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千枚岩的英文

音标:[ qiānméiyán ]  发音:  
"千枚岩"怎么读用"千枚岩"造句

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  • phyllite

例句与用法

  • The wall is, also here, commonly talcose, and the beds of phyllite are cut and dragged by the movements .
    墙壁,这里也是,一般是滑石化的,千枚岩层被运动所切割、拖曳。
  • Development research on application of phyllite powder used as filler in rubber
    千枚岩粉体橡胶填料开发研究
  • Brown spar phyllite
    褐菱晶千枚岩
  • Recovery and utilization of sericite from tailings of phyllite type gold ores
    千枚岩型金属矿山尾矿中浮选回收绢云母的应用研究
  • ( 4 ) the collapse often involves with the fault and the phyllite . fault ' s strength parameter is very low , and the phyllite is liable soften to the water
    断层破碎带岩体力学性能极差,千枚岩遇水易软化,这些地段发生的塌方往往是支护不及时或支护不力造成的。
  • ( 2 ) taking the geology analysis as main way and combining the pre - test , predicating the tunnel ' s main geology condition ( rock quality , surrounding rock classification , long - wide joint , fault , ground water , crustal stress ) , and predicating the main potential disaster ( collapse , breaking water , rockburst , large deformation ) ( 3 ) employing the stress test result and inverse analysis of the stress field , finding out the crustal stress " s distributing rule along the tunnel axes section : the highest crustal stress is 24mpa near the deepest spot , and predicting that the k2 + 260 ~ k3 + 000 likely to be the high crustal stress segment for this tunnel
    通过地质分析、类比分析、监控量测、数值模拟、神经网络等方法,对鹧鸪山隧道潜在的主要地质灾害(塌方、涌水、岩爆和大变形)进行了预测预报( 3 )在现场地应力测试成果的基础上,运用数值计算进行应力场反演,基本查明了沿隧道轴线剖面的地应力分布规律:地应力量级在最大埋深附近达到最大值24mpa ,并预测k2 + 260 k3 + 000段将很可能成为鹧鸪山隧道的高地应力段。 ( 4 )塌方往往与断层破碎带及千枚岩相联系。
  • The fluids upwelled to seafloor along fault thus ore - forming metals accumulated . 2 . this paper indicated the definition the hydrothermal sedimentary rocks . the definition is a group of especial sedimentary rocks forming at the temperature ranging from 70 ? to 350 ? ( or more high ) through sedimentation and synsedimentary metasomatism in the seafloor
    区内的热水沉积岩主要有硅质岩、钠钾长石岩、重晶石岩、透闪石岩、碳酸盐岩、绿泥石岩和铁白云石斑点千枚岩,它们往往与热水沉积矿体紧密伴生。
用"千枚岩"造句  

其他语种

百科解释

千枚岩是一种浅变质的岩石,是泥质、粉沙质或中酸性凝灰岩等岩石经过区域变质作用而形成的,一般颜色较浅,为黄色、绿色、褐色或灰色,经过变质作用后,原岩中的物质也大部分重结晶,生成石英、绢云母、绿泥石等。
详细百科解释
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