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
   断层系统 的翻译结果: 查询用时:1.056秒
图标索引 在分类学科中查询
所有学科
地质学
矿业工程
石油天然气工业
更多类别查询

图标索引 历史查询
 

断层系统
相关语句
  fault system
     The dominant strik direction of fault system in the lower sequence is NE 30° ̄40°,and the upper one is NE 70° ̄80°.
     下部断层系统的走向优势方位为北东30°~40°,按倾向分为同向正断层和反向正断层两组; 上部断层系统的走向优势方位为北东70°~80°。
短句来源
     FAULT SYSTEM AND TECTONIC STYLE OF THE YITONG GRABEN
     伊通地堑断层系统与构造样式
短句来源
     It is found, by using box-counting method, that the fault system conforms to the power-law distribution on the scale from 5 km to 75 km in the central and western Hainan gold metallogenic province , the fractal dimension of the faults is 1.70. The whole area is divided into nine subblocks according to the difference of the metallogenic systems;
     利用数盒子法对海南岛中西部金矿集中区断层分布统计表明 :断层系统在 5~ 75km尺度内符合分形分布 ,其分维值为 1 .70。
短句来源
     ④stripping fault system provide ore-hosted space;
     ④剥离断层系统进一步提供了扩容空间;
短句来源
     It can be seen that although the larger fractal dimension values of faults are the favorable condition for gold mineralization, the fault system needs to be in the state of the critical fractal dimension(D c=1.5) in order to form super-large scale ore deposit.
     断层的分维值较大 ,是形成金矿化的有利条件 ,若形成超大型矿床 ,则断层系统需处于临界分维状态(Dc≈ 1 .5 )。
短句来源
更多       
  fault systems
     The multifractal dimensions of fault systems conside the contribution of each fault to fractal dimension and reflect the characteristics of fault spatial distributions, avoiding the shortcomings of the research about the fractal dimension of capacity (D0).
     断层系统多重分形避免了容量维D0的不足,考虑了每一条断层对整体分维的贡献,反映了断层的空间分布特征。
短句来源
     Sand Box Analog Models of Extensional Fault Systems
     伸展断层系统的砂箱模拟实验
短句来源
     The strata overlying the Triassic in the Mosuowan on the whole occur as a monocline and the traps are mostly related to faults,which may fall into the deep and shallow fault systems.
     莫索湾地区三叠系以上地层整体近单斜形态,圈闭大都与断层相关,并且断层在纵向上可划分为深、浅2套断层系统
短句来源
     Fractal has been used successfully in the study of impalpable structure of metacrystals, fault systems and geological structure distribution, porous medium, surface roughness of geological bodies and other problems.
     分形已成功地应用于准晶体微粒结构、断层系统和地质构造分布、多孔介质、地质体表面粗糙度和其他问题研究。
短句来源
     mploying the fractal and renormalizational group theories,the essay has established fractal percolation inodels of the rift system umder complex geological conditions,The computation of the fractal dimensions of the actual fault systems reveals that faults are closely related to the connection and per-colation between developed rifts,which may solve some difficult problems in exploring and opening up newoil-gas fields.
     运用分形与重正化群理论,建立了复杂地质条件下裂缝系统的分形渗流模型.计算了实际断层系统的分维后揭示了断层与裂缝发育带以及储集空间的连通性与渗流性的密切联系.解决了勘探开发中的某些疑难问题.
短句来源
更多       
  “断层系统”译为未确定词的双语例句
     The crust extension and rifting occurring in the late post-collisional stage (>18 Ma) formed a series of NS-striking normal faults and associated rifting basins (≤13.5 Ma) across the Tibetan plateau.
     晚期阶段主要发生地壳伸展与裂陷(<18Ma):垂直碰撞带的EW向伸展,形成一系列横切青藏高原的NS向正断层系统(≤13·5Ma)及其围陷的裂谷系和裂陷盆地。
短句来源
     the subblocks are all conformable to the power-law distributions on the scale from 2.5 km to 25 km.
     根据成矿系统的差异 ,将全区分为 9个子区块 ,各子区块断层系统在 2 .5~ 2 5km尺度内均符合分形分布 ,其分维值介于 0 .6 6~ 1 .72之间。
短句来源
     The formulas of friction for three types of fault under Anderson faults systems was gained based on Byerlee law;
     根据Byerlee定律 ,给出了在Anderson断层系统下三种断层的摩擦滑动强度公式 .
短句来源
     The ore forming mechanism of the gold veins which was controlled by the detachment fault was discussed by the analysis on the origin and evolvement of the fault that is developed in the Zhangjiahe gold mine.
     通过对张家河金矿区内发育的拆离断层系统的具体分析,揭示了其产生、发展的过程,对由其控制的金矿脉的形成机制进行了合理的探讨。
短句来源
     THE FEATURES OF FRACTAL DIMENSION OF FAULTS SYSTEM IN THE MIDDLE--SOUTH REGION OF SHANDONG PROVINCE
     鲁中南地区断层系统的分数维特征
短句来源
更多       
查询“断层系统”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。
  fault system
The Yanshan orogenic belt fault system deflected from an EW to a NE direction, then to a NNE direction during the Indo-Chinese epoch-Yanshanian epoch.
      
The thrust-nappe strength of the Qinling-Dabie orogenic belt fault system showed the tendency that the strength was greater in the south and east, but weaker in the north and west.
      
This fault system faulted in the east and folded in the west from the Indo-Chinese epoch to the early Yanshanian epoch.
      
The Tanlu fault system caused the basin to migrate from west to east and south to north.
      
The migration regularity of the East China Sea shelf basin-Okinawa trough fault system shows that the formation age became younger in the west.
      
更多          
  fault systems
Distribution, migration and derivation of Mesozoic-Cenozoic regional fault systems in the central continental margin of eastern
      
The four fault systems exhibit different migration behaviors.
      
The four fault systems and their migration regularities were respectively the results of four different geodynamic backgrounds.
      
The coastal area is dissected by two major fault systems: the first group strikes ENE-WSW and controls the evolution of the adjacent Quaternary basin, while the second one trends NNE-SSW.
      
These fault systems must be taken into account in any coastal engineering considerations.
      
更多          


Two thrust systems in NW and NE directions were formed sutcessively in the diwa tectonic stage on the base of Indosinian folds at the Yanshanian phase in the western part of the Suzhou area. Some of the leading thrust zones have controlled the localization of magmatic rocks. Secondary thrust zones have controlled iron, copper and polymetallic ore deposits. Tectonites at the edges and ends of orebodies and oriented specimen of fracture structures (relic) in skarns and orebodies have been studied systematically...

Two thrust systems in NW and NE directions were formed sutcessively in the diwa tectonic stage on the base of Indosinian folds at the Yanshanian phase in the western part of the Suzhou area. Some of the leading thrust zones have controlled the localization of magmatic rocks. Secondary thrust zones have controlled iron, copper and polymetallic ore deposits. Tectonites at the edges and ends of orebodies and oriented specimen of fracture structures (relic) in skarns and orebodies have been studied systematically with macroscopic and microscopic methods. Based on the relationship between the mineral generations of the skarn-sulfide stage and fracture structures as well as the classification of fault tectonites, we can determine the sequence and intensity of tectonism. Furthermore, we have discussed the leading role of tectonic activities in the concentration, transportation and deposition of ore fluids and the reformation of ore deposits after mineralization. The pulsation of tectonic activity is a prerequisite for the formation of skarn-hydrothermal deposits. Although ore-forming material is dependent on the metallogenic specialization and abundance of elements in the regional deep-seated and mantle rocks, the depth and scope of tectonomagmatic and tectonohydrothermal processes are the key factors for the activation, concentration and transportation of ore-forming elements. The time and space of ore deposition are controlled by the intensity of tectonic activity. Fracture metallogenesis plays a leading role in the diwa region.

苏州西部地区当地壳演化进入地洼阶段后,在印支褶皱的背景上燕山期先后发育了北西、北东向两套逆推断层系统。其主干断裂是岩浆岩的控岩构造。岩浆岩的演化具有地洼区的特色。次一级的逆推断层是区内铁、铜、多金属、黄铁矿矿床的控矿构造。对矿体边部、尾端及岩芯的构造岩剖面、定向标本作了系统的宏观和微观观察;借助于夕卡岩—硫化物阶段矿物世代及其穿插关系,对成矿过程的构造活动序次和强度作了详细的划分。根据断裂活动与矿物世代的相关性,探讨了构造活动对成矿流体的汇聚、运移、沉淀和改造所起的巨大作用。它和区域构造、控矿构造(包括容矿构造、导矿构造和汇聚构造)一样,是断裂成矿构造学的重要研究内容。断裂成矿在地洼构造区占据重要的主导地位。

This paper describes an understanding on the correlation of various blocks in the fault-folded belt in the northern part of western border of Shanxi- Gansu-Ningxia basin and the location of its eastern border which is different from the majority of opinions so far published.It is suggested that various types such as vertical shearing,high angle shrust,compressional pairs and low angle overthrust are formed due to the non-synchronization of the disp- lacement resulting from the background environment and boundary...

This paper describes an understanding on the correlation of various blocks in the fault-folded belt in the northern part of western border of Shanxi- Gansu-Ningxia basin and the location of its eastern border which is different from the majority of opinions so far published.It is suggested that various types such as vertical shearing,high angle shrust,compressional pairs and low angle overthrust are formed due to the non-synchronization of the disp- lacement resulting from the background environment and boundary conditi- ons.This paper points out that the western dipping of the fault plane in Majiatan Area (as usually accepted) refers really to the fault system ot the overthrust sheet and is in a different type with the fault system with east dipping fault plane characterizing the feature of the overthrust sheet front zone,so that they cannot be correlated.The fault plane of the compressio- nal zone of the overthrust sheet front in Majiatan Area dips to the east also,and is in consistent with the same zone in Hengshanbao and Tiekesu- miao Areas.An assumption on the variation of the type of the sheet front is suggested that various blocks in this region are different expressions for- med under the same geostress field,and thus it is not necessary to give an explanation as to whether it is compressive torsional or tensile in nature regarding to different sections.It is also suggested that the east border of this region cannot be recognized according to fault systems or the syncline axis.A concept of tectonic transition is suggested in this paper in this res- pect.This paper suggests also that the tectonic of Tiekesumiao sag should be rediscussed.

本文对西缘断褶带(北段)的区块对比及其东界位置提出了新的观点。认为在若干千米长的推覆带上,因背景环境、边界条件造成的位移不同步,可以形成纵向剪切、高角度掩冲、挤压对峙和低角度推覆等多种类型。指出所谓马家滩地区断面西倾实指各种冲断席的断层系,与表征前缘推挤带特征的断面东倾断层系统不属同类,不能对比。马家滩地区前缘推挤带断层断面同样是东倾的,和该带的横山堡地区,铁克苏庙地区一致。从而提出了推覆体前缘带形式变化说,认为各区块是同一地应力场下的不同表现形式,无须做分段的扭压拉张等解释。同时不同意以断层或向斜轴划分该区东界,提出了构造过渡的观点,并建议重新考虑铁克苏庙坳陷的大地构造单元属性。

In this daper, the dissipative structure, synergetic and catastrophic characters of the evolution of fault system are discussed, the self-organization in fault evolution is expounded, and based on this, the significance of self-organization of fault evolution system in earthquake predi-ction is stated. The auther suggestes that the sef-organization of fault evolution system is the cardinal physical base for earthquake predi ction. Finally, basing on above-mentloned discussion, some earthquake exampl-es are given...

In this daper, the dissipative structure, synergetic and catastrophic characters of the evolution of fault system are discussed, the self-organization in fault evolution is expounded, and based on this, the significance of self-organization of fault evolution system in earthquake predi-ction is stated. The auther suggestes that the sef-organization of fault evolution system is the cardinal physical base for earthquake predi ction. Finally, basing on above-mentloned discussion, some earthquake exampl-es are given in terms of Thorns type A3 cusp catastrophe.

本文讨论了断层系统演化过程的耗散性、协同性、突变性,阐明了断层演化系统的自组织,并以此为基础,论述了断层演化系统自组织对地震预报的意义。作者认为,断层演化系统的自组织,才是地震预报根本的物理基础。基于上述讨论,本文最后结合Thom的A3类尖交变(CuspCatas trophe),给出了地震发生的实际例子。

 
<< 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断层系统的内容
在知识搜索中查有关断层系统的内容
在数字搜索中查有关断层系统的内容
在概念知识元中查有关断层系统的内容
在学术趋势中查有关断层系统的内容
 
 

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