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
   韧性推覆构造 的翻译结果: 查询用时:0.258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
 

韧性推覆构造
相关语句
  tenacity nappe tectonics
     Nappe tectonics was classified into three types thrust nappe tectonics, slipping tectonics (stretch nappe tectonics) and tenacity nappe tectonics.
     依据推覆构造形成的力学机制,将推覆构造分为边冲推覆构造、滑覆构造和韧性推覆构造三大类型。
短句来源
     By comprehensive study, Wudang Mountain tenacity nappe tectonics has been pointed out at the first time. Its geometrical pattern is a giant "AB"type of fold.
     通过对武当山地区的综合研究,提出武当山地区为一韧性推覆构造,其几何样式为一个巨型的“AB”型褶皱。
短句来源
  ductile nappe structure
     BASIC CHARACTERISTIC OF DUCTILE NAPPE STRUCTURE AND ITS ORE-CONTRAL OF GOLD DEPOSIT IN NORTH ANKANG
     安康地区北部韧性推覆构造基本特征及对金矿成矿控制作用
短句来源
  “韧性推覆构造”译为未确定词的双语例句
     STUDY OF THE EASTERN QINLING SHEAR OROGENIC BELT──Based on the Wudang Mountain nappe
     论东秦岭剪切造山带──以武当山韧性推覆构造为例
短句来源
  相似匹配句对
     THE CHAOHU NAPPE STRUCTURE
     巢湖推覆构造
短句来源
     NAPPE TECTONICS IN ANHUI
     安徽的推覆构造
短句来源
     DUCTILE SHEAR ZONES AND NAPPE-GLEDENG STRUCTURE IN ALTAY, XINJIANG
     阿尔泰地区韧性剪切带和推覆-滑脱构造
短句来源
     “L-STRUCTURE”FOR FUZZY SET IN A LINEAR SPACE
     L—构造
短句来源
     BRITTLE-DUCTILE THRUST NAPPES ON THE SOUTH SLOPE OF TONGBAI MOUNTAINS
     桐柏山南坡的脆-韧性逆冲推覆构造
短句来源
查询“韧性推覆构造”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
没有找到相关例句


Nappe tectonics was classified into three types thrust nappe tectonics, slipping tectonics (stretch nappe tectonics) and tenacity nappe tectonics. By comprehensive study, Wudang Mountain tenacity nappe tectonics has been pointed out at the first time. Its geometrical pattern is a giant "AB"type of fold. It was proved by many means,that mechanism of deformation in Wudang Mountains area is simple shear. The whole Eastern Qinling orogenic belt is a shear orogenic belt. The concept,characteristics and important...

Nappe tectonics was classified into three types thrust nappe tectonics, slipping tectonics (stretch nappe tectonics) and tenacity nappe tectonics. By comprehensive study, Wudang Mountain tenacity nappe tectonics has been pointed out at the first time. Its geometrical pattern is a giant "AB"type of fold. It was proved by many means,that mechanism of deformation in Wudang Mountains area is simple shear. The whole Eastern Qinling orogenic belt is a shear orogenic belt. The concept,characteristics and important significance of shear orogenic belt have been discussed in the article.

依据推覆构造形成的力学机制,将推覆构造分为边冲推覆构造、滑覆构造和韧性推覆构造三大类型。通过对武当山地区的综合研究,提出武当山地区为一韧性推覆构造,其几何样式为一个巨型的“AB”型褶皱。并证实武当山地区为剪切变形区,其变形机制为简单剪切机制。文章还提出整个东秦岭造山带为剪切型造山带。

In this paper, the geological characterstic and the evoluation of the duetile nappe structure is mainy discussed in north Ankang,and its ore-contual of gold deposlt is also expounded from four respects. Huanglong gold deposit and Maoyiazi gold deposit are to be thought as ductile nappe-sheare belt-type deposit. In addition, the prospecting scope for searching gold deposit is discussed.

本文着重介绍了陕西安康地区北部韧性推覆构造的地质特征及其演化,从4个方面扼要论述了它对该区金矿的控制作用,并明确指出茅垭子、黄龙金矿等属韧性推覆剪切带型矿床,在此基础上指出了安康地区北部今后金的找矿方向。

The Erlangping back arc basin was an important part of the North Qinling active continental margin in early Palaeozoic Era The Erlangping Group is the remains of back arc basin,and records its evolution Analysis of the sedimentary textures demonstrated that the Southern and Northern clastic sedimentary rocks were formed in different active continental margin Besides,there are two series of subdutional granites which distributing along the two ...

The Erlangping back arc basin was an important part of the North Qinling active continental margin in early Palaeozoic Era The Erlangping Group is the remains of back arc basin,and records its evolution Analysis of the sedimentary textures demonstrated that the Southern and Northern clastic sedimentary rocks were formed in different active continental margin Besides,there are two series of subdutional granites which distributing along the two boundaries of Erlangping back arc basin Tectonicly,the main orogenic period of deformation can be devided into an early stage and a late stage Two sets of thrust ductile deformation were formed in early stage while the complex tight folds were formed in late stage The characteristics of sedimentation,magmatism and deformation all indicate that this back arc basin is characterized by bidirectional subduction during late Palaeozoic Era,i e ,a subduction downward to the Kuanping ancient continent,and another downward to the Qinling ancient island arc

二郎坪弧后盆地是北秦岭早古生代活动大陆边缘沟-弧-盆系统的重要组成部分,现今二郎坪岩群是古弧后盆地的物质残存,记录了盆地演化方式和过程。沉积建造和岩浆作用研究发现,在二郎坪弧后盆地南北两侧各发育一套活动型陆缘沉积体系和一系列府冲型花岗岩;变形构造解析反映出主造山期早期沿弧后盆地两侧各形成一套韧性推覆构造系,并具对冲型几何学样式,为俯冲带典型构造。综合分析表明,弧后盆地在造山早期分别俯冲于南部秦岭古岛弧和北部宽坪古陆之下,具双向式俯冲特征。

 
<< 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韧性推覆构造的内容
在知识搜索中查有关韧性推覆构造的内容
在数字搜索中查有关韧性推覆构造的内容
在概念知识元中查有关韧性推覆构造的内容
在学术趋势中查有关韧性推覆构造的内容
 
 

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