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北东东的英文

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"北东东"怎么读用"北东东"造句

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  • east northeast

例句与用法

  • The first belt stretches from qinghe , wenquan to the nw direction and the second extends from nankou , changping to the ene direction
    一条从清河、温泉一带向北西方向伸展,到怀来县以北的黄土窑一带;另一条是自南口、昌平一带向北东东向伸展的活动断裂带。
  • Some controversy has been put on aheqi fault , our data shows it is a ne trending left lateral strike slip fault , but its activity is weak
    阿合奇断裂是一条引起争议的断裂,我们收集的资料表明它是一条走向北东东的左行走滑断裂,但它的活动性不是很强烈。
  • The faults consist of three groups : one is nw direction , others are ne to nee direction and sn direction . the group which is nw direction is the most important one
    断裂构造十分发育,均为正断层,主要有三组,北西向、北东北东东向和南北向,其中以北西向一组最为发育。
  • By analyzing the development characteristics of budate group source faults in beier depression based on seismic data , a lot of source faults are found
    摘要通过地震资料对贝尔凹陷布达特群源断裂发育及其活动特征进行了分析,发现贝尔凹陷布达特群发育有大量北东东和北北东向的源断裂。
  • Multistage structural deformations are experienced in kongquehe area , the basical fault systems of nww - near ew , nne - near sn , nnw and nee are established , the fault movement has the characteristics of multistage and inheritance , in the area multi - structural deformations are experienced in sinian to early ordovician , early ordovician - silurian , jurassic cretaceous - caenozoic , etc . late structural deformation shapes are changed for different levels of formar structural layer , in which different deforming shapes are created and integrated overlying of deformation is induced
    摘要孔雀河地区经历了多期次的构造变形作用,形成了现今北西西近东西向、北北东近南北向、北北西向和北东东向基本断裂体系,同时断裂活动表现为多期性和继承性的特点;该区经历了震旦纪至早奥陶世、早奥陶世末志留纪、侏罗系、白垩纪新生代等多期构造变形作用,且后期的构造变形作用在不同程度上对前期的构造层的变形样式有所改造,形成了有一定差异的变形面貌,造成变形的复合登加。
  • The anatomy of small - scale to meso - scale deformational structures have resulted in the reconstruction of the structural framework of the yanbian group . the statistical analyses of the fold hinge and cleavages developed in the yanbian group suggest the trend of the first stage penetrating structures of the yanbian group is een - wws . 2
    基于对盐边群中、小尺度变形构造进行构造解析,建立了区域构造格架,通过对褶皱枢纽和劈理的分析,提出盐边群第一期透入性变形构造的走向为北东东?南西西向。
  • Tertiary structures are developed in mesozoic - palaeozoic tectonic settings , the general framework is faulted depression faulted in the north and onlapped on the south and arch bounded by faults . they are controlled and affected by three sets of large successive - active faults ( nw , ne and nee strike ) , they are successive and segmented , with multiples types and zoning distribution
    第三系的构造是在中、古生界构造的背景上发育起来的,它以北断南超的箕状断陷和断层为界的凸起为总的构造格架,受北西、北东和北东东向三组继承性活动大断层的控制和影响,构造具有继承性和分割性、类型具有多样性、分布具有分层分带性。
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