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ore controlling factors
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  控矿条件
     According to the geological features, especially the metallogenesis and mineraliza tion pattern, of the deposits studied and some data measured, and in consideration of the ore material sources and ore controlling factors, the Pb--Zn ore deposits in Nanling and its neighbouring districts are classified into three types, or more de tailed into eight sub-types.
     根据矿床地质特征和部分测试资料,以成矿作用、成矿方式为主,并考虑物质来源、控矿条件等因素,将南岭及其邻区的铅锌矿床划分为3个类型8个亚类型。
短句来源
     The article discusses the geological characters,gold ore controlling conditions and ore prospecting indicators of Bayanwula mountain ore belt and analyzes the ore controlling factors of the ore belt. It is of great importance for further geological prospecting.
     论述巴彦乌拉山成矿带地质特征、金矿控矿条件及其找矿标志 ,分析成矿带的控矿因素 ,对进一步开展地质找矿有重要意义
短句来源
     The article discusses the geological characteristics,gold ore controlling conditions and ore prospecting indicators of Haoping gold deposit and analyzes the ore controlling factors of the gold deposit. it is of great importance for further geological prospectiong.
     论述蒿坪金矿床地质特征、金矿控矿条件及其找矿标志 ,分析金矿床的控矿因素 ,对进一步开展找矿具有重要意义
短句来源
     The ore controlling factors are geodynamic mechanism,layer of volcanic rock,structurl deformations in Dulengou Cu-Co deposit.
     认为该矿床控矿条件为地球动力学环境、变质火山岩及构造变形综合控制。
短句来源
  “ore controlling factors”译为未确定词的双语例句
     Major ore controlling factors and prospecting orientation of Lijiachong gold deposit in Taoyuan county,Hunan
     湖南省桃源县李家冲金矿主要控矿因素及找矿方向
短句来源
     On Geological Characteristics and Ore Controlling Factors of Maojiadian Gold Deposit
     毛家店金矿床地质特征及控矿因素
短句来源
     ANALYSIS OF ORE CONTROLLING FACTORS OF HEQIN MANGANESE DEPOSIT
     云南鹤庆锰矿控矿因素初步分析
短句来源
     ANALYSIS OF ORE CONTROLLING FACTORS OF HUANGTULIANG GOLD DEPOSIT, NORTHWEST HEBEI PROVINCE
     冀西北黄土梁金矿控矿因素分析
短句来源
     This paper sums up the geological features of these Pb-Zn deposits, compares them with MVT deposits abroad and discusses their ore material source, ore fluids, genetic mechanism and ore controlling factors.
     笔者总结了这些铅锌矿床的地质特征,并将这些矿床与国外的MVT矿床进行对比,探讨它们的矿质来源、成矿溶液、成矿机制和成矿控制因素等。
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  相似匹配句对
     Controlling F.
     因此控制F.
短句来源
     and ore-controlling geological interface.
     地质界面控矿。
短句来源
     Quality of Controlling Output of Ore with Computers
     应用电子计算机控制输出矿石的质量
短句来源
     THE ORE-CONTROLLING FACTORS AND PROGNOSIS OF THE MUDING COPPER DEPOSITS
     牟定铜矿控矿因素及成矿预测
短句来源
     APPLICATION OF ASSOCIATION ANALYSIS TO STUDY ON ORE-CONTROLLING FACTORS
     关联度分析在控矿因素研究中的应用
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The YT wulfenite deposit is a new Mo deposit type found out by means of application of diwa theory and probably having more economic value. Its prospect is rather good and it should be studied further.The geotectonic conditions of metallogenesis, geologic features of the deposit and ore-controlling factors have a unique style. The deposit is expected to occur in the area of distribution of the algal-reef ore-source-bed, in the regional tenso-shear fault zone of the NE tectonic system...

The YT wulfenite deposit is a new Mo deposit type found out by means of application of diwa theory and probably having more economic value. Its prospect is rather good and it should be studied further.The geotectonic conditions of metallogenesis, geologic features of the deposit and ore-controlling factors have a unique style. The deposit is expected to occur in the area of distribution of the algal-reef ore-source-bed, in the regional tenso-shear fault zone of the NE tectonic system in the diwa stage cutting deeply into the crust, or in the areas connected with this fault zone.

YT钼铅矿床是运用地洼学说理论发现的、可能具有较大工业价值的一种新型钼矿床类型,前景颇好,值得进一步研究。 其成矿大地构造条件、矿床地质特征、控矿因素等独具一格。在有藻礁矿源层分布,区域性剖切很深的地洼期北东系张剪性断裂发育或与之连通的地段均是本矿的远景区。

Five uranium deposits of carbonate. siliceous-pelitic type occurred in different geological setting are studied. The geological data suggest that this type of uranium deposits is mostly located in the plunging portions of down- faulted zones. The cause of this kind of occurrence is tentatively discussed. It is proposed that uraniferous strata are the uranium source in deposits. The infiltration under arid climatic conditions promoted the uranium concentration up to ore grade. The mesozoic-cenozoic era...

Five uranium deposits of carbonate. siliceous-pelitic type occurred in different geological setting are studied. The geological data suggest that this type of uranium deposits is mostly located in the plunging portions of down- faulted zones. The cause of this kind of occurrence is tentatively discussed. It is proposed that uraniferous strata are the uranium source in deposits. The infiltration under arid climatic conditions promoted the uranium concentration up to ore grade. The mesozoic-cenozoic era which is characterized by the arid climate was the main ore-forming period, The converging condition of ground water in the plunging portions of down-faulted zones was better. Therefore, the plunging portions of down-faulted zones were more favourable for uranium ore formation compared with that of the uplifting portions. The preservation is the most important ore-controlling factor under the neotectonic movement and the plunging portions are the most favourable in this sense. The recognition criteria for the plunging portions of down-faulted zones which can be used in uranium exploration are proposed.

文章以产于不同地质背景及不同层位的五个碳硅泥岩型铀矿床为例,说明该类型铀矿床常分布于断陷带的倾伏地段。初步探讨了该类型铀矿床产于断陷带倾伏地段的原因:富铀地层是成矿的物质基础和前提,经干旱气候条件下地下水的淋积造矿作用成为工业富集,成矿期都在气候干旱的中、新生代;断陷带的倾伏地段比扬起段汇水条件好,易形成铀矿床;在新构造运动上升区,保矿条件是控矿诸因素中最关键的条件,倾伏地段最有利于保矿。文章指出了识别断陷带倾伏地段的标志,对该类型锚矿床找矿勘探有实际意义。

Detailed geochemical studies of the Xi 'an tungsten ore deposit in west Hunan have been conducted with a diversity of geochemical approaches. As deduced from analyses of more than twenty kinds of trace elements and isotopie characteristics of C, 0 and Pb, the Banxi Group slate of great thickness is the source bed of the deposit. H and 0 isotopie compositions of water isolated from fluid inclusions show that the water in ore-forming hydrothermal solutions was derived mainly from heated formation water....

Detailed geochemical studies of the Xi 'an tungsten ore deposit in west Hunan have been conducted with a diversity of geochemical approaches. As deduced from analyses of more than twenty kinds of trace elements and isotopie characteristics of C, 0 and Pb, the Banxi Group slate of great thickness is the source bed of the deposit. H and 0 isotopie compositions of water isolated from fluid inclusions show that the water in ore-forming hydrothermal solutions was derived mainly from heated formation water. Various phy-sico-chemical parameters for the hydrothermal solution have also been obtained from fluid inclusion studies.As deduced from Pb isotopic model age and whole-rock K-Ar age, the age of ore formation falls within the range of 500-600 Ma, suggesting that the Caledonian move-ment is a tectonic movement which had the greatest influence on the studied region. The principal ore-controlling factors are: stratum (source bed), lithologic character (carbo-nate host rock), and tectonics (Caledonian tectonic movement). The available evidence suggests that this deposit is a sedimentary-reworked strata-bound deposit.

使用微量元素、同位素和矿物包裹体等方法对湘西西安白钨矿矿床进行了较详细的地球化学研究。认为该矿床属于沉积-改造型层控矿床,并阐述了矿床的矿源层、成矿时代、成矿条件及控矿因素等问题。

 
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