钠闪石

  • 网络riebeckite
钠闪石钠闪石
  1. 钠闪石花岗岩的Rb-Sr等时线年龄为125Ma。

    Riebeckite granites emplaced in Jurassic volcanic basin of Da Hinggan Ling and its Rb Sr isochron age is 125 Ma .

  2. 沉积岩中镁钠闪石石棉矿物的初步研究

    Magnesian riebeckite asbestus from sedimentary rocks & a preliminary study

  3. 因52个样品中,也包含钠钙闪石亚族,故对整个闪石族用X射线衍射估算阳离子占位的问题已基本解决。

    As Na-Ca sub-amphiboles appeared among the52 samples , the method of estimating canon occupancied by X-ray diffraction is suitable to all amphiboles .

  4. 利用岩石薄片X衍射技术,在松辽盆地深层富碱酸性火山岩中识别出特征的碱性暗色矿物&钠铁闪石,从而确定其为碱流岩。

    Using thin section X-ray diffraction techniques , his paper identified arfvedsonite in volcanic rocks from Songliao Basin , and thus confirmed that the volcanic rocks are composed of pantellerite .

  5. 碱性花岗岩类,包括钠铁闪石花岗岩以及孪生的钾长花岗岩类;

    The alkaline granitoid including arfvedsonite granite and assemblage moyite ;

  6. 罕见的蓝色钾钠透闪石研究

    Study on a Rare Mineral : Blue K-Na Richterite

  7. 拉斑玄武岩质粒玄岩依兰地区黑龙江增生杂岩碱性玄武质火山碎屑岩中钠质闪石特征及成因探讨

    Characteristics and genesis of sodium amphiboles in alkaline basaltic pyroclastic debris of Heilongjiang accretionary complexes in Yilan area

  8. 本文还从霓石、钠铁闪石的结构、生长条件方面的差异对其形貌差异进行了对比分析。

    Through the analysis of the difference in structure and growth condition between aegirine and arfvedsonite , the differ-ence in morphology and surface microtopography between these two minerals has also been ana-lysed .

  9. 具交代结构的翡翠中常因含有钠质闪石、钠长石或绿泥石,且使翡翠的粒度不均匀而使其质量变差;

    The jadeite 's quality with the micro-crystalloblastic fiber texture is high , whereas that with the metasomatic texture is poor because there are sodium amphibole , albite or chlorite in it .

  10. 黑龙江涌泉地区变质基性火山岩中钠质角闪石的成因及演化

    Origin and evolution of sodium amphibolite in metamorphic basic volcanic rocks from Yongquan area of Heilongjiang

  11. 这些基性火山岩至少发生了两期高压变质,两期高压变质形成的钠质角闪石具有不同成因。

    These basic volcanic rocks underwent high pressure metamorphism for two times , at least , in which sodium amphibolites are formed by high pressure metamorphism with different genesis .