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entered the peak
相关语句
  进入生油高峰
     The type Ⅰ hydrocarbon generation sag which has entered the peak stage is favorable for hydrocarbon (generation and discharge. 2)Based on mudstone) compression curve and clay mineral change, the rapid compression stage is the most favorable era for hydrocarbon discharge(primary migration).
     进入生油高峰阶段的Ⅰ类生油凹陷有良好的生烃与排烃条件,具有形成工业价值油气藏的能力; 2)根据泥岩压实曲线和粘土矿物变化等资料分析认为,快速压实阶段是排烃(油气初次运移)的最佳时期;
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  “entered the peak”译为未确定词的双语例句
     Since the year of 2003, China's household appliances have entered the peak of obsolescence, which discards approximately more than 30 million every year.
     自2003年起,我国的家用电器已进入报废的高峰期,每年约有3000多万台家电被淘汰。
短句来源
     In Indosinian,tectonic framework in this area is characterized by large uplift and large depression and the source rocks have entered the peak hydrocarbon generation stage,resulting in the early enrichment of hydrocarbons in the uplifted area.
     印支期区内构造格局以大隆大坳为特征,是区内烃源岩的生烃高峰期,形成了隆起区早期的油气富集。
短句来源
     Before the deposition of Quantou Fm,Shahezi and Huoshiling Fins source rocks would have entered the peak of gas generation.
     泉头组沉积前,沙河子组及火石岭组烃源岩已进入生气高峰。
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  相似匹配句对
     China has be entered into the WTO.
     中国已加入WTO。
短句来源
     China has entered into WTO ;
     中国已加入WTO ;
短句来源
     China has entered WTO.
     我国已加入WTO。
短句来源
     The Thought about Entered into WTO
     面对入世的思考——试论加入世贸对中国非织造布工业的影响
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  entered the peak
Finally, note that station BRIB has turned black, indicating that it has entered the peak ground motion window.
      


Based on the structural growing history, analysis of oil source rocks and crude oil geochemical features such as crude oil physical property and characteristics of nitrogen bearing and phenol compounds, a preliminary analysis is carried out on oil and gas migration and pool forming history of CⅢ oil set in Tazhong area It is deduced comprehensively that there may possibly be three pool forming periods in Carboniferous system:①the source rocks of Cambrian and lower Ordovician begin to enter the peak...

Based on the structural growing history, analysis of oil source rocks and crude oil geochemical features such as crude oil physical property and characteristics of nitrogen bearing and phenol compounds, a preliminary analysis is carried out on oil and gas migration and pool forming history of CⅢ oil set in Tazhong area It is deduced comprehensively that there may possibly be three pool forming periods in Carboniferous system:①the source rocks of Cambrian and lower Ordovician begin to enter the peak of hydrocarbon generation and expulsion in Permian period, thus leading to the formation of Tazhong 4 oilfield The reservoir begins to redistribute in Cretaceous period because of Yanshan tectonic movement The fault becomes active and the reservoir formed earlier is damaged by tilting of the formation and some geochemical process, such as biodegradation and water washing taking place in the reservoir;②in the period of Yanshan and Xishan Orogenesis, especially in 100 Ma after the Cretaceous period the marly source rocks reach the peak of hydrocarbon generation and expulsion in middle lower Ordovician system The hydrocarbon migrates from the west to east and into the traps of TZ10, TZ11, TZ4 and mixes with the hydrocarbon remained in reservoir early;③at the same time or later time (mainly after the Xishan tectonic movement), the source rocks at different zones of O 2+3 go into the high mature stage and form natural gas, light oil is from the east to west and comes into Tazhong 1 and Tazhong 4 oilfields because of Tertiary megasedimentation Because of oil and gas migration and mixing with oil from different sources, thus differences are caused between the east and west with the existence of various reservoirs and all kinds of oil and gas distribution in Tazhong area

根据该区构造发育史、油源区分析、原油的地球化学特征如原油物性特征、含氮和酚类化合物特征等 ,对塔中地区 C 油组的油气运移和成藏史进行了初步分析。综合推断 ,该区石炭系可能存在三次成藏期 :1在二叠纪 ,寒武系下奥陶统源岩进入生烃和排烃的高峰阶段 ,并聚集形成 TZ4油田。在白垩纪 ,受燕山构造运动影响 ,油气藏重新分配 ,断层开启 ,地层的翘倾作用使早期油藏遭到破坏 ,油藏经历水淹和生物降解作用 ;2燕山喜山期 ,特别是白垩纪以后的 1 0 0 Ma内 ,中、下奥陶统泥灰岩源岩达到了生、排烃高峰 ,生成的烃类自西向东运移至 TZ1 0 ,TZ1 1 ,TZ4等圈闭 ,并与早期残余在油藏中的烃类混合。 3与此同时或较晚 ,由于沉积了巨厚的第三系 ,中、上奥陶统不同带的源岩及寒武系下奥陶统源岩在较高成熟度条件下形成的天然气、轻质油 ,自东向西进入 TZ1和 TZ4油田。由于以上三期的油气注入及不同生源的油气混合 ,从而造成了塔中地区石炭系油藏存在东西差异及多种油藏并存的油气分布面貌。

By using the method of biomechanics, the author finds out that in the distance of 7 meter curved arc peak with the condition of high speed skating, all skaters do not have perfect step. Most skaters come into this area by right holding on one leg, and leave here by holding on the double legs. Judging from the body posture, squatting posture is low, and upper body is high. All skaters enter the peak of arc with lower upper body posture, and leave with higher posture. The smaller the obliquity of body...

By using the method of biomechanics, the author finds out that in the distance of 7 meter curved arc peak with the condition of high speed skating, all skaters do not have perfect step. Most skaters come into this area by right holding on one leg, and leave here by holding on the double legs. Judging from the body posture, squatting posture is low, and upper body is high. All skaters enter the peak of arc with lower upper body posture, and leave with higher posture. The smaller the obliquity of body and angle of kicking, the faster the speed is. As far as the average speed at arc peak of curved lane, female skaters' average speed of 500 m is faster than that of 1000 m, and at the same time, the averagespeed at the stage of holding on one leg is faster than that of holding on the double leg. The longitudinal kicking of single holding on one leg is the main driving force source of acceleration at the curved lane. Doing a side-kicking at the stage of holding on the double legs is still the important means of promoting speed.

对运动员的比赛动作进行了运动生物力学分析 ,得知在弯道弧顶 7m长的距离内 ,在高速滑跑的情况下 ,所有运动员都没有完整的单步 ,多数运动员以右单支撑进入该区域 ,以双支撑离开该区域。从身体姿势看 ,蹲屈姿势低 ,上体姿势高。所有运动员都以较低的上体姿势进入弧顶段而以较高姿势离开。身体倾角和蹬冰角越小 ,滑速越快。从弯道弧顶段的平均速度来看 ,女运动员 5 0 0 m的平均速度比 10 0 0 m要快 ,单支撑蹬冰阶段的平均速度比双支撑蹬冰阶段快 ,单支撑阶段的纵向蹬冰是弯道增速的主要动力来源。双支撑阶段的侧蹬冰仍是提高弯道速度的重要手段。双支撑阶段浮腿着冰较早 ,而蹬冰腿迟迟不进行侧蹬冰是导致速度下降的主要原因

Based on analyses of data including neotectonics earthquake,drilling,seismic,stratigraphy,structural features and satellite remote sensing,it is believed that Himalayan movement can be divided into three episodes in Songliao basin.The first and third episodes have mainly been affected by the Indian plate and result in NE SW regional principal compressive stress;while the second episode has mainly been affected by the Pacific plate and has given rise to NW SE or nearly W E regional principal compressive stress;the...

Based on analyses of data including neotectonics earthquake,drilling,seismic,stratigraphy,structural features and satellite remote sensing,it is believed that Himalayan movement can be divided into three episodes in Songliao basin.The first and third episodes have mainly been affected by the Indian plate and result in NE SW regional principal compressive stress;while the second episode has mainly been affected by the Pacific plate and has given rise to NW SE or nearly W E regional principal compressive stress;the NW tectonism in the third episode has important effects on the early formed structural traps and the remigration and accumulation of hydrocarbons in those traps.The Tertiary in Songliao basin was deposited in a compresso depressed basin,characterized by limited distribution of formations,coarse grained clastics,and the uplifted area to be the provenance.Analysis of the Tertiary tectonic deformation ellipsoid in Songliao basin reveals that the direction of compressional stress turned from N S to nearly W E in the middle and late Paleogene(since 43?Ma).Under compression at the end of Cretaceous,the moderate depth and shallow structures grew progressively and provided good traps for hydrocarbon accumulation.The moderate depth and shallow faults are the result of superposition of multistage fracturing,and faults formed in different stages have different extending characteristics.NE and NNE faults were mainly developed under nearly E W extensional stress during the deposition of Qingshankou Formation;only the nearly E W faults were developed under nearly S N extensional stress at the end of deposition of Yaojia Formation;and the NNW and NW faults were mainly developed under left lateral compresso shear stress after the deposition of Mingshui Formation.Structural inversion at the end of deposition of Mingshui Formation has resulted in the Songliao basin entering the peak of hydrocarbon generation;and changes of direction of compressional force has resulted in the opening of shallow and moderate depth old faults with different directions,which would consist of multi directional migration pathways.The compressional setting would not only provide pathways and reservoirs for hydrocarbon migration and accumulation,but would also be favorable for generation and preservation of hydrocarbons,thus realizing good matching of hydrocarbon generation,migration,accumulation and preservation.

通过对新构造运动、天然地震、钻探、人工地震、地层、构造形迹、卫星遥感等资料分析 ,认为喜山运动在松辽盆地可分为 3幕 ;第一、第三幕运动主要受印度板块影响 ,产生的区域主压应力为北东 -南西向 ;第二幕运动主要受太平洋板块影响 ,产生的区域主压应力方向为北西 -南东或近东西向 ;第三幕所产生的北西向构造作用对早期形成的北东向构造圈闭及其中的油气再运移和聚集有重要影响。松辽盆地第三系为压陷盆地沉积 ,表现为地层分布局限、充填碎屑粗、隆起区可作为物源区。松辽盆地第三系构造变形椭球体反映在老第三系沉积中晚期 (4 3Ma以来 )挤压应力方向发生了由南北到近东西向的变化。在白垩纪末的挤压作用下 ,中浅层构造不断壮大 ,为油气聚集提供了良好的圈闭。中浅层断层为多期断裂活动的叠加产物 ,不同时期的断层具有各自的延伸特征 :青山口组沉积期在近东西向伸展应力作用下 ,主要发育北东、北北东向断层 ;姚家组沉积末在近南北向伸展应力作用下 ,只发育近东西向断层 ;明水组沉积期以后在近南北向左行压扭应力作用下 ,主要发育北北西、北西向断层。明水组沉积末期的构造反转使松辽盆地开始进入生烃高峰期 ,挤压力方向的改变导致了中浅层不同方向的...

通过对新构造运动、天然地震、钻探、人工地震、地层、构造形迹、卫星遥感等资料分析 ,认为喜山运动在松辽盆地可分为 3幕 ;第一、第三幕运动主要受印度板块影响 ,产生的区域主压应力为北东 -南西向 ;第二幕运动主要受太平洋板块影响 ,产生的区域主压应力方向为北西 -南东或近东西向 ;第三幕所产生的北西向构造作用对早期形成的北东向构造圈闭及其中的油气再运移和聚集有重要影响。松辽盆地第三系为压陷盆地沉积 ,表现为地层分布局限、充填碎屑粗、隆起区可作为物源区。松辽盆地第三系构造变形椭球体反映在老第三系沉积中晚期 (4 3Ma以来 )挤压应力方向发生了由南北到近东西向的变化。在白垩纪末的挤压作用下 ,中浅层构造不断壮大 ,为油气聚集提供了良好的圈闭。中浅层断层为多期断裂活动的叠加产物 ,不同时期的断层具有各自的延伸特征 :青山口组沉积期在近东西向伸展应力作用下 ,主要发育北东、北北东向断层 ;姚家组沉积末在近南北向伸展应力作用下 ,只发育近东西向断层 ;明水组沉积期以后在近南北向左行压扭应力作用下 ,主要发育北北西、北西向断层。明水组沉积末期的构造反转使松辽盆地开始进入生烃高峰期 ,挤压力方向的改变导致了中浅层不同方向的老断层开启 ,形成了多方位的油气运移通道。挤压背景

 
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