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   钨成矿作用 的翻译结果: 查询用时:0.748秒
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钨成矿作用
相关语句
  tungsten mineralization
     EVOLUTION AND TIN—TUNGSTEN MINERALIZATION OF THE JINNING—AGED GRANITES IN THE YUNNAN SECTION OF THE KANE DIAN AXIS
     康滇地轴云南段晋宁期花岗岩演化及锡、钨成矿作用探讨
短句来源
     Preliminary discussion of Caledonian granitoids and related tungsten mineralization in west section of northern Qilian Mts.
     北祁连西段加里东期花岗岩类与钨成矿作用的关系浅议
短句来源
  “钨成矿作用”译为未确定词的双语例句
     Ebullition of the Residual Magma and Sn-W Mineralization
     残浆沸腾与锡钨成矿作用
短句来源
     Recent study indicates that a great amount of boiling inclusions exist in the granite associated with W - Sn mineralization.
     近年来,开展了花岗岩与锡钨成矿作用的研究,取得了重要进展。
短句来源
  相似匹配句对
     MULTIPLE DIAGENESIS-MINERALIZATION OF VEIN-TYPE TUNGSTEN KEPOSITS
     脉矿床的多次成岩成矿作用
短句来源
     NEW EVIDENCE FOR THE LIQUATION MINERALIZATION OF W AND Sn
     、锡液态分离成矿作用的新证据
短句来源
     5. regional mineralization;
     5.成矿作用的区域性;
短句来源
     Metallogeny in Relation to Supercontinent
     超大陆旋回和成矿作用
短句来源
     DAJISHAN TUNGSTEN ORE CONCENTRATING MILL
     大吉山选矿厂
短句来源
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  tungsten mineralization
New dating of Dajishan granite and related tungsten mineralization, South Jiangxi Province, China
      
REE geochemistry of fluorites from tungsten mineralization at Dajishan, Jiangxi Province, China
      
The homogenization temperatures of inclusions in the skarn stage range from 350°C to 530°C, later tungsten mineralization-stage inclusions homogenize between 200°C and 300°C, as do inclusions in veins.
      
Fluid inclusions in granite and greisen resemble those of the late tungsten mineralization stage, with low salinity and homogenization temperatures of 200°-360°C.
      
Tungsten mineralization and mica REE geochemistry, Huangsha, Jiangxi
      
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  w mineralization
Several W mineralization stages are shown by the occurrence of ore in massive skarn deposits and in later cross-cutting veins.
      
A polymetallic zone dominated by U-W mineralization was found in Northeast Guangxi.
      
The meta-sedimentary rocks host Damaran-age hydrothermal quartz vein-hosted Sn-W mineralization at Brandberg West and numerous nearby smaller deposits.
      
These MIs represent various stages of evolution of a highly evolved melt system that finally gave rise to granite-related Sn-W mineralization.
      
Tourmaline also occurs as fault-fill and in granitic rocks and associated Sn-W mineralization nearby.
      


A violent ebullition occurred in late residual magma of the S_type granite related to.Sn-W mineralization,and induced the generation of Sn and W ore_forming fluids of high temperature,high pressure,high salinity and high density.The fluids followed a path of stress difference,temperature difference,salinity difference and density difference for lateral migration or vertical migration in a relatively enclosed environment.The physicochemical condition experienced a jumping mutation, so that fluids precipitated...

A violent ebullition occurred in late residual magma of the S_type granite related to.Sn-W mineralization,and induced the generation of Sn and W ore_forming fluids of high temperature,high pressure,high salinity and high density.The fluids followed a path of stress difference,temperature difference,salinity difference and density difference for lateral migration or vertical migration in a relatively enclosed environment.The physicochemical condition experienced a jumping mutation, so that fluids precipitated and formed deposits when they were transported to the place where stress was released.

与锡钨成矿作用有关的“ S”型花岗岩,晚期残浆有强烈的沸腾作用,同时派生出高温、高压、高盐度和高密度锡钨成矿流体,并遵循应力差、温度差、盐度差和密度差的轨迹,在相对封闭的环境中作侧向或垂向运移,当运移到应力释放部位时,流体的物理化学条件发生跳跃式突变而成矿。

A great deal of research shows that the ore forming granite in the Xihuashan tungstun field is a complex intrusion and composed of the Xihuashan complex formed during the second stage of early Yanshanian,the Dangping complex formed during the third stage of early Yanshanian and the single granite and granoporphyry intrusion formed during the first stage of the late Yanshanian. Three tungstun metallogenetic processes are associated with three stages of granitic intrusions and a series of tungsten deposits (such...

A great deal of research shows that the ore forming granite in the Xihuashan tungstun field is a complex intrusion and composed of the Xihuashan complex formed during the second stage of early Yanshanian,the Dangping complex formed during the third stage of early Yanshanian and the single granite and granoporphyry intrusion formed during the first stage of the late Yanshanian. Three tungstun metallogenetic processes are associated with three stages of granitic intrusions and a series of tungsten deposits (such as the Xihuashan tungsten deposit) of different sizes have been formed. This is a typical example in China of multistage diageneses and multiple stages of mineralization in the same granite regions.

大量研究工作证实 ,西华山钨矿田成矿花岗岩为一复式岩体。该复式岩体由燕山早期第二阶段西华山杂岩体 ,燕山早期第三阶段荡坪杂岩体和燕山晚期第一阶段花岗岩、花岗斑岩单一侵入体组成。与两期三个阶段花岗岩有关 ,相应具有三次钨的成矿作用 ,形成了以西华山钨矿为代表的一系列不同规模的钨矿床 ,成为我国花岗岩区多阶段成岩多次成矿的典型范例。

Recent study indicates that a great amount of boiling inclusions exist in the granite associated with W - Sn mineralization. The more boiling inclusions, the more beneficial to the mineralization. Existence of boiling inclusions is an important criterion for searching for W - Sn ores.

近年来,开展了花岗岩与锡钨成矿作用的研究,取得了重要进展。研究表明,与锡钨成矿作用有关的花岗岩,广泛分布有沸腾包裹体,沸腾包裹体愈发育,愈有利于成矿,是重要的找矿标志。

 
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