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
   mineralization fluid 的翻译结果: 查询用时:0.36秒
图标索引 在分类学科中查询
所有学科
地质学
矿业工程
更多类别查询

图标索引 历史查询
 

mineralization fluid
相关语句
  成矿流体
     It is revealed that,cation in the mineralization fluid is Na+ and K+,while ation is Cl-and F-. The content of CO2 in gas phase is usually high,and the mineralization fluid is a little-alkaline and low-salinity Na solution. Gold mainly transferred to the form of [Au(S2O3)2]3-and -.
     研究结果表明:金成矿流体中的阳离子主要为Na+、K+,阴离子主要为Cl-、F-,气相组分中CO2的含量普遍较高,成矿流体属于偏碱性,具有低盐度的Na质溶液,其中金主要以[Au(S2O3)2]3-、[AuS2]-形式迁移;
短句来源
     THE RELATIONSHIP BETWEEN TECTONIC STRESS FIELD AND THE MOVING AND DISTRIBUTION OF MINERALIZATION FLUID(GROUNDWATER)
     构造应力场与成矿流体(地下水)运移、分布的关系研究
短句来源
     During the study on inclusions in an ore field in southern Hunan province, the composition data of the inclusion handled by R - type of cluster analysis show internal relations which indicate source and evaluation process of mineralization fluid.
     在湘南某区包裹体研究中,用R型点群分析对包裹体的成分数据进行处理,使数据显示内在联系。 从而阐明了成矿流体的来源及演化过程:通过对该区包裹体成分数据的数学处理,为解释成矿流体来源。
短句来源
     The mineralization temperature is in a range of 90℃~300℃, and the mineralization fluid is a combination of slightly acidic-slightly alkalic precipitations,seawater and magmatic water.
     其成矿温度在90~300℃之间,成矿流体为低盐度的弱酸性一弱碱性大气降水、海水和岩浆水的混合溶液。
短句来源
     INFLUENCE OF TELLURIDE FUGACITY IN THE MINERALIZATION FLUID ON FINENESS OF NATIVE GOLD
     成矿流体中碲逸度对自然金成色的影响
短句来源
更多       
  流体包裹体
     Isotope Composition of Fluid Inclusion and Tracing to the Source of Mineralization Fluid in Dongsheng Uranium Deposit, North Ordos Basin
     东胜铀矿流体包裹体同位素组成与成矿流体来源研究
短句来源
     After studying ore-bearing rock series,Cu-Au Mineralization,fluid inclusion and H-O isotopes,it is believed that 202 Cu deposit is a porphyry one,and that Lushigou Cu deposit is a skarn. Then,it is pointed out that the key to prospecting Cu and Au in studied area is the depth of denudation.
     通过研究琼河坝地区的含矿岩系、铜金矿化、流体包裹体和氢氧同位素,认为202铜矿为斑岩型矿床,绿石沟铜矿为夕卡岩型矿床,剥蚀程度是本区铜金找矿的关键。
短句来源
     Studies on tbe evolution of fluid from the ductile shear belt in granulite facies terrain and the correlation with the fluid inclusion from the gold deposit in Daqingshan area,Inner Mongoliar shew that the genetic type of gold deposit in the Archean high-grade metamorphic region was complicated,part of mineralization fluid derived from the evolution of retrogres-sive metamorphic hydrothermal soltition and this kind of deposit can be called retrogressive metamorphic hydrothermal gold deposit.
     通过内蒙古大青山地区麻粒岩相岩石内韧性剪切带中流体演化研究,以及与该区内金矿床中流体包裹体的对比,认为产于太古宙高级变质区内的金矿床成因类型复杂,其中有的成矿流体是退变质热液演化的产物,该类矿床可称为退变质热液型金矿床。
短句来源
     The new data of metallogenic epochs, the zoning of the mineralization , fluid inclusions and deep mining outcrops in the Jinqingding gold deposit have been reviewed comprehensively.
     综合评述了金青顶金矿矿化分带、成矿年龄、流体包裹体以及深部采矿露头新资料。
短句来源
  矿化流体
     The formation temperature is below the range of 266--180℃ and the mineralization fluid has a pH value of 5.3--7.6. Its log fo_2 and log fs_2 at 400K, 500K and 600K are also listed in the paper.
     白钨矿化形成温度在266~180℃以下,矿化流体pH为5.3~7.6。 文中列出了400K、500K、600K时的logfo_2和logfs_2值。
短句来源
     Based on the geochemital studies of the ore-bearing formation and the mineralization fluid in the epithermal metasegenetic area, the west of Hunan Province, the paper points out the ore-forming fluid evolutionary regularity which endowed with a continuous drandown in sulfide a markes rise in chloride and a sharp increase in the proportion of meteoric water from An-Sb metallogenization of Proterozoic group to the Hg mineralization of Cambrian group.
     在对湘西低温矿化区中含矿建造的地球化学研究及典型矿床成矿流体性质的比较研究后指出,由元古界板溪群内发育的An、Sb矿化至古生界寒武系内的Hg矿化,其矿化流体具有硫浓度不断降低,氯浓度显著升高,大气降水的比例不断增加的明显规律。
短句来源
  “mineralization fluid”译为未确定词的双语例句
     The gas component was composed of mainly H 2O, less CO 2, H 2 and O 2. The mineralization fluid with averaging 9 168 g/L in degree of mineralization and with range from 5 7 to 8 8 in pH value, was detected that the lg f O 2 value changed from -37 to-38 3 in early mineralization stage and from -37 to -39 in late.
     气相成分以H2 O为主 ,其次是CO2 、H2 和O2 。 矿化度平均 9 68g/L ,pH为5 7~ 8 8,成矿早期氧逸度为 - 37~ - 38 3,晚期为 - 37~ - 39。
短句来源
     The mineralization fluid in Axi gold deposit was divided into five stages. Study on the fluid inclusions shows that the ionic component in fluid was composed of mainly K +, less Na +,SO - 4, Cl - and NO - 3 and minor Ca 2+ and Mg 2+ .
     阿希金矿的成矿分 5个阶段 ,流体成分以K+为主 ,其次是Na+、SO2 - 4、Cl- 、NO- 3 ,Ca2 +和Mg2 +少量。
短句来源
     It is shown that mineralization fluid was not of meteroic origin,but added by fliud of meteroic origin at late mineralization stage. The(87Sr/86Sr)_i,ε_Nd(0) and f_Sm/Nd of the hydrothermal calcite are 0.721123±30,1.14 and 0.13 respectively,which are unanimous with the crust rocks formed in the ocean.
     热液方解石锶同位素初始值 (87Sr/ 86 Sr) i,为 0 .712 12 3± 30 ,Nd同位素组成的现今比值相对于CHUR地幔源中 Nd同位素组成现今比值的万分偏差 εNd(0 )为 1.14,相对于方解石形成时 CHUR地幔源分馏沉淀程度的参数 f Sm Nd为 0 .13,与海洋环境下形成的玄武岩一致。
短句来源
     The movement of mineralization fluid is jointly controlled by tectonic stress,temperature gradient and hydraulic gradient.
     成矿流体的运移受构造应力、温度梯度和水力梯度的联合控制。
短句来源
     It is suggested that the mineralization fluid is over-saturation and occurring boilization and supposed that there is magma chamber in deep of mining area. The second stage is behind hydrothermal of magma with middle-high temperature, middle and high salinityH 2O-NaCl fluid, which homogenization temperature are 300~350oC and salty 7.4~41.59(w t%NaCl),pressure 10.8~19.3MPa.
     均一温度为300~350oC,盐度7.4~41.59(wt%NaCl),压力10.8~19.3MPa。
短句来源
更多       
查询“mineralization fluid”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


It has been consistently held that the mineralization fluid forming wolframite quartz-vein is high-middle hydrothermal solution. In this paper, according to a large number of geological facts, it is believed that ore-forming fluid forming wolframite quartz-vein is likely a fluid which has transitional property between hydrothermal solution and magma. It has great viscosity and density. It contains a great quantity of SiO2. The facts are as follows., the transition from quartz-vein to aplite...

It has been consistently held that the mineralization fluid forming wolframite quartz-vein is high-middle hydrothermal solution. In this paper, according to a large number of geological facts, it is believed that ore-forming fluid forming wolframite quartz-vein is likely a fluid which has transitional property between hydrothermal solution and magma. It has great viscosity and density. It contains a great quantity of SiO2. The facts are as follows., the transition from quartz-vein to aplite and to pegmatite, the changes of varieties and intensity of country rock alteration, vug characteristics in wolframite quartz-vein, the results of the study of mineral inclusions,the irregularity of local concentration of a large quantity of metal minerals, the emerged features of wolframite in quartz-vein, the granite breccia in quartz vein filling in hornfels, the variation of MnO/FeO ratio in wolframites and of mineral assemblage and chemical composition in the ore-vein etc. The transitional fluid is c

对于黑钨矿石英脉的成因,历来都认为是高中温热液充填而成。本文根据石英脉与细晶岩、伟晶岩过渡;围岩蚀变种类及强度的变化;石英脉中晶洞特征的研究;矿物包裹体研究及测温资料;金属矿物局部大量集中的不规律性;石英脉中黑钨矿的产出特点;产在角岩中的石英脉内出现花岗岩角砾;黑钨矿中MnO/FeO比值变化特征:含钨石英脉中矿物组合和化学成分变化特征,认为形成黑钨矿石英脉的成矿流体是一种粘稠的、密度较大、成分以SiO_2为主的熔浆—热液过渡性流体,它具有上部偏液、下部偏浆的特点。

the Yinshan Cu-Pb-Zn ore deposits are closely related with the Xi-shan caldera. The ore bodies are distributed in the fracture system of thecaldera abd in both sides of contact zones between the subvolcanic por-phyny bodies and country rocks.The volcanic activity may be divided into two cycles from early tolate stage of valcanism. They consist of rhyolitic and dacitic extrusive-intrusive rocks respectively. The metallogenesis followed during each cycle.In the same time two types of alteration of country rocks...

the Yinshan Cu-Pb-Zn ore deposits are closely related with the Xi-shan caldera. The ore bodies are distributed in the fracture system of thecaldera abd in both sides of contact zones between the subvolcanic por-phyny bodies and country rocks.The volcanic activity may be divided into two cycles from early tolate stage of valcanism. They consist of rhyolitic and dacitic extrusive-intrusive rocks respectively. The metallogenesis followed during each cycle.In the same time two types of alteration of country rocks are cormed cor-respondingly. The mineralization is obviously zoned, especially for sub-volcanic dacite porphyry.Considering the chemical nature of Cu, Pb, Zn sulphioes and the sur-roundings of the mineralization fluid, the authors have predicted the pro-spect region for this type of ore deposit in Yinshan district and in North-eastern Jiangxi. According to the data of the stable isotopes, the rare ele-ments and the petrology, the authors suggest that the ore-forming androck-forming materials nearly have the same origin, but some mobilizedore-forming material from metamorphic volcanic rock of ShuangqiaoshanGroup has participated in the metallogenesis.

江西德兴银山矿区的矿床分布特征、火山构造、成矿物理化学条件和同位素资料表明,该区铜铅锌矿床的成矿作用无论在时间上、空间上,还是在成因上,都与火山活动有着密切的联系,并且都受西山塌陷破火山口的形成发展控制。

Scheelite in this district is the mineralization product at the early reworked period. Its mincralization intensity is in positive corelation with the wolframite with a mineralizat on scope larger than that of the wolframite. The formation temperature is below the range of 266--180℃ and the mineralization fluid has a pH value of 5.3--7.6. Its log fo_2 and log fs_2 at 400K, 500K and 600K are also listed in the paper.

白钨矿化是改造早期金属矿化的产物。矿化强度与黑钨矿化呈正消长,范围常大于黑钨矿化。白钨矿化形成温度在266~180℃以下,矿化流体pH为5.3~7.6。文中列出了400K、500K、600K时的logfo_2和logfs_2值。

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