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液态包裹体
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  liquid inclusions
     STUDIES ON DETERMINATION OF Rb-Sr ISOTOPE OF LIQUID INCLUSIONS IN CHALCOPYRITE
     黄铜矿中液态包裹体Rb-Sr同位素测定方法研究
短句来源
     Investigations on fluid inclusions demonstrate that pure liquid inclusions are the major fluid inclusions in the Gaoshan gold deposit.
     矿床流体包裹体以纯液态包裹体为主 ,成矿流体的温度介于 15 0℃~ 30 0℃之间。
短句来源
  “液态包裹体”译为未确定词的双语例句
     The correlative coefficient equal to -0.62. The infrared spectra of quartz thin-section may be used to study fluid inclusio'n in the quartz and determine its genesis. In Tuan Jiegou porphyry gold deposits, the relative-absorbance of water is higher and there is on carbon-dioxide inclusion in the quartz.
     石英薄片的红外吸收谱可以用来研究它的液态包裹体并决定其成因,在团结沟斑岩金矿床中,石英的水相对光密度较高,并且没有二氧化碳包裹体。
短句来源
     The homogenization and melt temperatures (homogenized at 71 to 140℃ and melted firstly at - 32 to - 22 ℃ and finally at -9 to -5℃)of the two-phase fluid inclusions within these cements indicate that the calcite cement formed at a depth of 1500~1800 m in NaCl-H2O system with 8wt. %~15wt. % NaCl equivalent;
     这些胶结物中的两相液态包裹体的均一化温度和熔化温度表明,方解石胶结物形成于深度为1500~1800m的NaCl-H2O系统中,盐度为8%~20%;
短句来源
  相似匹配句对
     (2) liquid vapor two phases organic inclusion;
     (2 )气液态包裹体 ;
短句来源
     The Fluido Inclusion Geobarometery
     包裹体地质压力计
短句来源
     STUDIES ON DETERMINATION OF Rb-Sr ISOTOPE OF LIQUID INCLUSIONS IN CHALCOPYRITE
     黄铜矿中液态包裹体Rb-Sr同位素测定方法研究
短句来源
     The preparation of liquid hydrogen sulfide
     液态硫化氢的制备
短句来源
     Stimulated Raman scattering in liquid air
     液态空气的受激喇曼散射
短句来源
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  liquid inclusion
The horizontal motion of a liquid inclusion under the action of a stationary reservoir pressure gradient is also studied.
      
The preparation of the first indium liquid inclusion compound and crystal structure of its pa
      
When the reaction is carried out in the presence of an aromatic solvent such as toluene, a liquid inclusion complex forms readily.
      
Tetrabutylammonium salts of the mixed haloindates, [Bu4N][InCl3X], X=Cl, Br, I, interact with aromatic solvents forming liquid inclusion compounds.
      
This liquid inclusion complex, liquid clathrate, can accommodate 8.5 benzene molecules or 8.3 guest toluene molecules per anionic moiety.
      
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  liquid inclusions
Migration of liquid inclusions in a solid under asymmetric temperature oscillations
      
The isomorphic impurities incorporated into the quartz structure by this mechanism are either formed through the decomposition and transformation of composite complexes or as a result of diffusion from crystalline and gas-liquid inclusions.
      
A vast amount of the melt inclusions and fluid-melt inclusions have been found in skarn minerals from Fe, Cu(Au) and Au(Cu) ore deposits distributed from Daye to Jiujiang along the Yangtze River besides vapor-liquid inclusions.
      
Homogenization temperatures of gas liquid inclusions in quartz are 230 - 520°C (mostly 230 - 270°C) for quartz porphyry, 200 - 450°C (mostly 200 - 360°C) for ore-bearing quartz veins, 150- 210°C for granite and 170 - 200°C for the vein quartz in it.
      
The homogenization temperatures of the various types of inclusions are 160°C, 180 - 350°C, 530°C and 870°C for organic inclusions, liquid inclusions, two-phase immiscible liquid inclusions and melt inclusions, respectively.
      
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There are always mechanical mixtures of various minerals, impurity elements and fluid inclusions in quartz, the features of its infrared spectra are quite different. The experiments have shown that as orthoclase and oligoelase are mixed in quartz, the intensities of absorption band at 790 and 909cm~(-1) are related to the content of the quartz, and at 625 and 641cm~(-1) are to the content of the orthoclase and the oligoclase respectively. A negative correlative relation appears between the intensity at 695cm~(-1)...

There are always mechanical mixtures of various minerals, impurity elements and fluid inclusions in quartz, the features of its infrared spectra are quite different. The experiments have shown that as orthoclase and oligoelase are mixed in quartz, the intensities of absorption band at 790 and 909cm~(-1) are related to the content of the quartz, and at 625 and 641cm~(-1) are to the content of the orthoclase and the oligoclase respectively. A negative correlative relation appears between the intensity at 695cm~(-1) and the content of impurity-texture aluminium. The correlative coefficient equal to -0.62. The infrared spectra of quartz thin-section may be used to study fluid inclusio'n in the quartz and determine its genesis. In Tuan Jiegou porphyry gold deposits, the relative-absorbance of water is higher and there is on carbon-dioxide inclusion in the quartz. In Jiapigou metamorphic hydrothermal gold deposits the quartz usually contains more CO_2 inclusions. As relative-absorbance of the carbon dioxide in the quartz is higher, the quartz probably is auriferous one.

本文研究证明,当石英中有正长石和奥长石存在时,在790和909cm~(-1)吸收带的强度与石英有关,而625和641cm~(-1)的强度则分别与正长石和奥长石有关。在956cm~(-1)吸收带的强度与杂质结构铝含量之间有负的相关关系,相关系数是-0.62。石英薄片的红外吸收谱可以用来研究它的液态包裹体并决定其成因,在团结沟斑岩金矿床中,石英的水相对光密度较高,并且没有二氧化碳包裹体。在夹皮沟变质热液金矿床中,石英通常含有较多的二氧化碳包裹体。当石英中二氧化碳的相对吸光度较高时,则可能为含金石英。

This paper summarizes the principle of the fluid inclusion crushing stage and its application in exploration of mesothermal gold deposits. Examples of the use of the stage in determining locations of the altered halos surrounding mesothermal gold depositsand identifying ore-bearing characters of rocks are introduced.

本文综述了液态包裹体压碎法的机理以及该方法在寻找热液型金矿中的应用,例举了用该方法判别岩石的含金性、圈定蚀变晕的空间位置等方面的实例。

The Spiro Sandstone is a rock unit,20-25 m thick, that consists of about equal amounts of limestones and sandstones in the South Hartshorne Gas Field,southeastern Oklahoma.Six lithofacies have been recognized.Depositional characteristics observed in outcrops and cores indicate that cross bedded sandstones and rippled and bioturbated sandstones are reservoir factes and are interpreted as sand-bar (sometimes tidal channel)and sand-sheet deposits in a barrier island complex. Three diagenetic events(compaction,cementation...

The Spiro Sandstone is a rock unit,20-25 m thick, that consists of about equal amounts of limestones and sandstones in the South Hartshorne Gas Field,southeastern Oklahoma.Six lithofacies have been recognized.Depositional characteristics observed in outcrops and cores indicate that cross bedded sandstones and rippled and bioturbated sandstones are reservoir factes and are interpreted as sand-bar (sometimes tidal channel)and sand-sheet deposits in a barrier island complex. Three diagenetic events(compaction,cementation and dissolution)significantly influenced reservoir quality of the Spiro sandstone within the study area.The effect of compaction and consequent pressure solution in reducing primary porosity mainly occured in the sandy limestones and sandstones with greater amounts of carbonate grains, in which the detrital quartz was squeezed into relatively soft and soluble carbonate grains. Five kinds of cements (quartz,calcite, ferroan dolomite,ankerite and asphalt) are present but the calcite cement is most abundant and has the greatest effect on reservoir porosity. The homogenization and melt temperatures (homogenized at 71 to 140℃ and melted firstly at - 32 to - 22 ℃ and finally at -9 to -5℃)of the two-phase fluid inclusions within these cements indicate that the calcite cement formed at a depth of 1500~1800 m in NaCl-H2O system with 8wt. %~15wt. % NaCl equivalent;the ferroan dolomite and ankerite cements precipitated at 2500 ~ 3000 m in a NaCl - MgCl2- H2O system with 10wt. %~20wt. % NaCl equivalent.Overgrowth quartz may have been formed at a depth of 3800 m or more. Dissolution of calcite cements provided the main reservoir porosity.

斯普罗(Spiro)储层是美国俄克拉荷马州匹兹堡县哈桑(Hartshorne)南部气田的一个厚20~25m的岩石地层单元,由大致等量的灰岩和砂岩构成。已鉴别出6种岩石相,储集相为交错层砂岩与波状和生物扰动砂岩,被解释为障壁岛组合中的沙坝(时为潮道)沉积和砂席沉积。在研究区内,3种成岩事件(压实作用、胶结作用和溶蚀作用)严重影响着斯普罗砂岩的储集性能;压实作用和随之而来的压溶作用,在减少原生孔隙度力面的影响主要发生在灰岩和合大量碳酸盐颗粒的砂岩中。该区可见5种胶结物(石英、力解石、含铁白云石、铁由云石和沥青),其中方解石胶结物最丰富并对孔隙度的影响最大。这些胶结物中的两相液态包裹体的均一化温度和熔化温度表明,方解石胶结物形成于深度为1500~1800m的NaCl-H2O系统中,盐度为8%~20%;含铁白云石和铁白云石胶结物形成于深度为2500~3000m的NaCl-MgCl2-H2O系统中,盐度为10%~20%;次生加大石英可能生成于3800m或更深处。方解石胶结物溶蚀所产生的次生孔隙是主要的储集空间。

 
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