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1)  phyllite [英]['filait]  [美]['fɪl,aɪt]
千枚岩
1.
Similar Simulation on Support Structure of Stope in Phyllite Ground
千枚岩采场支护结构相似模拟试验研究
2.
Rapid construction of horniness phyllite area in Baojia hill tunnel
包家山隧道硬质千枚岩段快速施工技术
3.
The ratio of SiO 2/ (Al 2O 3+Fe 2O 3) is 2 2~2 6 (type Ⅰ ) or 2 8~3 2 (type Ⅱ ) and the ratio of SiO 2/Al 2O 3 is 3 2~3 7 (type Ⅰ ) or 3 9~4 3 (type Ⅱ ) in Changjiang argillic phyllite, Hainan The contents of negative compositions are 0 52%~0 98% for MgO, 3 11~3 59% for (K 2O+Na 2O), 0 017%~0 036% for SO 3, 0 0029%~0 0039% for Cl - All the above parameters are confored the demands of quality.
海南昌江粘土质千枚岩矿的硅酸率(SiO2/(Al2O3+Fe2O3))为:Ⅰ类矿石22~26,Ⅱ类矿石28~32;硅铝比SiO2/Al2O3为:Ⅰ类矿石32~37,Ⅱ类矿石39~43。
2)  phyllitization
千枚岩化
3)  phyllite section
千枚岩地段
4)  phyllitic slate
千枚状板岩
1.
On the basis of field survey of phyllitic slate along passenger dedicated line,through the experimental study,the engineering characteristics of the phyllitic slate which is used for filling subgrade,including the structural characteristics,physical and chemical properties,and hydrological properties are analyzed.
针对客运铁路专线沿线遇到的大量软质千枚状板岩,通过室内试验研究,得出试验成果,并分析了作为路基填料的软质千枚状板岩的工程特性,包括结构特征、物理化学性质、水理性质等。
2.
In view of the fact that large amounts of phyllitic slate are found along the Wu-Guang Railway Line,a lot of interior experiments and studies are made on the structural characteristics of the phyllitic slate used as subgrade filling materials,such as the grain composition and crushing characteristics.
针对武广客运专线沿线遇到的大量软质千枚状板岩,对作为路基填料的软质千枚状板岩的结构特征,包括颗粒组成和破碎特征进行室内实验研究,重点分析千枚状板岩的击实工程特性,包括击实特性、抗剪强度、回弹模量、CBR值、渗水特性、压缩特性等。
3.
In order to study the main influence factors of the CBR value and CBR characteristics of phyllitic slate,the CBR tests of the subgrade with materials of weathered soft-rock from the Wu-Guang Railroad Passenger Dedicated Line were done.
为了研究千枚状板岩CBR值的特征和影响CBR值的主要因素,结合武广客运专线的工程实际,对沿线的千枚状板岩进行了室内CBR值试验。
5)  feldspar phyllite
长石千枚岩
6)  phyllite aggregate
千枚岩骨料
补充资料:千枚岩
千枚岩
phyllite

   一种细粒显微晶质的浅变质岩石。原岩多为泥质、粉砂质岩和中酸性火山岩。属低级区域变质产物,但变质程度较板岩稍高。重结晶作用明显。呈细粒状或鳞片状变晶结构,绢丝光泽。其典型的矿物组合为绢云母-绿泥石-石英,亦可见少量长石、磁铁矿和碳质、铁质物。岩石类型有石英千枚岩、绢云千枚岩、绿泥千枚岩、银灰色千枚岩、黄绿色千枚岩等。千枚岩与板岩、片岩常常共存在一个变质岩系中,分布广泛。如中国南方中晚元古代的昆阳群、双桥山群中都有大量分布。
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