助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   low angle normal fault 的翻译结果: 查询用时:0.154秒
图标索引 在分类学科中查询
所有学科
地质学
更多类别查询

图标索引 历史查询
 

low angle normal fault
相关语句
  低角度正断层
     and 4, low angle normal fault or detachment fault.
     4.低角度正断层或滑脱断层。
短句来源
  相似匹配句对
     angle.
     角。
短句来源
     Low and N.
     Low和N .
短句来源
     ORIGIN OF LOW-ANGLE NORMAL FAULTS
     低角度正断层的形成模式
短句来源
     Analysis of and Research on Radar's Low Angle Tracking
     雷达低角跟踪分析与探讨
短句来源
     Low Angle Tracking Techniques for WYCK System
     WYCK统一测控系统的低仰角跟踪技术
短句来源
查询“low angle normal fault”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  low angle normal fault
Nevertheless, the mechanisms by which friction might be effectively reduced on low-angle normal fault surfaces are not understood.
      
In this regard, it is the first large historical earthquake for which slip on a low-angle normal fault has been documented.
      
A low-angle normal fault emerges along the northern flank of Moresby Seamount, a continental crustal block with greenschist metamorphic basement.
      


Based on geometric and kinematic characteristics the normal faults in East China can be grouped into four kinds.1,non-rotational planar normal tault;2, rotational planar normal fault; 3, listric normal fault; and 4, low angle normal fault or detachment fault. They control the configuration, size, sedimentation, and deformation of the basin and so the formation of oil traps. Through analyses of the normal faults. We come to the conclusion that the basins in East China were resulted from the...

Based on geometric and kinematic characteristics the normal faults in East China can be grouped into four kinds.1,non-rotational planar normal tault;2, rotational planar normal fault; 3, listric normal fault; and 4, low angle normal fault or detachment fault. They control the configuration, size, sedimentation, and deformation of the basin and so the formation of oil traps. Through analyses of the normal faults. We come to the conclusion that the basins in East China were resulted from the normal faulting process in zones suffered extension and thining of the earth crust.

中国东部拉张区变形期间发育的正断层,按其几何形态和运动学特征的差异,可确定为四种类型:1.非旋转平面状正断层;2.旋转平面状正断层;3.犁状正断层;4.低角度正断层或滑脱断层。它们及其组合控制着沉积盆地的外部轮廓、规模大小、沉积建造类型和内部变形以及油气构造的形成。本文综合分析了各类正断层特征及其演化过程,认为不同层次、不同尺度和不同类型正断层的发育过程,也是中国东部地壳拉伸变薄及沉积盆地的形成过程。

A neo tectonic fault zone was discovered at Taihelingkou village of Daixian county,Shanxi province The main fault was developed between the bedrock and the Quaternary system,and the dip angle of fault plane shows a characteristic of the upper steep and the lower gentle On the downthrown side of the normal fault,there appears some reversely dragged anticline and normal fault.It indicates that the horizontal displacement and velocity of the fault...

A neo tectonic fault zone was discovered at Taihelingkou village of Daixian county,Shanxi province The main fault was developed between the bedrock and the Quaternary system,and the dip angle of fault plane shows a characteristic of the upper steep and the lower gentle On the downthrown side of the normal fault,there appears some reversely dragged anticline and normal fault.It indicates that the horizontal displacement and velocity of the fault may be greater than those of the vertical displacement.Therefore,it is a low angle normal fault possessing listric character and was formed in the course of rift extending

本文以山西省汾西矿区崔家沟井田断层构造的展布规律、断层面构造岩特征及断层滑动擦痕为依据,分析断层发育的力学机制及成生序次,应用赤平投影图解矿区两条主干断层,得出矿区三向主地应力轴方向的认识,提出一种在华北地区有代表性的煤矿区断层构造展布模式。这对断层的识别和预测具有指导意义。

This paper divided structural elements of the compressional and extensional system in the Yunmenshan Mountain into five parts,namely the Sihetang nappe,the Dashuiyu ductile shear zone,the Yunmengshan antiform,the Qifengcha deachment zone and the Hefangkou low angle normal fault,and gave a description of geological features of this compressional and extensional system.Rock fabric studies were carried out by X ray diffraction method for layered deformation structures of rocks of different...

This paper divided structural elements of the compressional and extensional system in the Yunmenshan Mountain into five parts,namely the Sihetang nappe,the Dashuiyu ductile shear zone,the Yunmengshan antiform,the Qifengcha deachment zone and the Hefangkou low angle normal fault,and gave a description of geological features of this compressional and extensional system.Rock fabric studies were carried out by X ray diffraction method for layered deformation structures of rocks of different ages in Yunmengshan mountain area.Mechanical properties and major stress orientations during the ductifle brittle deformation were determined.Kinematic and dynamic analysis on the formation and evolution of the deformation structures in the compressional and extensional system of the Yunmengshan Mountain was also made.

本文将云蒙山地区挤压 伸展体系的构造要素划分为 :①四合堂推覆体 ;②大水峪韧性剪切带 ;③云蒙山背形构造 ;④崎峰茶滑脱带 ;⑤河防口低角正断层 ;并简述了它们的地质特征。采用X射线衍射法对云蒙山花岗岩及周围不同时代岩石的不同层次变形构造开展了岩石组构特征研究 ,确定了韧 脆性构造变形时的力学性质和主应力方位 ,对挤压 伸展体系变形构造的形成演化进行了运动学和动力学分析。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关low angle normal fault的内容
在知识搜索中查有关low angle normal fault的内容
在数字搜索中查有关low angle normal fault的内容
在概念知识元中查有关low angle normal fault的内容
在学术趋势中查有关low angle normal fault的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社