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天然气注入
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  “天然气注入”译为未确定词的双语例句
     The natural gas began to charge from Jidike to Kangcun stage that was the main time of inclusion formation.
     天然气注入开始于吉迪克末期—康村期 ,该阶段是包裹体形成的主要时期。
短句来源
     The characteristics of fluid inclusions in Lianyuan sag indicate that two episodes are involved in regard to formation time of gas reservoirs. The first episode for gas reservoir formation is early Triassic and the temperature ranges between 120.8~126.2℃, the second episode for gas reservoir formation is late Triassic, which proves to be the principal episode for gas reservoir formation in Lianyuan sag, and the temperature ranges between 154.4~169.7℃.
     流体包裹体特征反映出该区气藏成藏期有两期,即第一期天然气注入时温度120.8~126.2℃,对应成藏时间为早三叠世,第二期天然气注入时温度154.4~169.7℃,对应成藏时间为晚三叠世,其中主要成藏期为晚三叠世。
短句来源
  相似匹配句对
     On Natural Gas's Storage
     天然气的储存
短句来源
     Storage of Natural Gas
     天然气的储存
短句来源
     NUMERICAL SIMULATION OF WATER-GAS ALTERNATE INJECTION FOR NATURAL GAS DRIVE
     天然气驱水气交替注入数值模拟研究
短句来源
     MAIN GAS SOURCES AND GAS CHARGE HISTORY IN YINGGEHAI-QIONGDONGNAN REGION
     莺-琼气区天然气主气源及注入史分析
短句来源
     the injection pressure is controlled carefully.
     控制注入压力。
短句来源
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  natural gas injection
All of the furnace sections contain multiple ports for sample extraction,observations, and overfire air or natural gas injection.
      
Example of sound spectrum during natural gas injection at flow rate 50 cc/min is shown in Figure 3.
      
Furthermore, the natural gas injection provides the highest recovery than carbon dioxide and nitrogen.
      
There are four identical trains designed for natural gas injection service.
      


In this paper, the author researched diagenesis and organic inclusion in reservoir. In this area, organic inclusions were mostly formed by recrystalization and metaspmasis and with various phases. They distributed chiefly in dissolved seams and pores in quartz grains and not in structure slot. The organic inclusion abundance in Upper Triassic was more than that in Shaximiao Formation. The homogenization temperature of organic inclusion was between 100℃ and 110℃ in the second interval of Xujiahe Formation and...

In this paper, the author researched diagenesis and organic inclusion in reservoir. In this area, organic inclusions were mostly formed by recrystalization and metaspmasis and with various phases. They distributed chiefly in dissolved seams and pores in quartz grains and not in structure slot. The organic inclusion abundance in Upper Triassic was more than that in Shaximiao Formation. The homogenization temperature of organic inclusion was between 100℃ and 110℃ in the second interval of Xujiahe Formation and between 90℃ and 100℃ in Shaximiao Formation. The second segment gas reservoir of Xujiahe Formation was formed earlier and underwent the course early from small charge to large charge and late again from adjustment to small charge. The gas reservoir of Shaximiao Formation was formed in the course of Xishan Tectonic Movement

通过储集层成岩作用与有机包裹体的研究认为 ,研究区储集层有机包裹体主要通过交代和重结晶作用而形成 ,有各种相态形式 ,主要分布在石英颗粒内溶蚀缝或孔隙中 ,构造裂缝中基本未见有机包裹体。上三叠统储集层包裹体丰度明显高于侏罗系沙溪庙组。香二气藏砂岩有机包裹体均一温度主峰在 10 0~ 110℃ ;沙溪庙气藏砂岩有机包裹体均一温度主峰在 90~ 10 0℃。香二气藏形成时间早 ,经历了印支期少量注入到印支期末—喜山早期大量注入 ,再到喜山晚期调整、部分注入的过程。沙溪庙气藏天然气注入则主要发生于喜山运动期。

Natural gas in Upper Ordovician system might be related to Upper Paleozoic sources by showing some similar geochemical criterion to coal bearing units in former series. According to component and isotopic ratios of gaseous alkanes, the gas, which was drilled by Well Wushen 1 on the western Wumaying buried hill, might be experienced multi stage charging. The accumulation of gas pool in western Wumaying buried hill was evidently influenced by succeeding tectonic evolution. And natural gas in Ordovician system...

Natural gas in Upper Ordovician system might be related to Upper Paleozoic sources by showing some similar geochemical criterion to coal bearing units in former series. According to component and isotopic ratios of gaseous alkanes, the gas, which was drilled by Well Wushen 1 on the western Wumaying buried hill, might be experienced multi stage charging. The accumulation of gas pool in western Wumaying buried hill was evidently influenced by succeeding tectonic evolution. And natural gas in Ordovician system in Well Wushen 1 was newly gathered through remigration of hydrocarbon which accumulated during latter Mesozoic era, after the former hydrocarbon trap being altered with dramatic faulted block rotation during latter Oligocene. The forming time of which was inferred roughly during latter Tertiary according to fluid inclusion datum in cores of Wushen 1, delayed than critical moment of Paleozoic petroleum system in Wumaying district. Hydrocarbon generating history of Wumaying buried hill was discussed in this paper based on analyzing process of ancient trap reconstruction by using paleostructure restoration technique. According to analyses, hydrocarbon in Ordovician carbonate reservoir in Wumaying buried hill has undergone complicated remigration from northeastern to southwestern buried hill, and hydrocarbon distribution changed from eastern condensate relic to western "wet gas", owing to limitation of heterosphere of carbonate reservoir.

乌马营潜山西部乌深 1井在奥陶系顶部钻遇的天然气地球化学特点与黄骅坳陷南区上古生界煤系烃源岩相近 ,证实两者具有亲缘关系 ,并有较明显的多阶混源特征。乌深 1井区天然气注入期为晚第三纪 ,远晚于烃源岩成熟的晚中生代。在分析乌马营潜山古圈闭改造历史的基础上 ,研究了潜山油气的充注、改造过程 ,推测潜山油气曾经历由东向西迁移和凝析油裂解的过程 ,乌深 1井区天然气藏应属于晚中生代形成的古油气藏中的烃类在第三纪晚期再迁移分配的产物 ,现今乌马营潜山可能具有东部为凝析油气、西侧为湿气的油气分布规律。

On the basis of the theory of petroleum system,t he geochemical mode of gas reservoir formation in Carboniferous in East Sichuan Basin was studied by applying gas reservoir geochemical methods.Through contrast ing the aromatic hydrocarbon fraction of reservoir bitumen in carboniferous wit h the carbonaceous shales in Silurian and Lower Permian in East Sichuan,it was p roved that the reservoir bitumen in Carboniferous is of a strong affinity with L ower Silurian.The Carboniferous formation water and reservoir...

On the basis of the theory of petroleum system,t he geochemical mode of gas reservoir formation in Carboniferous in East Sichuan Basin was studied by applying gas reservoir geochemical methods.Through contrast ing the aromatic hydrocarbon fraction of reservoir bitumen in carboniferous wit h the carbonaceous shales in Silurian and Lower Permian in East Sichuan,it was p roved that the reservoir bitumen in Carboniferous is of a strong affinity with L ower Silurian.The Carboniferous formation water and reservoir rocks suffered thr ee evolution stages,i.e. sedimentation,denudation and deep burial stages and the gas reservoir formation was suffered roughly the same two stages,i.e Indo Chin e se~Yanshan epoch was the main formation stage of ancient oil reservoirs and Him alayan epoch was that of gas reservoirs.In the paper,according to natural gas ge ochemical characteristics,the gas migration direction is discussed and it is pro posed that the gas reservoirs with an early charging time are in the Dachiganjin g,Gaofengchang,Xiangguosi and Datianchi structures in East Sichuan,the others be ing relatively later,in which the gas charging sequence in Dachiganjing structur e was the Wanshunchang,Diaozhongba,Longtou and Mopanchang highs successively.Thr ough studying at present it is shown that there were three gas migration directi ons in Carboniferous,i.e. the gas was migrated from southwest to northeast and f rom west to east in the west part of Kaijiang ancient uplift and the gas in the southeast part of the ancient uplift might come from the direction of Shizhu synclinori um.Finally it is pointed out that the gas accumulation Carboniferous was control led by the Indo Chinese~Yanshan epoch Kaijiang ancient uplift;the traps formed during Himalayan epoch played an adjustment role in gas reservoir formation;and the next beneficial exploration tracts are put forward from the point of view of gas reservoir geochemistry,which has a guiding significance for deepening Carbo niferous exploration.

本文根据含油气系统理论 ,采用气藏地球化学方法 ,研究了四川盆地东部石炭系天然气成藏的地球化学模式。应用储层沥青中的芳香烃馏份进行了川东石炭系与志留系和下二叠统碳质页岩的特征对比 ,证实了石炭系的储层沥青与下志留统亲缘关系密切。石炭系地层水和储集岩经历了沉积、暴露剥蚀和深埋藏三个演化时期 ,天然气主要经历了大致相同的两次成藏过程 ,印支—燕山期为古油藏的主要成藏期 ,喜山期为天然气的主要成藏期。应用天然气地球化学特征探索了石炭系天然气的运移方向 ,提出了川东地区注入时间较早的气藏有大池干井、高峰场、相国寺和大天池等 ,其他气藏相对较晚 ,其中大池干井构造天然气的注入顺序依次为万顺场、吊钟坝、龙头和磨盘场。目前研究表明 ,石炭系天然气存在 3个运移方向 ,即开江古隆起西部由南西向北东和由西向东两个方向 ,开江古隆起东南部则可能有石柱复向斜方向运移来的天然气。指出石炭系天然气的聚集受开江印支—燕山期古隆起的控制 ,喜山运动形成的圈闭对天然气成藏具有调整作用 ,从气藏地球化学角度提出了下步勘探较为有利的区块 ,对深化石炭系勘探具有指导意义

 
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