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烃源区
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  hydrocarbon source region
     ② Normal structures like arch stretching hydrocarbon source region should be main accumulating area;
     ②伸入烃源区的凸起等正向构造是天然气主要汇聚区;
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  “烃源区”译为未确定词的双语例句
     GIS acts as a "manager" and "analyst" in oil and gas exploration, which not only can manage mega-data, but also can assist oil and gas exploration decision support by acquiring related data from GIS database to make various complicated thematic analysis.
     油气的运移路径是连接烃源区和聚集区的纽带,基于GIS的油气运移路径模拟以GIS的栅格数据结构为基础,以油气成藏理论为指导,按照油气运移的机理,设计专门的算法来实现。
短句来源
     A large quantity of the oil which sourced from hydrocarbon source rocks migrated upward along slopes through darrier layers of faults, unconformities and sand bodies, and accumulated in Bamianhe structural belt, forming far-ranging distribution and various kinds of oil and gas reservoirs as a consequence of well trap-source conditions and space-time configuration relation, coupled with superior petroleum reservoir-forming conditions.
     源自烃源区的大量油气沿断层、不整合面及砂体等输导层向本区运移,由于本区具有良好的圈源条件和时空配置关系,成藏条件优越,形成了分布广泛、类型多样的隐蔽油藏。
短句来源
     Fault subsidence is characterized by easy dividing, clear differential uplift, multiple source materials and oil source areas, low thermal gradient and magmatic activity relatively weaker at the late period.
     断陷分割性强、差异升降明显、具有多物源、多烃源区、低地温梯度、后期岩浆活动相对较弱等特点。
短句来源
     Based on hydrocarbon expulsion modeling,synthesis to the latest research results and the actual situation in the carbonate source rock area,the paper regards the hydrocarbon expulsion with independent phase along microfracture as a repeating process of “pressure increase rock fracture hydrocarbon expulsion microfracture close”.
     在评述排烃模拟研究现状的基础上,综合排烃研究的最新成果及若干碳酸盐岩烃源区的实际地质情况,认为碳酸盐岩油气运移的主要机理为压力驱动下沿微裂缝的独立烃相排出。
短句来源
     Related source rocks in Tarim basin are selected to do thermal simulation and R o~ δ 13C 1 are established at the end of this article. The maturity of natural gas are calculated from R o~ δ 13C 1 relational expression. The calculation results are: R o of natural gases distributed in Tazhong major host belts is 1.4%, R o of natural gases distributed in the north slope of Tazhong uplift is 1.1%.
     对塔里木盆地相关气源岩进行热模拟实验 ,建立了Ro 与δ13 C1回归方程 ,应用该方程确定的塔中地区天然气成熟度为 :塔中主垒带上天然气的Ro 值约为 1 .4% ,塔中北斜坡的天然气Ro 值约为 1 .1 % ,烃源区均为塔中地区。
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  相似匹配句对
     HYDROCARBON RESOURCES IN THE GIANT GAS AREA IN WESTERN SOUTH CHINA SEA
     南海西部大气潜力
短句来源
     Hydrocarbon generating conditions of source rocks in Daqing region, Tarim basin.
     塔里木盆地大庆岩生条件
短句来源
     Progresses in the Research of Effective Source Rocks in Craton Area in Tarim Basin
     塔里木盆地台盆有效研究进展
短句来源
     The characteristics of the hydrocarbon source rocks in this region are analyzed using organic geochemistry methods.
     运用有机地球化学方法,分析了该岩的特征。
短句来源
     Study on Organic Maturity of Cambrian Source Rocks in Tarim Platform Area
     塔里木盆地台盆寒武系岩有机成熟度
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The basement of Hailaer basin is a Palaezoic fold zone formed after Siberian Plate & Sino-Korea Plate converged. Based on the existing fracture activity, a series of fault subsidence of Mcsozoic is developed. Development of fauit subsidence was undergone five evolution stages including initial tensional fault, strong tension, lensional rift,slow subsidence and backword shrieve.Six types of structural belts and three types of fault subsidence can be bivided in the basin. Fault subsidence is characterized by easy...

The basement of Hailaer basin is a Palaezoic fold zone formed after Siberian Plate & Sino-Korea Plate converged. Based on the existing fracture activity, a series of fault subsidence of Mcsozoic is developed. Development of fauit subsidence was undergone five evolution stages including initial tensional fault, strong tension, lensional rift,slow subsidence and backword shrieve.Six types of structural belts and three types of fault subsidence can be bivided in the basin. Fault subsidence is characterized by easy dividing, clear differential uplift, multiple source materials and oil source areas, low thermal gradient and magmatic activity relatively weaker at the late period. Formation condition of hydrocarbon of fault subsidence in the west of the basin is preferable to the condition in the east and reverse drag structure belt and slip faulted anticlinal belt is favourable to hydrocarbbon accumulation and commercial oil has been found in the basin.

海拉尔盆地的基底是西伯利亚板块和中朝板块敛合后形成的古生代褶皱带。中生代,在先存断裂活动基础上发育了一系列断陷。断陷发育经历了初始张裂、强烈拉张、拉张裂陷、缓慢沉降、回返萎缩五个演化阶段。可划分出三类断陷六类构造带。断陷分割性强、差异升降明显、具有多物源、多烃源区、低地温梯度、后期岩浆活动相对较弱等特点。并指出盆地西部断陷油气形成条件优于东部,逆牵引构造帝、滑陷式背斜带等有利于油气聚集,并已获工业油流。

Oil and gas enrichment area in basins offshore China are controlled by rich hydrocarbongenerating Paleogene depression。 Relating with large drape anticline,accompanied by largedelta sandstone reservoir or large biohermal carbonate reservoir and areal distribution of regional cap rock,large oil and gas fields could usually be formed.In continental deposit,oiland gas reservoirs are usually close to the source area。In marine sequences,if there are favorable carrier bed and areal cap rock,oil could migrate to a...

Oil and gas enrichment area in basins offshore China are controlled by rich hydrocarbongenerating Paleogene depression。 Relating with large drape anticline,accompanied by largedelta sandstone reservoir or large biohermal carbonate reservoir and areal distribution of regional cap rock,large oil and gas fields could usually be formed.In continental deposit,oiland gas reservoirs are usually close to the source area。In marine sequences,if there are favorable carrier bed and areal cap rock,oil could migrate to a long distance,and can form oilreservoirs from distant source areas。Coal measure units of the Paleogene spread in a largearea offshore China with abundant coal-generating gas potential.In west of South China Seathe Paleogene marine formations are very thick with fast depositional rate,high geothermalgradient,also has favorable gas-generating capacity。

中国沿海大陆架盆地油气富集区,受下第三系富生油凹陷控制,与其相联系的大型披复背斜,配以大型三角洲砂岩体或大型生物礁滩灰岩储层,及大面积分布的区域盖层,往往形成大油气田。油气田在陆州沉积中近烃源区分布,在海相地层中有良好运载层及大面积顶盖层的条件下,石油可长距离运移,在远离油源区也可形成油田。下第三系煤系地层在大陆架大面积分布,具有雄厚的煤成气潜力。南海西部有巨厚上第三系海相地层,沉积速度快,地温梯度高,也有优越的成气条件。

Luliang uplift zone in an inherited positive tectonic unit from marginal arcalong the north margin of Junggar plate during the Late Paleozoic,which is a long-term trendfor petroleum migration,To the west,Mahu source sag(Permian)is a major source area,Pri-mary Paleozoic volcanic reservoir formed at the close of Triassic, Triassic and Jurassic reser-voirs formed during the late Middle Jurassic to Early Cretaceous, secondary Paleozoic volcanic reservoir formed after the Late Cretaceous period. Volcanic rocks (particularly...

Luliang uplift zone in an inherited positive tectonic unit from marginal arcalong the north margin of Junggar plate during the Late Paleozoic,which is a long-term trendfor petroleum migration,To the west,Mahu source sag(Permian)is a major source area,Pri-mary Paleozoic volcanic reservoir formed at the close of Triassic, Triassic and Jurassic reser-voirs formed during the late Middle Jurassic to Early Cretaceous, secondary Paleozoic volcanic reservoir formed after the Late Cretaceous period. Volcanic rocks (particularly daciteand andesite),which have a good reservoir quality,are the major reservoir rock in this area,whereas clastic reservoir is well developed but with poor quality Upper Triassic is the re-gional sealing bed, acting as a barrier for hydrocarbon preservation, The western part ofsouth slope of Luliang uplift should be considered as the important exploration objective inthe future,because it is characterized by approaching source area,good reservoir and sealingconditions,richness in trap type,and high hydrocarbon potential.

陆梁隆起带是在晚古生代准噶尔板块北缘陆缘岛弧背景上发展起来的一个继承性正性构造单元,是油气运移的长期指向,西侧的玛湖二叠系生油凹陷是主要的烃源区。三叠纪末期是古生代火山岩的第一次成藏期,中侏罗世晚期至早白垩世为三叠、侏罗系油气藏成藏期,晚白垩世后是古生代火山岩的第二次成藏期。火山岩,尤其是钙碱系列的英安岩、安山岩,储层物性好。是本区的主要储集区;碎屑岩储层虽很发育,但普遍物性差。上三叠统是区域性油气盖层,对该区油气保存起着重要作用。陆-梁隆起南斜坡西段,紧临油源区,储盖条件好,圈闭类型多,含油气远景好,应作为今后重要的钻探地区。

 
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