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
   hydrothermal 的翻译结果: 查询用时:0.012秒
图标索引 在分类学科中查询
所有学科
地质学
化学
矿业工程
无机化工
材料科学
海洋学
有机化工
物理学
电力工业
更多类别查询

图标索引 历史查询
 

hydrothermal     
相关语句
  水热
     Study on Hydrothermal & Solvothermal Synthesis of Metastable Phases of Functional Materials
     水热与溶剂热合成亚稳相功能材料研究
短句来源
     Hydrothermal Syntheses, Structures and Characterizations of Keggin-type POM Based Hybrids
     Keggin型多金属氧酸盐分子基化合物的水热合成、结构及表征
短句来源
     Hydrothermal Syntheses and Characterizations of Metal Cluster Polymers and Coordination Polymers
     金属簇聚物与配位聚合物的水热合成与表征
短句来源
     Study on Ba-Ti-based Microwave Dielectric Ceramics by Hydrothermal Synthesis
     水热合成Ba-Ti基微波介质陶瓷的研究
短句来源
     Hydrothermal Synthesis and Charaterization of Mn(Ⅱ)-substituted Aluminophosphates and Manganese Phosphates
     Mn(Ⅱ)取代磷酸铝和磷酸锰微孔化合物的水热合成与表征
短句来源
更多       
  热液
     Studies on Hydrothermal Circulation and Smokers of Modern Seafloor Hydrothermal Activity
     现代海底热液活动的热液循环及烟囱体研究
短句来源
     The Study on Models for Formation of Megaplume Flow in Modern Seafloor Hydrothermal Activity
     现代海底热液活动中巨羽流形成机制的模型研究
短句来源
     LOW TEMPERATURE lgfo_2-PH DIAGRAMS OF SULFUR ISOTOPE EVOLUTION IN EQUILIBRIUM WITH HYDROTHERMAL SYSTEM
     低温平衡热液系统中硫同位素演化的Igf_(O_2)-pH图解
短句来源
     HYDROTHERMAL URANIUM DEPOSITS AND SULPHUR ISOTOPES
     热液铀矿床与硫同位素
短句来源
     AN EXPERIMENTAL STUDY ON PHYSICO-CHEMICAL CONDITIONS FOR THE FORMATION OF SCAPOLITE IN THE HYDROTHERMAL SYSTEM
     方柱石在热液中形成的物理化学条件的实验研究
短句来源
更多       
  水热法
     Hydrothermal Synthesis and Structural Characterization of[(C_3H_7)_2NH_2 ] _4(H_2O)_4Ge_4S_(10)
     水热法合成[(C_3H_7)_2NH_2]_4(H_2O)_4Ge_4S_(10)及晶体结构分析(英文)
短句来源
     Hydrothermal Synthesis and Structure of a Super Molecular Compound [C_6H_(11)NH_3]_6[P_2Mo_(18)O_(62)]·4H_ 2O
     超分子化合物[C_6H_(11)NH_3]_6[P_2Mo_(18)O_(62)]·4H_2O的水热法合成及结构
短句来源
     Hydrothermal Synthesis of (Bi_(0.5)Na_(0.5)) TiO_3 (BNT) Powders
     水热法合成(Bi_(0.5)Na_(0.5))TiO_3(BNT)粉体
     Hydrothermal synthesis and diffuse reflectance spectra of [M(C_5H_4NCOO)_2(H_2O)_n]
     [M(C_5H_4NCOO)_2(H_2O)_n]的水热法合成及漫反射光谱研究
短句来源
     Hydrothermal synthesis of SrAl_2O_4: Eu~(2+) ,Dy~(3+)Long Afterglow Material
     水热法合成SrAl_2O_4:Eu~(2+),Dy~(3+)长余辉材料
短句来源
更多       
  热水
     In the TiO_2_Al_2O_3,(K_2O+Na_2O)_Al_2O_3 and (Co+Ni)_(As+Cu+Mo+Pb+V+Zn) diagram for siliceous rocks, the projection points of siliceous rocks in the Suoyipo copper deposit fall in the region related to the submarine hydrothermal system or hydrothermal sedimentary rock.
     在TiO2_Al2O3和(K2O+Na2O)_Al2O3关系图上和(Co+Ni)_(As+Cu+Mo+Pb+V+Zn)关系图上,其成分投影点均落入与海底热水系统有关或热水沉积岩区的硅质岩区;
短句来源
     The silicolites all belong to hydrothermal sediments in Fe—Mn—(Ni+Co+Cu) triangle diagram and SiO 2—Al 2O 3,SiO 2—Fe 2O 3 diagrams.
     在Fe—Mn—(Ni+Co+Cu)三角图及SiO2—Al2O3、SiO2—Fe2O3图上均属于热水沉积硅质岩。
短句来源
     The SiO 2 contents of siliceous rocks are from 64.2%~94.85%, the average value of which ( 75.9% ) and the relatively high Fe 2O 3, FeO, MnO,TiO 2, Al 2O 3 and MgO values are similar to hydrothermal cherts.
     硅质岩的SiO2 含量变化较大 (6 4 .2 %~ 94 .85 % ) ,平均为 75 .9% ; Fe2 O3 、FeO、MnO、TiO2 、Al2 O3 和MgO等含量相对较高 ,与其它热水成因硅质岩相近 ;
短句来源
     The ratios of Fe/Ti, (Fe+Mn)/Ti, Al/(Al+Fe+Mn) and U/Th, and Al Fe Mn and Fe Mn (Ni+Co+Cu) diagrams show that the siliceous rocks are the sedimentary rocks of hydrothermal origin.
     Fe/Ti、(Fe+Mn)/Ti、Al/(Al+Fe+Mn)、U/Th比值及AlFeMn、FeMn(Ni+Co+Cu)三角图均表明岩石为热水来源沉积岩。
短句来源
     In the Fe-Mn-(Cu+Co+Ni)× 10 diagram, all samples fall in the hydrothermal sediment field.
     在Fe-Mn-(Cu+Ni+Co)和P-Y关系图上,均反映为热水沉积成因;
短句来源
更多       

 

查询“hydrothermal”译词为其他词的双语例句

 

查询“hydrothermal”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。
  hydrothermal
Mordenite composite membranes were prepared by means of coating a porous α-alumina support with nanosized mordenite seeds followed by hydrothermal crystallization.
      
The growth rate of the mordenite crystal increases more along c-axis than that along a-axis or b-axis with increasing temperature for hydrothermal crystallization.
      
The ion-exchanger LiAlTiO4 of spinel type was prepared by the common precipitation/hydrothermal crystallization method, and was acid-modified.
      
Preparation of lithium fast ionic conductor by sol-gel-hydrothermal method
      
The solid fast ionic conductor was synthesized by the sol-gel-hydrothermal method.
      
更多          


The process of hydrothermal crystallization and dissolution of quartz crystals have been investigated by means of designed experiments. The possible structures of the dissolved molecules and the forms of their condensation and process of conversion before and during crystallization have been proposed. The normal and effective growth of crystals was realized by the temperature difference method.

本文实验部分主要研究了用温差法热液生长石英的溶液在冷却以后和重新建立的热液条件下所呈现的一些胶体化学性质。对冷却后的溶液做了超显微镜和电泳相结合的观察;对在重新建立起来的热液条件下的溶液仅做了电泳实验。在这两种情况下,对电泳迭合物都做了物相分析及加热过程中的物相转变的研究。 理论部分根据实验结果及对石英晶体结构的考虑,推测了热液中真溶液部分,在晶体溶解及生长过程中分子的分散和重合的几个可能和主要阶段的结构,着重考虑到溶液中六联环状分子Si_6O_6(OH)_(12)的形成、活动、配联和结晶等问题。从较大的水合分子在结晶过程中的脱水作用,结合表面张力等因素对石英表面上巨大的生长螺旋和一些其他模样的成因做了一些推论,并从生长着的小晶体落在生长着的大晶体柱面上的取向附生的事实说明较大分子的取向性地生长于晶体上是完全可能的。

The pyritic lead-zinc deposits of Chishiachan in the Nanjing Hills, some 20 KM. east of Nanjing of the Kiangzu province, discovered in 1950, have long been thought to be undoubtedly epigenetic and hydrothermal in origin. The writers recently studied the deposits in detail. They are much interested when they find out different sorts of framboidal pyrite in the concretionary and also in the laminated ores of the deposits. Some of the framboidal pyrite have distinct cellur structures of fossilized tissues...

The pyritic lead-zinc deposits of Chishiachan in the Nanjing Hills, some 20 KM. east of Nanjing of the Kiangzu province, discovered in 1950, have long been thought to be undoubtedly epigenetic and hydrothermal in origin. The writers recently studied the deposits in detail. They are much interested when they find out different sorts of framboidal pyrite in the concretionary and also in the laminated ores of the deposits. Some of the framboidal pyrite have distinct cellur structures of fossilized tissues of algae, and some can be identified to be Solenapora. The framboids are now made up mainly of pyrite and melnikovite. The interstices between the "cells" are mostly filled with organic matter. The internal structures of the cellular tissues are of two kinds: (1) the cells, about 20μ in size, are arranged in radiating siphon-like bodies, and (2) the cells, of 40 to 60μ in sizes, are orderly arranged. Associated with the iron sulphide framboids, there are also some metacolloidal structures composed of marcasite and wurtzite. It is probable that, the sulphides were formed when the decaying biogenic protoplasm occurred in the presence of sulphur-reducing bacteria to produce HS~-, which combined with Fe~(++) to yield framboidal melnikovite and its recrystallized product, pyrite. Therefore, they were formed by biochemical processes, as a result of syngenetie sedimentation and early-diagenetic products. The ore bodies are mostly stratiform, stratoid, or in large lenticular forms. The ores are laminated, banded, or in concretionary layers. These structures of the ore bodies are in the main parallel to the stratification of the country rocks. Such kind of ore will constitute the main industrial ores of this district. The age of the ore formation belongs to the early to middle Carboniferous period. But, there are also evidently hydrothermal effects which are superimposed upon the syngenetic ore-forming processes, resulting in the formation.

我们详细地研究了南京栖霞山铅锌硫矿床。特别有意义的是在结核状、层纹状矿石内发现了各种各样的草莓状黄铁矿。经研究藻类的专家鉴定,其中有些具藻类化石的细胞组织,有些具管孔藻类化石的细胞组织。它们主要是由黄铁矿和胶黄铁矿组成。其细胞的间隙常为有机质所充填。但其内部结构特征是:(1)由粒径约20μ的细胞排列成管状放射体;(2)主要由粒径自40—60μ的细胞有序地排列。其生成可能是当生物原生质腐烂时,遂发生硫还原细菌产生HS~-。这种HS`-与Fe~(2+)相结合生成草莓状黄铁矿。因此,它们是生物化学作用的产物,是同生沉积——早期成岩阶段的结果。与之伴生的还有变胶状构造。这类矿石将成为本区主要的工业矿体。其生成时代属早——中石炭世。矿体呈层状、似层状是或大透镜体。其产状与围岩基本上是一致的,但局部有斜交(热液迭加的结果)。但本区也有明显属后生的脉状、网脉状、浸染状及晶簇状矿石。它们往往具有显著的充填交代特征。此中普遍地表现为闪锌矿交代黄铁矿,方铅矿交代闪锌矿。其产出常与断裂构造及硅化、重晶石化具有密切的关系。显然,这是多期多阶段热液迭加的成矿现象。本区的铅锌矿,主要与这种成矿作用有关。因此,本区的矿石是由同生沉积——热...

我们详细地研究了南京栖霞山铅锌硫矿床。特别有意义的是在结核状、层纹状矿石内发现了各种各样的草莓状黄铁矿。经研究藻类的专家鉴定,其中有些具藻类化石的细胞组织,有些具管孔藻类化石的细胞组织。它们主要是由黄铁矿和胶黄铁矿组成。其细胞的间隙常为有机质所充填。但其内部结构特征是:(1)由粒径约20μ的细胞排列成管状放射体;(2)主要由粒径自40—60μ的细胞有序地排列。其生成可能是当生物原生质腐烂时,遂发生硫还原细菌产生HS~-。这种HS`-与Fe~(2+)相结合生成草莓状黄铁矿。因此,它们是生物化学作用的产物,是同生沉积——早期成岩阶段的结果。与之伴生的还有变胶状构造。这类矿石将成为本区主要的工业矿体。其生成时代属早——中石炭世。矿体呈层状、似层状是或大透镜体。其产状与围岩基本上是一致的,但局部有斜交(热液迭加的结果)。但本区也有明显属后生的脉状、网脉状、浸染状及晶簇状矿石。它们往往具有显著的充填交代特征。此中普遍地表现为闪锌矿交代黄铁矿,方铅矿交代闪锌矿。其产出常与断裂构造及硅化、重晶石化具有密切的关系。显然,这是多期多阶段热液迭加的成矿现象。本区的铅锌矿,主要与这种成矿作用有关。因此,本区的矿石是由同生沉积——热液迭加形成的。

The pyritic lead-zinc depcsits of Chishiashan in the Nanjing Hills, some 20 KM. east of Nanjing of the Kiangsu province, discovered in 1950, have long been thought to be undoubtedly epigenetic and hydrothermal in origin. The writers recently studied the deposits in detail. They are much interested when they find out different sorts of framboidal pyrite in the concretionary and also in the laminated ores of the deposits. Some of the framboidal pyrite have distinct cellur structures of fossilized tissues...

The pyritic lead-zinc depcsits of Chishiashan in the Nanjing Hills, some 20 KM. east of Nanjing of the Kiangsu province, discovered in 1950, have long been thought to be undoubtedly epigenetic and hydrothermal in origin. The writers recently studied the deposits in detail. They are much interested when they find out different sorts of framboidal pyrite in the concretionary and also in the laminated ores of the deposits. Some of the framboidal pyrite have distinct cellur structures of fossilized tissues of algae, and some can be identified to be Solenapora. The framboids are now made up mainly of pyrite and melnikovite. The interstices between the "cels" are mostly filled with organic matter. The internal structures of the cellular tissues are of two kinds: (1) the cells, about 20μ in size, are arranged in radiating siphon-like bodies, and (2) the cells, of 40 to 60μ in sizes, are orderly arranged. Associated with the iron sulphide framboids, there are also some metacolloidal structures composed of marcasite and wurtzite. It is probable that, the sulphides were formed when the decaying biogenic protoplasm occurred in the presence of sulphur-reducing bacteria to produce HS_-, which combined with Fe~(++) to yield framboidal melnikovite and its recrystallized product, pyrite. Therefore, they were formed by biochemical processes, as a result of syngenetic sedimentation and early-diagenetic products. The ore bodies are mostly stratiform, stratoid, or in large lenticular forms. The ores are laminated, banded, or in concretioary layers. These structures of the ore bodies are in the main parallel to the stratification of the country rocks. Such kind of ore will constitute the main industrial ores of this distrier. The age of the ore formation belongs to the early to middle Carboniferous period. But, there are also evidently hydrophermal effects which are superimposed upon the syngenetic ore-forming processes, resulting in the formation.

我们详细地研究了南京栖霞山铅锌硫矿床。特别有意义的是在结核状、层纹状矿石内发现了各种各样的草莓状黄铁矿。经研究藻类的专家鉴定,其中有些具藻类化石的细胞组织,有些具管孔藻类化石的细胞组织。它们主要是由黄铁矿和胶黄铁矿组成。其细胞的间隙常为有机质所充填。但其内部结构特征是:(1)由粒径约20μ的细胞排列成管状放射体;(2)主要由粒径自40—60μ的细胞有序地排列。其生成可能是当生物原生质腐烂时,遂发生硫还原细菌产生HS~-。这种HS~-与Fe~(2+)相结合生成草莓状黄铁矿。因此,它们是生物化学作用的产物,是同生沉积——早期成岩阶段的结果。与之伴生的还有变胶状构造。这类矿石将成为本区主要的工业矿体。其生成时代属早——中石炭世。矿体呈层状、似层状或大透镜体。其产状与围岩基本上是一致的,但局部有斜交(热液迭加的结果)。但本区也有明显属后生的脉状、网脉状、浸染状及晶簇状矿石。它们往往具有显著的充填交代特征。此中普遍地表现为闪锌矿交代黄铁矿,方铅矿交代闪锌矿。其产出常与断裂构造及硅化、重晶石化具有密切的关系。显然,这是多期多阶段热液迭加的成矿现象。本区的铅锌矿,主要与这种成矿作用有关。因此,本区的矿石是由同生沉积——热液...

我们详细地研究了南京栖霞山铅锌硫矿床。特别有意义的是在结核状、层纹状矿石内发现了各种各样的草莓状黄铁矿。经研究藻类的专家鉴定,其中有些具藻类化石的细胞组织,有些具管孔藻类化石的细胞组织。它们主要是由黄铁矿和胶黄铁矿组成。其细胞的间隙常为有机质所充填。但其内部结构特征是:(1)由粒径约20μ的细胞排列成管状放射体;(2)主要由粒径自40—60μ的细胞有序地排列。其生成可能是当生物原生质腐烂时,遂发生硫还原细菌产生HS~-。这种HS~-与Fe~(2+)相结合生成草莓状黄铁矿。因此,它们是生物化学作用的产物,是同生沉积——早期成岩阶段的结果。与之伴生的还有变胶状构造。这类矿石将成为本区主要的工业矿体。其生成时代属早——中石炭世。矿体呈层状、似层状或大透镜体。其产状与围岩基本上是一致的,但局部有斜交(热液迭加的结果)。但本区也有明显属后生的脉状、网脉状、浸染状及晶簇状矿石。它们往往具有显著的充填交代特征。此中普遍地表现为闪锌矿交代黄铁矿,方铅矿交代闪锌矿。其产出常与断裂构造及硅化、重晶石化具有密切的关系。显然,这是多期多阶段热液迭加的成矿现象。本区的铅锌矿,主要与这种成矿作用有关。因此,本区的矿石是由同生沉积——热液迭加形成的。

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