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斑岩的的英文

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"斑岩的"怎么读用"斑岩的"造句

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  • porphyritic

例句与用法

  • The copper is disseminated in small joint surfaces and cracks in the porphyries .
    铜浸染在斑岩的细小节理面和裂隙中。
  • ? norwinks the gold fin in the porphyryfont ?
    斑岩的泉水中金鳍也不再闪动
  • The granite and porphyry monuments of egypt exert an incredible sway over our feelings
    埃及的花岗岩和斑岩的纪念碑在我们的感觉上发挥了一种难以置信的影响。
  • How little attention is paid to this in our time is shown by certain extravagances of the large granite and porphyry manufactures in sweden and russia
    但现在还很少注意到这点,这从瑞典和俄国某些对大块花岗石和斑岩的制造的奢侈可以看出。
  • Their massive vaults , carried at both levels by monolithic columns of green and white marble and purple porphyry , serve as buttresses to receive the thrust of the great dome and its supporting arches
    它们大块的拱顶,都擒带着同样等级的绿色和白色大理石和紫色斑岩的大块圆柱,作为支撑之用,受到了巨大的圆屋顶和它的支撑拱门的插入。
  • 2 . 38 . 6ma and 36 . 7ma isotopic ages of quartz - monzonite - porphyry in lianhuashan and alkaline porphyry in zhuopan have respectively been obtained . those results are consistent with the ages of the porphyries in both lanping - shimao basin and changdu basin related igneous rocks , representing the first episode ( lanping movement ) of tectonics - magmatism - metallogenic event during the himalayan movement
    获得了莲花山石英二长斑岩及卓潘碱性斑岩的ar - ar年龄,分别为38 . 6ma与36 . 7ma ,与整个兰坪?思茅盆地与昌都盆地及两侧的斑岩与相关火山岩一致,代表喜马拉雅运动第一幕(兰坪运动)的重要构造?岩浆?成矿事件。
  • It is difficult to conform the derivations of the native heavy minerals , so the author assumes corresponding procedures as follows to accomplish the research task : firstly , according to the composition typomorphic peculiarities of minerals deriving from mantle , the author selected a part of minerals as preliminary reseach objects from the native heavy minerals and then further investigate the mantle ones and their host rocks in two ways : one is the method of comparation with the corresponding minerals of rocks deriving mantle in the research field and other places ; anorther is the method of multivariate statistical analysis
    本次工作为了尽可能地排除非幔源矿物的干扰,根据陈光远( 1990 ) 、潘兆橹( 1994 )等学者有关矿物成分标型的论断,筛选出地幔特征元素含量较高的重砂矿物做为初步研究对象,为达到研究目的采取了如下方法:与区内已发现的幔源岩石(如钾镁煌斑岩等) 、国内外有代表性的碱性玄武岩、金伯利岩、钾镁煌斑岩的深源包体中的相应矿物进行对比研究的方法;多元统计分类的方法。
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