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
   成矿作用关系 的翻译结果: 查询用时:0.352秒
图标索引 在分类学科中查询
所有学科
矿业工程
地质学
更多类别查询

图标索引 历史查询
 

成矿作用关系
相关语句
  relationship to mineralization
     AN ANALYSIS OF THE CHARACTERISTICS OF METALLOGENETIC STRUCTURE AND THEIR RELATIONSHIP TO MINERALIZATION IN YANGJIAZHANGZI PORPHYRY MOLYBDENUM ORE FIELD OF DIWA TYPE
     杨家杖子地洼型斑岩钼矿田成矿构造特征及其与成矿作用关系分析
短句来源
     A PRELIMINARY STUDY ON ALTERATION ZONING OF THE YANGCHULING PORPHYRY W-MO DEPOSIT AND ITS RELATIONSHIP TO MINERALIZATION
     阳储岭斑岩钨钼矿床蚀变分带特征及与成矿作用关系的初步研究
短句来源
  “成矿作用关系”译为未确定词的双语例句
     Discussion on the relationship of magmatism and gold metallogeny in Beishan mountain area
     北山地区岩浆活动与金矿成矿作用关系探讨
     The Experimental Study About The Liquid Immiscibility and Ore-Forming process In Felsic Magma
     长英质岩浆中液态不混溶与成矿作用关系的实验研究
短句来源
     Tectonic evolution of Chagannuoer basin and its relationship to uranium metallogenetic process
     查干诺尔盆地构造演化与铀成矿作用关系
短句来源
     Study on adakitic rock and Cu-Au mineralization.
     埃达克质岩与Cu-Au成矿作用关系的初步探讨
短句来源
     A PRELIMINARY STUDY ON PALEOCLIMATE, TECTONIC GEOMORPHY AND URANIUM MINERALIZATION OF M ROCK BODY
     M岩体古气候和构造地貌与铀成矿作用关系的初步探讨
短句来源
更多       
  相似匹配句对
     I is presented.
     I的关系
短句来源
     relation.
     关系;
短句来源
     RELATION OF GOLD MINERALIZATION TO COUNTRY ROCKS
     金矿成矿作用与围岩的关系
短句来源
     A DISCUSSION ON THE RELATIONSHIP BETWEEN FLOW PATTERNS OF KARST WATER AND ORE-FORMING PROCESSES
     岩溶水流方式与成矿作用关系探讨
短句来源
查询“成矿作用关系”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。
  association with mineralization
Gene Expression and Immunohistochemical Localization of Biglycan in Association with Mineralization in the Matrix of Epiphyseal
      
  relationship to mineralization
A major lineament in the Arabian Shield and its relationship to mineralization
      


With lineaments in five different directions and four types of circularstructures being interpreted, detalied analyses have been done in this pa-per on the relationships between silver-gold mineralization and geologicalenvironments, including geotectonics, deep structures, regional structuralframework and circular structures, etc, and thereby, some prospectivemineralization beltes are supposed,

本文对该区五组线性构造和四类环形构造进行了解释,并对大地构造、深部构造环境、区域构造格架以及环形构造等与银金成矿作用的关系进行了详细分析,从而想出了远景予测区。

This paper prelimilarily analyses fhe formational environment, evolution and deformed mechanism of the uraniumbearing siliceous fracture belt No. 330 in stress minerals, rock fabrics,paleo-stress estimates and structural geochemistry and deals with its relationship with uranium mineralization. Based on the microscopic observations on tectonite, quartz and mica in the fracture belt, it is suggested that it appears to have undergone a process of deformation from ductile, brittle, ductile-brittle to brittle stage....

This paper prelimilarily analyses fhe formational environment, evolution and deformed mechanism of the uraniumbearing siliceous fracture belt No. 330 in stress minerals, rock fabrics,paleo-stress estimates and structural geochemistry and deals with its relationship with uranium mineralization. Based on the microscopic observations on tectonite, quartz and mica in the fracture belt, it is suggested that it appears to have undergone a process of deformation from ductile, brittle, ductile-brittle to brittle stage. The features of ductile deformation in rock are the microstructures and microfabrics of undulating extinction, deformation lamellae, flowage structure and B + S-tectonite etc. Measurement of the rccrystallised grain size indicates that the differcntial stress averages 0.5 Kbar.Brittle deformation obviousiy differs from ductile deformation and is characterized by cataclastic structure, breccia, Luders lines, quartz sand-watch structure and S-tectonite or homogeneous fabrics. The mylonite formed during the primary ductile deformation stage is a kind of silica-rich rock ank and the silica mainly comes from late hydrothermal solutions and also from thc dynamic differentiation and the dynamothermal metamorphism The ductile deformation stage is followed by the brittle deformation stage and cataclastic structures appear in the rock, with the early veins filling in it. The mineralization mainly develpps during the ductile-brittle deformation stage in which cataclstic mylonite is formed and the ore-bearing fracture belt is a semi- open system. The geological environment of uranium mincralization is at a temperature of 200-300℃; differential stress, 0.5 Kbar; regional differcntial stress, 0.5 Kbar; depth, 1—2km, essentially belonging to a low-temperature supergene environment.

本文从应力矿物、岩石组构、古应力估算及构造地球化学等方面对330产铀硅质断裂带的形成环境、发展演化及变形机制作了初步分析,并讨论了它们与铀成矿作用的关系。通过构造岩及石英、云母的微观研究,认为本断裂带经历了韧性—脆性—脆韧性—脆性的交替变换变形过程。韧性变形具有波状消光、变形纹、流动构造、B+S构造岩等显微构造和组构特征。据重结晶晶粒粒径测定,其差异应力平均值为0.5干巴。脆性变形与韧性变形明显不同,表现出破裂构造和角砾岩类发育,可见吕对尔线和石英沙钟构造以及S构造岩或均质组构等特点。早期韧性变形阶段形成的糜棱岩是一种富硅岩石,硅除主要来自后来的热液外,也来自原岩的动力分异和动热变质作用。韧性变形阶段之后接着是脆性变形阶段,岩石产生破裂构造,充填了早期脉体。成矿作用主要发生在形成碎裂糜棱岩的脆韧性变形阶段,此时的含矿断裂带是一个半开放系统,成矿的地质环境是:温度200—300℃,差异应力0.5干巴,区域差应力0.5干巴,深度1—2公里,基本上属低温浅成环境。

This paper elucidates the historical setting,the geotecto- hie environment,the features of the crustal movement and their relation to mineralization during the formation of the volcano—tectonic. depression It puts forward a lot of mineralized features of uranium and multimetals:Lead and zinc mineralized earliest,occurring on the outside of the marginal circular texture zone;uranium mineralization and its replacement iufietration found,in the depression on its marginal circular texture zone fluorite mineralized...

This paper elucidates the historical setting,the geotecto- hie environment,the features of the crustal movement and their relation to mineralization during the formation of the volcano—tectonic. depression It puts forward a lot of mineralized features of uranium and multimetals:Lead and zinc mineralized earliest,occurring on the outside of the marginal circular texture zone;uranium mineralization and its replacement iufietration found,in the depression on its marginal circular texture zone fluorite mineralized latest,snperimposed on the mariginal circular texture zone in replacement infiltration.

本文阐述了该火山洼地形成的历史背景、大地构造环境、形成时地壳运动的特点及与成矿作用的关系。提出了铀及多金属的矿化特点:铅、锌成矿最早,产于边缘环状构造带外侧;铀矿化以交代充填方式产于洼地内及其边缘环状构造带上;萤石成矿最晚,以充填方式迭加于洼地边缘环状构造带上。

 
<< 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成矿作用关系的内容
在知识搜索中查有关成矿作用关系的内容
在数字搜索中查有关成矿作用关系的内容
在概念知识元中查有关成矿作用关系的内容
在学术趋势中查有关成矿作用关系的内容
 
 

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