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
   掩卧 的翻译结果: 查询用时:0.205秒
图标索引 在分类学科中查询
所有学科
更多类别查询

图标索引 历史查询
 

掩卧
相关语句
  parallel lying
     The ductile shear zone, mylonite,layer parallel lying fold and boudinage come out extensively in the third group of Langshan.
     在狼山群第三岩组中发育韧性剪切带、糜棱岩、顺层掩卧褶铍及石香肠构造。
短句来源
  “掩卧”译为未确定词的双语例句
     Its gliding nappe system,which was composed by C-P structure layer,developed gliding tectonics such as synclinorium,bedding rhed fold,penetrative stretching and flow cleavage,etc.
     滑覆系统由C-P构造层组成,发育有复式向斜、顺层掩卧褶皱、透入性拉伸线理和流劈理等滑动构造;
短句来源
  相似匹配句对
     Crouching Tiger,Hidden Dragon
     “虎藏龙”
短句来源
     Crouching Tiger Hidden Dragon
     虎藏龙
短句来源
     The ductile shear zone, mylonite,layer parallel lying fold and boudinage come out extensively in the third group of Langshan.
     在狼山群第三岩组中发育韧性剪切带、糜棱岩、顺层褶铍及石香肠构造。
短句来源
     and E.
     短板耳螽E .
短句来源
     new wine in the old bottle: the renaissance of earth-sheltered buildings
     旧瓶装新酒:浅谈土建筑的复兴
短句来源
查询“掩卧”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


Wangxia gliding nappe structure was formed with the forcing intrusion of Bawan-glin superunit granite in western Hainan. Its gliding nappe system,which was composed by C-P structure layer,developed gliding tectonics such as synclinorium,bedding rhed fold,penetrative stretching and flow cleavage,etc.,The autochthon was O-S structure layer. Wangxia gliding nappe structure was formed in the middle and late period of Indosinia;All gliding nappe system was in extension state in early period,and in pressure state...

Wangxia gliding nappe structure was formed with the forcing intrusion of Bawan-glin superunit granite in western Hainan. Its gliding nappe system,which was composed by C-P structure layer,developed gliding tectonics such as synclinorium,bedding rhed fold,penetrative stretching and flow cleavage,etc.,The autochthon was O-S structure layer. Wangxia gliding nappe structure was formed in the middle and late period of Indosinia;All gliding nappe system was in extension state in early period,and in pressure state in later period. The gliding nappe di-rection of the gliding tectonics was N-S and had been displaced Southward for about 7 km.Strong gold mineralization had occurred in Wangxia and Yalao faults which were in the system of detachment faults.

琼西王下滑覆构造是由坝王岭超单元花岗岩的强力侵位而形成的。滑覆系统由C-P构造层组成,发育有复式向斜、顺层掩卧褶皱、透入性拉伸线理和流劈理等滑动构造;原地系统为O-S构造层。王下滑覆构造形成于印支中、晚期。在早期滑覆系统处于伸展状态,晚期则处于挤压状态,滑覆构造的滑覆方向为N→S,滑覆距离大于7km。在滑脱断层系统内的王下断层及牙劳断层中,均发生了较强的金矿化。

Sandai area in Mianning County lies in the western margin of Yangtze Platform. Sedimentary and voleanic rocks from the Sinian to the Late Permian are exposed in the area. Most of the rocks underwent metamorphism of low greenschist facies and low-and medium-deformation characterized by bedding schistositization, bedding flat-lying folding and ductile shearing with normal stratigraphic sequence. The resulting structures are structural assemblage of the folding layers which occurred in extensional tectonic regime...

Sandai area in Mianning County lies in the western margin of Yangtze Platform. Sedimentary and voleanic rocks from the Sinian to the Late Permian are exposed in the area. Most of the rocks underwent metamorphism of low greenschist facies and low-and medium-deformation characterized by bedding schistositization, bedding flat-lying folding and ductile shearing with normal stratigraphic sequence. The resulting structures are structural assemblage of the folding layers which occurred in extensional tectonic regime during the Late Permian-Triassic Period.

位于扬子地台西缘的冕宁三代地区,出露有震旦纪一晚二叠世的沉积岩及火山岩,岩石普遍遭受了低绿片岩相变质和浅-中构造相变形,尤以顺层片理、顺层掩卧褶皱、顺层韧性剪切带最为发育,地层序列正常。它们是地壳伸展机制下的褶叠层构造组合,它发生于晚二叠世,定型于三叠纪。

Situated in the east margin of the south Qinling orogen, Yungaishi area is wellknown throughout the world as one of the high quality turquoise occurrences. By detailed investigation, the rheid structures group has been found in formerly so - called "monocline", which is composed of bedding recumbent folds, sheath folds, bddding ductile shear zones, sticky boudinage, intrafolial folds, etc. This type of stuctures group was developed in a lower structural level through bedding stratified shear deformation under...

Situated in the east margin of the south Qinling orogen, Yungaishi area is wellknown throughout the world as one of the high quality turquoise occurrences. By detailed investigation, the rheid structures group has been found in formerly so - called "monocline", which is composed of bedding recumbent folds, sheath folds, bddding ductile shear zones, sticky boudinage, intrafolial folds, etc. This type of stuctures group was developed in a lower structural level through bedding stratified shear deformation under conditions of high temperature and low strain rate. It is considered that the turquoise was formed by cavity filling with epithermal metamophic solution and the rheid deformation controled some of the host structures and supporting structures of the turquoise ore deposit.

云盖寺地区位于南秦岭造山带东缘,以盛产优质绿松石而闻名。研究发现,在前人所称单斜“层”内包容有丰富的固态流变构造群落,如:顺层掩卧褶皱,鞘褶皱、顺层韧性剪切带、粘滞型石香肠及片内无根褶皱等,并认为它们是在较深构造层次中,以较高温低应变速率方式通过顺层分层剪切变形作用形成。笔者认为绿松石为低温变质热液充填成因,固态流变构造变形控制了绿松石矿床的一些容矿和配矿构造。

 
<< 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掩卧的内容
在知识搜索中查有关掩卧的内容
在数字搜索中查有关掩卧的内容
在概念知识元中查有关掩卧的内容
在学术趋势中查有关掩卧的内容
 
 

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