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矿石组构特征
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  “矿石组构特征”译为未确定词的双语例句
     The formation of the deposit is related to action of deposition,as well as afterward metamorphic deformation and hydrothermal superimposed reconstructing.
     对矿石组构特征研究表明,该矿床形成既与沉积作用有关,又遭受后期变质变形及热液的叠加改造,矿床为热水沉积—变质热液改造成因。
短句来源
     THE CHARACTER AND GENESIS OF THE FABRICS OF THE PRECAMBRIAN STRATA-BOUND COPPER ORE DEPOSIT IN CHINA
     中国前寒武纪层控铜矿的矿石组构特征及其成因分析
短句来源
     THE FABRICS OF THE GAOBANHE STRATA-BOUND SULPHIDE DEPOSIT IN HEBEI PROVINCE AND THEIR IMPLICATION OF ORIGIN
     河北高板河层控硫化物矿床矿石组构特征及其成因意义
短句来源
     THE ORE-FABRIC CHARACTERISTICS IN SEVERAL CU-NI DEPOSITS IN NORTHWESTERN CHINA
     西北地区几个铜镍矿床的矿石组构特征
短句来源
     Ore Fabric Characterictics and Their Genetic Significance of Some Stratabound Pb-Zn-S Deposits in Fujian Province
     福建省若干层控型铅锌硫矿床的矿石组构特征及其成因意义
短句来源
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  相似匹配句对
     The Metamorphic Fabrics of Hongtoushan Copper Deposit
     红透山铜矿矿石变质的组构特征
短句来源
     THE ORE-FABRIC CHARACTERISTICS IN SEVERAL CU-NI DEPOSITS IN NORTHWESTERN CHINA
     西北地区几个铜镍矿床的矿石组构特征
短句来源
     the study of the geological characteristics of the deposit, the mineralogy, texture and structure of ores;
     矿床地质特征矿石矿物学和组构学研究;
短句来源
     ORE FABRIC CHARACTERISTICS OF COPPER-IRON DEPOSITS IN TONGLING DISTRICT,ANHUI,CHINA
     铜陵地区石炭系铁铜矿床的矿石组构组分特征
短句来源
     THE CHARACTER AND GENESIS OF THE FABRICS OF THE PRECAMBRIAN STRATA-BOUND COPPER ORE DEPOSIT IN CHINA
     中国前寒武纪层控铜矿的矿石组构特征及其成因分析
短句来源
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The characteristics of ore fabrics, the trace elements in main sulphides, the sulphur isotope, and the inclusion composition of Luo Chang Pb-Zn deposit in the north of Guang Dong are comparatively studied with those of Dong Po Pb-Zn deposit in Heng Shan Ling, the south of Hunan, Further more, the ore-for-ming process and their origins of the ore in the two kinds of deposit are dealt with in this paper. Therefore this paper can give some significances for revealing the origin of the deposits and looking for new...

The characteristics of ore fabrics, the trace elements in main sulphides, the sulphur isotope, and the inclusion composition of Luo Chang Pb-Zn deposit in the north of Guang Dong are comparatively studied with those of Dong Po Pb-Zn deposit in Heng Shan Ling, the south of Hunan, Further more, the ore-for-ming process and their origins of the ore in the two kinds of deposit are dealt with in this paper. Therefore this paper can give some significances for revealing the origin of the deposits and looking for new ones.

作者对比研究了粤北乐昌及湘南东坡横山岭两类铅锌矿床的矿石组构特征、主要硫化物的微量元素、硫同位素及包体成分特征等。从而,论述了两类矿床矿石的形成过程及矿石成因,对揭示矿床成因及指导找矿,具有一定意义。

Many types of ore fabric have been recognized in the Qiandongshan Le-adzinc deposits, and they can be summarized into the following four genetic types; the syngenetic, the diagentic,the epigenetic and the deformation fabrics.An exhaustive study shows that the epigenetic as well as the diagenetic fabrics are predominant.The later both include a lot of structures or textures, such as disseminated, laminated, striped brecciated framboidal, hypidiomorphic finegranular, a part of which can be transformed by the superimposition...

Many types of ore fabric have been recognized in the Qiandongshan Le-adzinc deposits, and they can be summarized into the following four genetic types; the syngenetic, the diagentic,the epigenetic and the deformation fabrics.An exhaustive study shows that the epigenetic as well as the diagenetic fabrics are predominant.The later both include a lot of structures or textures, such as disseminated, laminated, striped brecciated framboidal, hypidiomorphic finegranular, a part of which can be transformed by the superimposition of late tectonic deformation.

本矿床的矿石组构类型可概括为四类:同生沉积组构、成岩组构、后生叠加组构和后期变形改造组构。详细研究表明,以同生沉积和成岩作用形成的组构为主,如浸染状、层纹状、条带状、角砾状构造和莓球状、半自形细粒状结构等,其中部分受到后期构造变形改造、但后生成矿组构极为少见。矿床的地球化学特征研究提供了成矿物质来源于深部地层的信息。因此,从矿石组构特征及成矿物质来源两个方面分析,认为本矿床为海底喷流沉积—成岩弱改造型层控矿床.

This paper deals with geological conditions,S ,Ni abundance(W_s 2 823×10 ̄(-6),W_(Ni) 829×10 ̄(-6)) in ore content mass,and interesting ore fabric of Eastern Huangshan Cu-Ni deposit,Hamie. In addition,optical properties and chemical composition of newly-discovered three rare mineral(Pilsenite,Lead,Ullmannite)are also introduced. The physical-chemical conditions in the ore-building of Eastern Huangshan Cu-Ni deposit are discussed on the basis of chemical composi-tion and ore fabric of several rare minerals.The...

This paper deals with geological conditions,S ,Ni abundance(W_s 2 823×10 ̄(-6),W_(Ni) 829×10 ̄(-6)) in ore content mass,and interesting ore fabric of Eastern Huangshan Cu-Ni deposit,Hamie. In addition,optical properties and chemical composition of newly-discovered three rare mineral(Pilsenite,Lead,Ullmannite)are also introduced. The physical-chemical conditions in the ore-building of Eastern Huangshan Cu-Ni deposit are discussed on the basis of chemical composi-tion and ore fabric of several rare minerals.The conclusion is that it is difficult to form rich ores in the distfict.

本文概略地介绍了哈密黄山东Cu-Ni矿床产出的地质条件,含矿岩体的S,Ni丰度值(W_s2823×10 ̄(-6),W_(Ni)829×10 ̄(-6)),以及矿石中出现的有趣矿石组构;另外,对新发现的三个罕见矿物(叶碲铋矿、自然铅、锑硫镍矿)的光学性质和化学成分也作了介绍。根据几个罕见矿物的化学成分和矿石组构特征,文章讨论了黄山东Cu-Ni矿床的成矿物理化学条件。结论是不宜形成富矿。

 
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