内蒙地轴

  • 网络Inner Mongolian axis
内蒙地轴内蒙地轴
  1. 内蒙地轴南缘断裂带的活动时代及结构分析

    Ages of activities of the southern " Inner Mongolian axis " marginal fault belt and an analysis of its structure

  2. 晚侏罗世的盆地往北推移,在内蒙地轴南部及东部的E&W向及NE向的山间盆地中,接受了周边山地的物源而形成磨拉石建造;

    The basin was migrated northward in Late Jurassic , and in the piedmont basins with EW and NE directions in the southern and eastern parts of Inner Mongolian Axis , the substance from adjacent mountainous areas was deposited , forming the molasse formation ;

  3. 内蒙地轴南缘盖层中逆冲断层的样式及形成机制

    On styles and mechanism of thrust on the south margin of Inner Mongolia axis

  4. 内蒙地轴基底岩石淋滤试样稀土元素含量特征

    REE contents in leaching from samples of basement rocks in Nei monggol earth 's axis

  5. 内蒙地轴古老基底岩石淋滤试验样品的仪器中子活化分析

    Instrumental neutron activation analysis of leached samples of old basement rocks from the Nei Monggol earth 's axis

  6. 其大地构造位置在华北地台北缘内蒙地轴东部。

    The Honghuagou area of Chifeng City is tectonically located on the northern margin of the Inner Mongolian axis .

  7. 冀北崇礼赤城大断裂的多相逆冲兼论内蒙地轴隆升的构造制约因素

    Multiphase thrusting of the Chongli - Chicheng regional fracture of North Hebei Province and tectonic factors of Inner Mongolian axis upwarping

  8. 近北庄太古代变质铁矿床位于燕山沉降带北侧与内蒙地轴的交接部位。

    The Jinbeizhuang Archean metamorphic iron ore deposit is situated in where the north side of Yanshan settle-zone crosses Inner Mongolia Eath 's Axis .

  9. 凌源-北票断裂是内蒙地轴与燕山台褶带之分界断裂,对辽西大地构造格架和中新生代断陷盆地形成均具有重要作用。

    Lingyuan Beipiao fault zone is an important structural zone , which makes up the boundary of Inner Mongolia geological axis and Yanshan platform folding zone .

  10. 笔者等在华北地台北缘内蒙地轴范围内原太古宙、元古宙地层中发现大量早寒武世小壳化石。

    The author and his colleagues found large amounts of Early Cambrian small shelly fossils in the original Archean and Proterozoic strata within the realm of the " Inner Mongolian axis " on the northern margin of the North China platform .

  11. 晚三叠中侏罗世华北地台早中生代的盆山关系使内蒙地轴的挤压隆升,其南侧的山前盆地挠曲下沉形成含煤建造;

    The basin-mountain relation on North China Platform from Late Triassic to Middle Jurassic is that the Inner Mongolian Axis was compressed and uplifted , while the piedmont basin was flexed and sunk , forming the coal-bearing formation on its southern side ;