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纯气相包裹体
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  pure gaseous inclusions
     N2-CH4 pure gaseous inclusions are mostly primary ones and mainly occur as isolated or cluster ed inclusions in laminated quartz veins in the eclogites together with Ia and Ib inclusions, implying that the type Ⅲ inclusions were probably captured in HP-UHP metamorphism.
     N2-CH4纯气相包裹体均为原生包裹体,主要呈孤立和小群状与Ia和Ib类包裹体分布于榴辉岩中条带状石英脉中,可能主要是在高压-超高压榴辉岩相变质条件下被捕获的;
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  “纯气相包裹体”译为未确定词的双语例句
     It shows many advantages in the determination of compositions of gaseous inclusions, aqueous salt inclusions, volatile bearing aqueous inclusions, and hydrocarbon inclusions.
     激光显微喇曼光谱对纯气相包裹体、盐水溶液包裹体、含挥发分的水溶液包裹体 ,以及有机包裹体的分析已经显示出了很大的潜力。
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  相似匹配句对
     (3) vapor;
     (3) ;
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     CURING WITH VAPOURS
     固化
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     and type C,CO_2-rich or pure CO_2 inclusions of liquid CO_2-gaseous CO_2. Homogenization temperatures of fluid inclusions trapped in the early, middle and late stages concentrated at 300℃~370℃, 200℃~280℃ and 140℃~185℃, respectively.
     /富CO2(+液)两包裹体(C型)。
短句来源
     DETERMINATION OF GAS AND LIQUID COMPONENTS OF INCLUSION IN MINERALS
     矿物包裹体、液成分测定
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     The epoxidation of propene in gas phase has been investigated.
     研究了丙烯氧化的环氧化反应。
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Laser Raman Microspectrometry(LRM) is an important non destructive method for analyse of fluid inclusions. It can give the qualitative, semi quantitative, or quantitative data about the compositions of fluid inclusions quickly. LRM uses a confocal scattering technique, so the preparation of sample is simply, and the dimension of inclusion can be only several microns. It shows many advantages in the determination of compositions of gaseous inclusions, aqueous salt inclusions, volatile bearing aqueous inclusions,...

Laser Raman Microspectrometry(LRM) is an important non destructive method for analyse of fluid inclusions. It can give the qualitative, semi quantitative, or quantitative data about the compositions of fluid inclusions quickly. LRM uses a confocal scattering technique, so the preparation of sample is simply, and the dimension of inclusion can be only several microns. It shows many advantages in the determination of compositions of gaseous inclusions, aqueous salt inclusions, volatile bearing aqueous inclusions, and hydrocarbon inclusions. In addition reseavch, the determination of the ratio of isotope and the molecular interaction in fluid inclusions by LRM are new potential reseavch directions.

激光显微喇曼光谱已经成为流体包裹体非破坏性分析的重要手段。它可以快速方便地对单个包裹体进行定性、半定量乃至定量分析 ,且样品制备简单。通过对入射光进行聚焦 ,可以分析样品中微米级的包裹体。激光显微喇曼光谱对纯气相包裹体、盐水溶液包裹体、含挥发分的水溶液包裹体 ,以及有机包裹体的分析已经显示出了很大的潜力。此外 ,对流体包裹体中同位素比值的分析和作为高温高压下流体的分子之间作用的研究也具有很大应用前景

Preliminary petrographic observation and microthermometric measurements show that there exist three types of fluid inclusions in quartz veins and late stage carbonate veins in HP-UHP rocks from CCSD, including brine (NaCl-H2O) inclusions (type Ⅰ) , NaCl-CaCl2-H2O system inclusions (typeⅡ) and N2-CH4 pure gaseous inclusions (type Ⅲ) , among which the type Ⅰ may be divided into medium-high salinity (type Ia) , medium salinity (type Ib) and low salinity (type Ic) brine inclusions. The type Ⅲ are firstly discovered...

Preliminary petrographic observation and microthermometric measurements show that there exist three types of fluid inclusions in quartz veins and late stage carbonate veins in HP-UHP rocks from CCSD, including brine (NaCl-H2O) inclusions (type Ⅰ) , NaCl-CaCl2-H2O system inclusions (typeⅡ) and N2-CH4 pure gaseous inclusions (type Ⅲ) , among which the type Ⅰ may be divided into medium-high salinity (type Ia) , medium salinity (type Ib) and low salinity (type Ic) brine inclusions. The type Ⅲ are firstly discovered in the CCSD. Type Ia, Ib and Ⅱ inclusions mainly occur as primary or pseudosecondary ones in vein- or matrix quartz in the eclogites, while they were not discovered in vein- or matrix quartz and in the amphibolite facies gneisses, suggesting that these inclusions were probably captured in decompression-recrystallization and retrograde metamorphism of the eclogites. On the contrary, type Ic inclusions are widely distributed and were probably captured in the last stage of UHP exhumation. N2-CH4 pure gaseous inclusions are mostly primary ones and mainly occur as isolated or cluster ed inclusions in laminated quartz veins in the eclogites together with Ia and Ib inclusions, implying that the type Ⅲ inclusions were probably captured in HP-UHP metamorphism. Most of the quartz veins in the eclogites were probably formed by decompression-recrystallization and retrograde metamorphism during exhumation of the subducted plate, while the quartz veins in the gneisses were mainly formed by amphibolite facies or late stage retrograde metamorphism during the exhumation. Distinct differences in compositions and geochemical characteristics of the fluid inclusions in the quartz veins in the eclogites and those in the gneisses, and similarities of the inclusions in the quartz veins and the matrix quartz crystals in their respective hosting rocks suggest that the metamorphic fluid expelled from exhumation of the HP-UHP rocks in CCSD during the exhumation flowed mainly at grain scale.

初步的岩相学和冷热台显微测温表明,CCSDHP-UHP岩石中石英脉和后期碳酸盐脉中含有3种流体包裹体:盐水溶液(NaCl-H2O)包裹体(Ⅰ类)、NaCl-CaCl2-H2O(Ⅱ类)和N2-CH4纯气相(Ⅲ类)包裹体,其中Ⅰ类盐水溶液包裹体可进一步分为中高盐度盐水溶液包裹体(Ia)、中等盐度盐水溶液包裹体(Ib)和低盐度盐水溶液包裹体(Ic),而Ⅲ类为CCSD中首次发现;Ia、Ib和Ⅱ型流体包裹体主要以原生或假次生形式赋存在榴辉岩的石英脉或石英颗粒中,在角闪岩相的片麻岩及其石英脉中均未观察到,显示它们可能主要被捕获于榴辉岩的减压重结晶或退变质阶段,而Ic型包裹体分布广泛,表明其主体可能是在超高压变质岩折返过程的最晚阶段捕获的;N2-CH4纯气相包裹体均为原生包裹体,主要呈孤立和小群状与Ia和Ib类包裹体分布于榴辉岩中条带状石英脉中,可能主要是在高压-超高压榴辉岩相变质条件下被捕获的;CCSD榴辉岩中石英脉的主体形成于板块折返有关的减压重结晶和退变质,而片麻岩中石英脉则主要来源于角闪岩相及其后期退变质作用;榴辉岩和片麻岩中石英脉流体包裹体的组成和地球化学特征存在明显区别,但它们各自相似于其寄主岩石中...

初步的岩相学和冷热台显微测温表明,CCSDHP-UHP岩石中石英脉和后期碳酸盐脉中含有3种流体包裹体:盐水溶液(NaCl-H2O)包裹体(Ⅰ类)、NaCl-CaCl2-H2O(Ⅱ类)和N2-CH4纯气相(Ⅲ类)包裹体,其中Ⅰ类盐水溶液包裹体可进一步分为中高盐度盐水溶液包裹体(Ia)、中等盐度盐水溶液包裹体(Ib)和低盐度盐水溶液包裹体(Ic),而Ⅲ类为CCSD中首次发现;Ia、Ib和Ⅱ型流体包裹体主要以原生或假次生形式赋存在榴辉岩的石英脉或石英颗粒中,在角闪岩相的片麻岩及其石英脉中均未观察到,显示它们可能主要被捕获于榴辉岩的减压重结晶或退变质阶段,而Ic型包裹体分布广泛,表明其主体可能是在超高压变质岩折返过程的最晚阶段捕获的;N2-CH4纯气相包裹体均为原生包裹体,主要呈孤立和小群状与Ia和Ib类包裹体分布于榴辉岩中条带状石英脉中,可能主要是在高压-超高压榴辉岩相变质条件下被捕获的;CCSD榴辉岩中石英脉的主体形成于板块折返有关的减压重结晶和退变质,而片麻岩中石英脉则主要来源于角闪岩相及其后期退变质作用;榴辉岩和片麻岩中石英脉流体包裹体的组成和地球化学特征存在明显区别,但它们各自相似于其寄主岩石中的石英颗粒中包裹体,说明CCSD中HP-UHP岩石在板块折返过程中释放出的变质流体没有经过大规模的迁移。

On the basis of intensive observation of a part of the core of well BZ25-1-7 in the Central Bohai depression and a full understanding of deposit fillings,the authors studied the fluid inclusions in a key core interval.The results show that secondary fluid inclusions mainly occur in micro-fractures of quartz,cements of carbonates or calcite veins.There are four types of fluid inclusion in the area: pure liquid inclusions,pure vapor inclusions,two-phase vapor-fluid inclusions and saline inclusions.Measurements...

On the basis of intensive observation of a part of the core of well BZ25-1-7 in the Central Bohai depression and a full understanding of deposit fillings,the authors studied the fluid inclusions in a key core interval.The results show that secondary fluid inclusions mainly occur in micro-fractures of quartz,cements of carbonates or calcite veins.There are four types of fluid inclusion in the area: pure liquid inclusions,pure vapor inclusions,two-phase vapor-fluid inclusions and saline inclusions.Measurements of homogenization temperatures of most fluid inclusions display three stages of fluid flow: 88-100℃,115-140℃ and 140-155℃,suggesting that there were at least three stages of oil/gas migration and accumulation in the Central Bohai region.According to the above-mentioned study,combined with an analysis of the burial history and thermal history,the authors think that the oil accumulation in the Central Bohai region occurred relatively late,and that the main oil migration and accumulation stage occurred since the late Guantaoan period(13 Ma).

通过详细观察渤中坳陷部分钻孔岩心和充分认识坳陷沉积特征,对重点井段进行了流体包裹体的研究。研究表明:渤中坳陷次生流体包裹体主要赋存于石英颗粒的微裂隙、碳酸盐胶结物和方解石脉中,可分为4类:纯液相包裹体、纯气相包裹体、液态+气态包裹体、盐水溶液包裹体。包裹体均一温度的测定显示其主要分为3期:88~100℃、115~140℃和140~155℃,说明渤中地区油气运聚期次至少存在3期。结合埋藏史和热史的资料分析表明,渤中坳陷总的成藏时间较晚,主要运聚期发生在13Ma(馆陶晚期)以来。

 
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