- 更多网络例句与晶体发生学相关的网络例句 [注：此内容来源于网络，仅供参考]
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The formation of martensite is accomplished by the immigration of well-defined glissile interface (121)fcc type and its misfit dislocations can produce the lattice invariant deformation on the basis of phenomenal theory of martensitic crystallography, however, LID is retarded slightly after the migration of interphase (121)fcc, i.e.a thin plate-like zone exists without LID in martensite near the well-defined interface. When the temperature reduces to the Ms point, the lattice parameter of austenite matrix is √3/2 times that of the martensite without LID. This critical condition for spontaneous transformation agrees with that the stack fault energy in matrix is less than zero according to Olson and Cohen's nucleation model.
通过模型分析表明：fcc/bcc马氏体形核与长大过程是通过(121)fcc型择优界面推移进行的，界面上的错配位错可以完成马氏体晶体学唯象理论要求的点阵不变变形，但LID要稍滞后于界面迁移，即在马氏体形核与长大过程中推移界面新相一侧存在一未发生LID的新相薄区；当相变温度达到马氏体相变点Ms时，母相奥氏体与这一薄区的晶格常数比为√3/2，这一几何条件和Olson-Cohen形核模型中要求扩展位错层错区界面能γ≤0是等价的。
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Analyses of quenched nm products revealed that the nepheline was completely transformed into NaAlSiO4 with the calcium-ferrite-type structure at 23 GPa and 1500℃ In combination with previous results, the calcium-ferrite-type NaAlSiO4 can exit under the conditions of deep lower mantle and it may be the important host phase for sodium and aluminium in the deep lower mantle. With the change of temperature and pressure, the crystal parameters will change, though the ranges are limited.
结合前人的研究成果可以认为：型NaAlSiO4在地慢深部可以稳定地存在，并对Na、Al在深部的赋存具有重要意义；随着温度压力条件的变化，CaFe2O4型NaAlSiO4的晶体学参数（晶格常数、晶胞体积和计算密度）发生变化，但变化的幅度不大。
- 更多网络解释与晶体发生学相关的网络解释 [注：此内容来源于网络，仅供参考]
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crystallogenesis：晶体发生学,结晶发生学
crystallofluorescence | 晶体荧光 | crystallogenesis | 晶体发生学,结晶发生学 | crystallogeny | 晶体发生学 晶体发生学,结晶发生学
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crystallogeny：晶体发生学
crystallize 结晶 | crystallogeny 晶体发生学 | crystallogram 晶体衍射图
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crystallogeny：晶体发生学 晶体发生学,结晶发生学
crystallogenesis | 晶体发生学,结晶发生学 | crystallogeny | 晶体发生学 晶体发生学,结晶发生学 | crystallogphy | 结晶学, 晶体学