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ore controlling structures
相关语句
  控矿构造
     GEOLOGICAL CHARACTERISTICS AND ORE CONTROLLING STRUCTURES OF THE LISHAN GOLD DEPOSIT
     江西利山金矿床地质特征及控矿构造
短句来源
     This paper deals systematically with the various geological characteristics of the Lishan gold deposit,highlighting the ore controlling structures.
     本文较系统地阐述了利山金矿床的各项地质特征,并重点就控矿构造问题进行了总结讨论,认为NWW向断裂带严格控制了所有金矿体的产出。
短句来源
     Diagnosis of remote sensing geology on the deposits was tried through deciding the ore controlling structures and the favorable mineralizing radius of the deposits .
     尝试利用控矿构造和硫铁矿化的成矿有利半径对区内硫铁矿床进行遥感地质预测 ,圈定出莺子山和皇姑山 2个有利成矿地区的范围。
短句来源
     The main metallogenic and ore controlling factors for the gold deposit in the area are a favorite assemblage of metallogenic and ore controlling structures,the metamorphic rocks of Proterozoic Mayuan Group and the itermidiateacid magmatic activity in the early Yanshanian;
     该区有利的成矿、控矿构造条件、麻源群变质岩以及燕山早期岩浆活动是金矿成矿的最重要因素,也是找矿的主要标志。
短句来源
     The depths of ductile deformation of ore controlling structures are about 3 704~5 086 m and the depths of brittle deformation are about 375~2 944 m. Petrofabric analysis shows that polar projection of chlorite and quartz in NE trending faults are mainly horizontal big circle and density, and major density or dot density parallel or vertical to the kinematic main axis.
     声发射法、包裹体测压法推测控矿构造韧性变形时的形成深度为 3 70 4~ 5 0 86m ,脆性变形时为 375~ 2 944m。
短句来源
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  构造控矿
     Therefore we can analyse the deformation and evolution of ore controlling structure and find out regularity for the ore controlling structures
     据此可以分析控矿构造的变形性质及演化,查明构造控矿的规律。
短句来源
     Based on the thorough analysis of the ore controlling structures, source of ore forming material and transportation characteristics in Tomorite gold deposit region, the paper proposed a four stage ore controlling model of ductile brittle shear zones in the area.
     通过对青海省乌兰县托莫尔日特金矿区韧 -脆性剪切带变形特征、成矿物质与热液来源及运移条件分析 ,提出了该区构造控矿演化的四阶段模式。
短句来源
  “ore controlling structures”译为未确定词的双语例句
     POSITIVE EMPLACEMENT OF MANTLE GOLD BEARING FLUID AND FORMING MECHANISM OF ORE CONTROLLING STRUCTURES
     幔源含金流体主动就位与容矿断裂形成机制
短句来源
     Aimed at the three different types of orebody groups within the ore deposit, discussion was made from the angle of ore controlling structures on the controlling effects of the different times, types and levels of structures on the orebodies.
     针对该矿床存在三种不同类型的矿体群,从控矿构造的角度出发,分别论述了不同时代、不同类型和不同层次的构造对矿体的控制作用。
短句来源
     ORE CONTROLLING STRUCTURES OF THE SEDIMENTS HOSTED DISSEMINATED GOLD DEPOSIT IN THE NORTH WEST AND SOUTH WEST MARGINS OF THE YANGTZE PLATE
     扬子地块西北缘、西南缘卡林型金矿床的构造控矿特征
短句来源
     The mechanism of positive emplacement of mantle gold bearing fluid is proposed on the basis of the composition of quartz inclusions,theoretical analysis of forming mechanism of ore controlling struc tures,high T,P experiments and dynamic mathematical formulae,instantaneous emplacement of gold bearing fluid and forming setting of ore controlling structures.
     基于石英包裹体成分测定、容矿断裂形成机制的理论分析、高温高压实验研究、动力学数学公式举例、含金流体瞬间就位过程及容矿断裂形成环境的探讨 ,提出了幔源含金流体主动就位机制。
短句来源
     Shibangou gold deposit in Xixia, Henan, is a typical altered rock type gold deposit. Shear zones in near NW direction is the key ore controlling structures.
     河南西峡石板沟金矿为一典型的蚀变岩型金矿, 近NW 向的剪切带为主要控矿因素。
短句来源
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The general pattern of geological structures in Shanhu district is abroom-shaped rotational structure, with the Hululing structure-magmaticarch as the central axis, and strongly right-rotating in the periphery. Itis converged to the south and spreaded out to the north. Accordingto the differences of structural environments on the two sides of theBijiashan fault, this district can be divided into two orefields. It is pre-dicted that there exists a hidden granite intrusion to the south of Chang-yingling...

The general pattern of geological structures in Shanhu district is abroom-shaped rotational structure, with the Hululing structure-magmaticarch as the central axis, and strongly right-rotating in the periphery. Itis converged to the south and spreaded out to the north. Accordingto the differences of structural environments on the two sides of theBijiashan fault, this district can be divided into two orefields. It is pre-dicted that there exists a hidden granite intrusion to the south of Chang-yingling and underneath the region from Damudu to LiandLowan. The ore-controlling structures in this district are the Changyingling grid faultsystem, and the ore-holding structures are the secondary shear crackswithin this system. The metallogenic model of this district is proposed inthis paper, i. e. post-magmatic hydrothermal solution was segregated inmany stages from the Changyinglins hidden grante, and coordinating withthe crack structures developed, the ores were deposited by polystage filling,

珊瑚地区地质结构的总格局是以葫芦岭构造岩浆穹隆为中心砥柱,外围强烈右旋并向南收敛、向北撤开的帚状旋扭构造。根据笔架山断层两侧地质构造环境差异,可将珊瑚区划分为东、西两个矿田。预测长营岭以南,大木肚、镰刀湾一带地下存在着隐伏岩体。该区控矿构造为长营岭格状断裂系统;而容矿构造则为格状断裂系统中的次级剪切裂隙。文章最后初步提出该区成矿模式的设想,即长营岭隐伏花岗岩岩浆期后热液多阶段分异,配合构造的发育,多次充填成矿。

The Jinbeizhuang Archean metamorphic iron ore deposit is situated in where the north side of Yanshan settle-zone crosses Inner Mongolia Eath's Axis.The metamorphie iron deposit occurs in Guzuizi formation of Sang- gan group in metamorphic sequence.At the lower and middle parts of the formation the fine-graied garnet-bearing issite predominate the upper part,the biotite plagiogneiss.The iron ore deposit occurs between these two types of rock,mainly at the side of issite. The rouph considerations:the...

The Jinbeizhuang Archean metamorphic iron ore deposit is situated in where the north side of Yanshan settle-zone crosses Inner Mongolia Eath's Axis.The metamorphie iron deposit occurs in Guzuizi formation of Sang- gan group in metamorphic sequence.At the lower and middle parts of the formation the fine-graied garnet-bearing issite predominate the upper part,the biotite plagiogneiss.The iron ore deposit occurs between these two types of rock,mainly at the side of issite. The rouph considerations:the ore-controlling structure of this ore area being mainly a overturned anticline;the original rock of iron- bearing formation being mainly neutral and basic volcanic rock;me- tamorphic facies being mainly high-grade amphibolite faeies;there being migmatization at dearer-stage.

近北庄太古代变质铁矿床位于燕山沉降带北侧与内蒙地轴的交接部位。铁矿床赋存于桑干群谷咀子变质岩系中。含铁建造下部和中部以细粒含石榴石斜长角闪岩为主,上部以黑云斜长片麻岩为主,铁矿床主要产在上述两种岩类转换部位的斜长角闪岩一侧.初步认为,矿区主要控矿构造为一倒转背斜。含铁建造原岩以中基性火山岩为主,其变质相主要为较高级的角闪岩相。后期有混合岩化作用。

Fluorite fields in Zhejiang are located in a triangle massif confined bythree great faults, which had kept the ore--bearing solution from dissipatingand determined the basic pattern of ore controlling structures. It is the differences in mechanical properties, shapes and sizes,characteristics of evolution and deformation, that controlls the spacedistribution, grade and resources of ores and physical properties offluorite. On the basis of geomechanical analysis, the NE and NW--trendingore controlling...

Fluorite fields in Zhejiang are located in a triangle massif confined bythree great faults, which had kept the ore--bearing solution from dissipatingand determined the basic pattern of ore controlling structures. It is the differences in mechanical properties, shapes and sizes,characteristics of evolution and deformation, that controlls the spacedistribution, grade and resources of ores and physical properties offluorite. On the basis of geomechanical analysis, the NE and NW--trendingore controlling faults are regarded as compressive--shear conjugatedstructures.

武义-永康萤石矿田,位于乐清-章村、宁波-丽水和三门-衢县三大裂断带的交汇、闭合地段。不但形成了阻挡矿液逸散和萤石矿在本区集中分布的构造环境,而且也决定了矿田控矿构造的基本格局。不同方向控矿断裂的力学性质和复合机制不但决定着成矿机率、矿体形态规模,而且控制着矿体空间分布、矿液侵位高度与剥蚀深度的相应变化。本区属压扭性共轭控矿构造带。

 
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