為強化相,形成共纖維強化的自生復合材料。
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