摘要
青金石结构有无序和有序之别。无序青金石为光性均质体 ,但它的有序化及由此引起的结构调制 ,则有可能使青金石产生光性异常。使结构仍保持立方对称的有序化并不改变它光性上的均质性 ,而其他形式的有序化以及结构调制 ,如果它们是多方向的且在空间取向上具有立方对称的特征 ,则晶体仍是光性均质体 ,否则便转变为光性非均质体。此外 ,还提出了根据选区电子衍射花样对结构调制方向进行三维判识的可能性 ;报道了在所研究青金石中发现的沿 [110 ]方向n=4的有公度调制的有序结构 ,以及所观察到的其他有序结构和无公度调制结构。
In general, lazurites are sweepingly described as symmetrically cubic and optically isotropic. It was observed that, however, some lazurites are of optical anomaly, i.e. they are optically anisotropic. By means of the TEM investigation on lazurite from Baikal, Russia, a diversified variance in lazurite structure is observed, and combining with these diversified structures, the cause of optical anomaly of lazurite is discussed in this paper as follows: (1) The disordered structure of lazurite has a space group of P 4 3n, and consequently it is optically isotropic; (2) The structural ordering, which results from that the centers and corners of cubic cells of lazurite are orderly occupied by two different clusters respectively, would lead to an ordered superstrcture. The latter keeps cubic symmetry (but space group becomes P 23) and original cell size. Therefore it is still optically isotropic; (3) In the lazurite studied, the authors discoveried an ordered superstructure which is one dimentionally commensurate modulated along [110] direction with a repeated period of 4d 110 . This kind of structural modulation makes crystal to become optically anisotropic, because its symmetry is non cubic; (4) In lazurite the structural modulation resulting from partial ordering is usually incommensurate. It takes place frequently along one or several directions of <110>, <100> and/or <112>etc. Such modulated structure is also generally symmetrically non cubic and optically anisotropic; (5) However, whether the modulation is commensurate or incommensurate, the structure will be symmetrically modulated cubic and optically isotropic if the modulation concurred along all the symmetrically equivalent directions. Based on a way proposed by the present authors, the existence of such modulated cubic structure in the lazurite studied has been confirmed.
出处
《高校地质学报》
CAS
CSCD
2000年第2期132-136,共5页
Geological Journal of China Universities
基金
国家自然科学基金资助项目!(495 72 0 90 )
关键词
青金石
有序化
结构调制
光性异常
方钠石族矿物
lazurite
ordering
structural modulation
optical anomaly
sodalite group minerals
