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  hydrocarbon-source
    EVALUATION INDICES FOR MATURITY OF HYDROCARBON-SOURCE ROCKS
    烃源岩成熟度评价指标及选取
短句来源
    a great number of coal -bearing mudstones contain weak-mid hydrocarbon-source rocks in Shanxi Format ion, then that of Taiyuan Formation belongs to non-hydrocarbon-source rocks.
    结果表明:苏里格庙气田太原组、本溪组以及山西组的煤和碳质泥岩为非烃源岩,大部分山西组煤系泥岩属于差—中等烃源岩,少部分为非烃源岩,太原组则为非烃源岩。
短句来源
    Evaluation of the hydrocarbon-generating characteristic for coal-bearing hydrocarbon-source rocks of Suligemiao gas field
    苏里格庙气田煤系烃源岩生烃特征评价
短句来源
    The research on carbonate hydrocarbon-source rocks from Lower Permian in the Xichang basin, Lower Ordovician in the Ordos basin, and Lower Carboniferous in the Majaoba area, Jiangyou has proved that organic inclusions can form at each stage of thermal evolution of hydrocarbon-source rocks and are the primary samples preserved during oil and gas generation, evolution, migration, and accumulation.
    对西昌盆地、鄂尔多斯盆地及江油马角坝地区不同时代碳酸盐告烃源岩研究表明,在烃源告演化的各个阶段均可形成有机包裹体。
短句来源
    They accurately reflect the type, abundance, and genesis of hydrocarbon-source rocks and related hydrocarbon matter.
    有机包裹体是油气生成、演化、运移、聚集过程中遗留下来的原始样品,它反映烃源告及其中烃类的种类、丰度及成因。
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  “烃源”译为未确定词的双语例句
    RECONSTRUCTION OF ORIGINAL ORGANIC MATTER ABUNDANCE AND ITS HYDROCARBON-GENERATING POTENTIALITIES IN A HIGH MATURE COAL-BEARING STRATA IN CHUXIONG BASIN
    楚雄盆地高成熟煤成烃源岩中原始有机质丰度和原始产烃潜力的恢复
短句来源
    A Quantitative Relationship Between Well Logging Information and Organic Carbon Content
    测井资料与烃源岩有机碳含量的定量关系研究
短句来源
    MIXED SOLVENT EXTRACTION OF IMMATURE SOURCES AND ITS GEOCHEMICAL SIGNIFICANCE
    低熟烃源岩的超强混合溶剂抽提及其地球化学意义
短句来源
    And productivity for type Ⅰ and Ⅱ kerogens were obviously higher than type Ⅲ.
    其产出率Ⅰ,Ⅱ型明显高于Ⅲ型干酪根烃源岩;
短句来源
    Feitan Group Hydrosource Rock in Zhangpu and Oil-Gas Prospect in the Xiapang Seg
    漳浦佛昙群烃源岩与厦澎凹陷油气远景
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  hydrocarbon-source
Comprehensive geochemical identification of highly evolved marine carbonate rocks as hydrocarbon-source rocks as exemplified by
      
All these indicated that the settlement rates are low and the geological conditions are good for the preservation of organic matter, hence favoring the development of hydrocarbon-source rocks.
      
The Klimory and Wulalik formations show certain regularities in those aspects and, therefore, they can be regarded as the potential effective hydrocarbon-source rocks.
      
These facts showed that most of the hydrocarbon-source rocks were formed in shallow-water, high-energy oxidizing environments, thus unfavoring the development of hydrocarbon-source rocks.
      
It is feasible to make use of the geochemical method to comprehensively assess the highly evolved marine carbonates rocks as potential hydrocarbon-source rocks and their distributions.
      


According to the research made on fluid inclusions in Lower Permian carbonate rocks in Xichang Basin,the fluid inclusions could form in every stage of reservoir diagenetic evolution,hydrocarbon generation,migration and accumulation.This could be the direct evidence for the formation environment and development stages of reservoir porosity,and for hydrocarbon generation, migration and accumulation.The study on diagenetic cements and pore-filling minerals of fluid inclusions in different stages shows that the...

According to the research made on fluid inclusions in Lower Permian carbonate rocks in Xichang Basin,the fluid inclusions could form in every stage of reservoir diagenetic evolution,hydrocarbon generation,migration and accumulation.This could be the direct evidence for the formation environment and development stages of reservoir porosity,and for hydrocarbon generation, migration and accumulation.The study on diagenetic cements and pore-filling minerals of fluid inclusions in different stages shows that the evolution of Lower Permian source rocks and reservoir porosity development underwent following seven diagenetic stagesl,namely penecontemporaneous,early diagenetic,mid-late diasenetic,epidiagenetic,early,middle and late reburial stages.The epidiagenetic karst porosity, early reburial deep dissolution porosity and middle-late structural cracks constituted the main oil and gas reservoir spaces in hydrocarbon accumulation period. Hydrocarbon generation and primary migration occurred during LatePermian(i.e.early reburial stage); large amounts of hydrocarbon migrated and accumulated during the Triassic(middle reburial stage) and most of natural gas migration and accumulation took place in Jurassic(late reburial sarge) and thereafter.Hydrocarbon generation,migration and accumulation in the study area were closely related to Hereynian basalt eruption,and the tectonics and magmatic intrusion of indo-China and Yenshanian.

通过对西昌盆地下二叠统碳酸盐岩流体包裹体研究证实,储层成岩演化和烃类生成、运移、聚集的每一阶段均可形成流体包裹体,是储层孔隙形成环境、发育阶段以及油气演化、运移、聚集的直接标志。不同世代胶结物和不同期次孔隙充填矿物中流体包裹体研究结果表明,西昌盆地下二叠统烃源告演化及储层孔隙的发展经历了准同生期、成岩早期和中晚期、表生期、再埋藏早、中、晚期7个演化阶段。其中,表生期岩溶孔洞缝、再埋藏早期深部溶蚀孔洞缝和中晚期构造裂隙构成了区内聚烃期储集空间。石油开始生成和初次运移发生在晚二叠世(再埋藏早期),大量运移聚集发生在三叠纪(再埋藏中期),天然气大量运移聚集发生在侏罗纪及其之后(再埋藏晚期)。油气生成、运移和聚集与海西期玄武岩喷发(热)事件、印支-燕山期构造运动及岩浆多期侵入活动紧密相关。

In the light of gas components, carbon isotope value of commercial gas flow of Zhou-1 well drilled in Permian basalt of Zhougongshan structure in west area of Sichuan and the geochemistry features, combining the for mer researches and explorative achievements, the gas source and exploration potential are expounded. The gas of basalt unconventional. Reservoir is high maturation paulopost one of organic origin coal measure and has the characteristics of high methane, high drying coefficient, high isotope value,...

In the light of gas components, carbon isotope value of commercial gas flow of Zhou-1 well drilled in Permian basalt of Zhougongshan structure in west area of Sichuan and the geochemistry features, combining the for mer researches and explorative achievements, the gas source and exploration potential are expounded. The gas of basalt unconventional. Reservoir is high maturation paulopost one of organic origin coal measure and has the characteristics of high methane, high drying coefficient, high isotope value, low heavy hydrocarbon without H_2S. The gas maturity is identical with the show of thermal evolution tendency in P_2l coal measure area, having enough hydrocarbon source supply. It is possible to obtain the same gas reservoirs in Longtan formation of Permian basalt, tight sand and carbonate rock in Sichuan Basin. The favourable explorative area of basalt is to the west of the line of WeiyuanYibin-Xuyong and the other rocks for availably exploring are the rich hydrocarbon areas of Longnusi, Jiangjin as well as the vicinal regions.

根据川西地区周公山构造周1井在二叠系玄武岩中钻获工业气流的气体组分、碳氢同位素值等地球化学表征,并结合以往研究与勘探成果,对天然气来源、勘探前景进行了论证。研究表明,玄武岩非常规气藏之天然气具高含甲烷、高干燥系数、高同位素值、低重烃、无硫化氢(三高一低一无)特征,属有机成因的煤系高成熟晚期气。天然气主要来自同一层系(上二叠统煤系Ⅲ型母质烃源层)。天然气甲烷碳同位素虽然显示重值,但明显低于典型无机成因的甲烷碳同位素值,无疑属有机成因气。天然气成熟度与P_2l煤系区域热演化趋势展示吻合,成烃强度大,有足够的烃源供给。以此为据,认为四川盆地上二叠统龙潭组玄武岩、致密砂岩、碳酸盐岩有获得类似气藏的可能性,预测其勘探有利地区:玄武岩在成远-宜宾-叙永一线以西;其它岩类则以龙女寺、江津富烃区及其邻区有利。

On the base of summarizing the different packing density types of carboniferous gas developed in Chuandong area, the main factors of controlling gas packing density are discussed. It is proposed out that multiple hydrocarbon sources are the substance foundation of forming high packing density gas reservoirs. Silurian is the important source providing gas for carboniferous reservoirs. The reason for forming high packing density reservoirs is the hydrocarbon enrichment and preservation controlled by the historical...

On the base of summarizing the different packing density types of carboniferous gas developed in Chuandong area, the main factors of controlling gas packing density are discussed. It is proposed out that multiple hydrocarbon sources are the substance foundation of forming high packing density gas reservoirs. Silurian is the important source providing gas for carboniferous reservoirs. The reason for forming high packing density reservoirs is the hydrocarbon enrichment and preservation controlled by the historical and successive development of Kaijiang palaeohighslope belt. The immediate cause of influencing gas packing density is preservation conditions of faults and various traps. The low-secular and low-steep anticlines in the buried structures and synclines on the two wings or two ends of the high-steep structures being relative to Kaijiang palaeohigh slope belt have good exploration potential for drilling high packing density gas in carboniferous reservoirs.

本文在总结川东地区现已勘探开发的石炭系气藏天然气不同充满度类型的基础上,探讨了控制天然气充满度的主要因素。提出多烃源是形成高充满度气藏的物质基础,志留系是为石炭系气藏提供天然气的重要气源;开江古隆起-斜坡带的历史继承性发展,控制了烃类的富集和保存,是形成高充满度气藏的又一重要原因;断层及各种圈闭等保存条件是形成天然气充满度高低的直接原因。进而指出在开江古隆起-斜坡带有关的高陡构造带的两翼或两端的潜伏构造及向斜里的低缓背斜和低陡背斜,钻获高充满度石炭系气藏前景很好。

 
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