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P21ca斜方辉石相变的研究
A Study on the phase Transition of P21ca Orthopyroxene
【摘要】 笔者利用透射电子显微镜(TEM)和加热台等技术,对河北承德黑山P21ca顽辉石的相变过程进行动态观察,证实了P21ca斜方辉石是Pbca斜方辉石的同质多象低温变体。相变温度在800~900℃之间。这一变相是通过P21ca斜方辉石晶体结构中四分之一呈S旋转的Si—O四面体链改变为O旋转类型而实现的。
【Abstract】 Using transmission electron microscope and heating stage techniques, the authors have studied the phase transition of P21ca enstatite (En56Fs41Wo3). When the sample is heated to 900℃ or so, the diffraction spots of k≠2n in Okl diffraction of P21ca enstatite disappear, forming orthopyroxene with Pbca symmetry. The phase transition from P21ca orthopyroxene to Pbca orthopyroxene is achieved through the change in the rotation type of Si-O tetrahedra chain which is Srotation in the structure of P21ca orthopyroxene. This phase transition experiment demonstrates that P21ca orthopyroxene is the low-temperature polymorph of Pbca orthopyroxene.
【Key words】 P21ca orthopyroxene; Pbca orthopyroxene; phase transition;
- 【文献出处】 岩石矿物学杂志 ,Acta Petrologica Et Mineralogica , 编辑部邮箱 ,1989年02期
- 【被引频次】2
- 【下载频次】27