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   mantle fluid 在 矿业工程 分类中 的翻译结果: 查询用时:0.073秒
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mantle fluid    
相关语句
  地幔流体
    MANTLE FLUID AND ITS ROLE IN GOLD ORE FORMING PROCESS _TAKING JIAPIGOU GOLD FIELD FOR EXAMPLE
    地幔流体及其金成矿作用——兼论夹皮沟金矿田的地幔流体与成矿
短句来源
    An approach to mantle fluid mineralization in the superlarge Jinding Pb-Zn deposit, Yunnan Province
    云南金顶超大型铅锌矿床地幔流体成矿作用探讨
    The mineral crystalline age(116.0 Ma) of the mantle fluid metasomatism and the age(51.2 Ma) of the silicon-rich mineralizing fluid suggest that the mantle fluid had been active through the whole processe of the alkalic magma diagenism and associated mineralization.
    据此,从地幔流体交代矿物的结晶年龄(116.0 Ma)到富硅成矿流体年龄(51.2 Ma),揭示地幔流体作用贯穿于富碱岩浆成岩成矿的全过程。
短句来源
    The mantle fluid resulted in the concentrations of Si,Al,Na,K,Si-incompatible elements and ore elements,and the transition of Sr-Nd(isotopic) geochemistry from depleted mantle to enriched mantle,and the high temperature mineralization in the porphyry and the low temperature mineralization in the country rocks.
    正是这一地幔流体作用过程,导致Si、Al、Na、K及其它硅不相容元素和成矿元素富集,进而导致其Sr-Nd同位素特征由亏损地幔向富集地幔过渡,并引起从岩体→围岩对应、从高温→低温的系列成矿效应。
短句来源
    THE MANTLE FLUID AND METALLOGENY
    地幔流体与成矿作用
短句来源
更多       
  地幔流体
    MANTLE FLUID AND ITS ROLE IN GOLD ORE FORMING PROCESS _TAKING JIAPIGOU GOLD FIELD FOR EXAMPLE
    地幔流体及其金成矿作用——兼论夹皮沟金矿田的地幔流体与成矿
短句来源
    An approach to mantle fluid mineralization in the superlarge Jinding Pb-Zn deposit, Yunnan Province
    云南金顶超大型铅锌矿床地幔流体成矿作用探讨
    The mineral crystalline age(116.0 Ma) of the mantle fluid metasomatism and the age(51.2 Ma) of the silicon-rich mineralizing fluid suggest that the mantle fluid had been active through the whole processe of the alkalic magma diagenism and associated mineralization.
    据此,从地幔流体交代矿物的结晶年龄(116.0 Ma)到富硅成矿流体年龄(51.2 Ma),揭示地幔流体作用贯穿于富碱岩浆成岩成矿的全过程。
短句来源
    The mantle fluid resulted in the concentrations of Si,Al,Na,K,Si-incompatible elements and ore elements,and the transition of Sr-Nd(isotopic) geochemistry from depleted mantle to enriched mantle,and the high temperature mineralization in the porphyry and the low temperature mineralization in the country rocks.
    正是这一地幔流体作用过程,导致Si、Al、Na、K及其它硅不相容元素和成矿元素富集,进而导致其Sr-Nd同位素特征由亏损地幔向富集地幔过渡,并引起从岩体→围岩对应、从高温→低温的系列成矿效应。
短句来源
    THE MANTLE FLUID AND METALLOGENY
    地幔流体与成矿作用
短句来源
更多       
  地幔流体的
    The impure components captured in diamond can provide abundent information for the study of mantle fluid.
    金刚石生长阶段所捕虏的不纯净组分,能够提供大量地幔流体的信息。
短句来源
    The genesis of diamond, the solid inclusion indicating mantle fluid, the fluid inclusion and the restrictive factors of fluid are studied in this paper. The relationship between the impure component within diamond and the mantle fluid is also discussed.
    本文从金刚石的成因研究,表征地幔流体的固体包裹体、流体包裹体及流体的制约因素等方面讨论了金刚石不纯净组分与地幔流体的关系。
短句来源
    Ore ~ forming is connected to mantle fluid in the Himalaya stage and it plays essential role in the diagenetic stage and mineralization period.
    成矿与喜山期地幔流体 的活动有关,它在成岩成矿过程中起主导作用。
短句来源
  地幔流体
    MANTLE FLUID AND ITS ROLE IN GOLD ORE FORMING PROCESS _TAKING JIAPIGOU GOLD FIELD FOR EXAMPLE
    地幔流体及其金成矿作用——兼论夹皮沟金矿田的地幔流体与成矿
短句来源
    An approach to mantle fluid mineralization in the superlarge Jinding Pb-Zn deposit, Yunnan Province
    云南金顶超大型铅锌矿床地幔流体成矿作用探讨
    The mineral crystalline age(116.0 Ma) of the mantle fluid metasomatism and the age(51.2 Ma) of the silicon-rich mineralizing fluid suggest that the mantle fluid had been active through the whole processe of the alkalic magma diagenism and associated mineralization.
    据此,从地幔流体交代矿物的结晶年龄(116.0 Ma)到富硅成矿流体年龄(51.2 Ma),揭示地幔流体作用贯穿于富碱岩浆成岩成矿的全过程。
短句来源
    The mantle fluid resulted in the concentrations of Si,Al,Na,K,Si-incompatible elements and ore elements,and the transition of Sr-Nd(isotopic) geochemistry from depleted mantle to enriched mantle,and the high temperature mineralization in the porphyry and the low temperature mineralization in the country rocks.
    正是这一地幔流体作用过程,导致Si、Al、Na、K及其它硅不相容元素和成矿元素富集,进而导致其Sr-Nd同位素特征由亏损地幔向富集地幔过渡,并引起从岩体→围岩对应、从高温→低温的系列成矿效应。
短句来源
    THE MANTLE FLUID AND METALLOGENY
    地幔流体与成矿作用
短句来源
更多       

 

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  mantle fluid
In response to low environmental salinity, all three species closed the opercular plates firmly and rapidly used up oxygen within the mantle fluid.
      
Ventilation of the mantle cavity depended partially on external water flow, with higher and more stable mantle fluid oxygen concentrations being sustained when the water around barnacles was agitated.
      
Mantle fluid oxygen concentrations were extremely variable; behaviour and oxygen concentrations were not closely coupled.
      
When isolated, the mussels maintain a high osmotic concentration in the mantle fluid as the external salinity drops.
      
We also observed that both 3H-protein and 3H-glycine concentrations were higher in the mantle fluid than in the external sea water, although the ratios of 3H-glycine to 3H-protein in these two fluids were not different.
      
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