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   断层系统 在 石油天然气工业 分类中 的翻译结果: 查询用时:0.374秒
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断层系统
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  fault system
    The previous research showed that oil and gas pools of upper Tertiary system have close relationship with distribution and activity of fault system.
    初步的研究表明新近系油气成藏与断层系统的分布和活动关系密切。
短句来源
    Since Late Cretaceous, the evolution of extensional structural style could be classified into two orders: the evolution of domino-style normal faults to the listric or ramp-flat normal fault system in Lishui Sag;
    晚白垩世以来的伸展构造样式的演变大致可归纳为两个序列:丽水凹陷的断裂构造系统演变是由多米诺正断层系统演变为铲式或坡坪式正断层系统
短句来源
    The distribution of oil and gas is studied and it is discovered that reservoirs mainly distribute in antithetic nose or fault-block traps on both sides of the big fault. The distribution was controlled by source rock distribution,caprock distribution and fault system. Reserve abundance was subjected to sedimentary facies.
    本次工作对油气的分布规律进行深入研究,发现油气藏主要分布在大断层两侧的反向断鼻或断块圈闭内,分布规律主要受烃源岩分布、盖层分布以及断层系统的控制,储量丰度受沉积相的影响,这就为下步滚动勘探开发提供了方向。
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  “断层系统”译为未确定词的双语例句
    the evolution of groben-horst system controlled bynonrotational planar normal faults to listric or ramp flat normal fault in Jiaojiang Sag.
    椒江凹陷的断裂系统的演变是由非旋转的平面式正断层控制的地堑-地垒系统演变为铲式或坡坪式正断层系统
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  fault system
The Yanshan orogenic belt fault system deflected from an EW to a NE direction, then to a NNE direction during the Indo-Chinese epoch-Yanshanian epoch.
      
The thrust-nappe strength of the Qinling-Dabie orogenic belt fault system showed the tendency that the strength was greater in the south and east, but weaker in the north and west.
      
This fault system faulted in the east and folded in the west from the Indo-Chinese epoch to the early Yanshanian epoch.
      
The Tanlu fault system caused the basin to migrate from west to east and south to north.
      
The migration regularity of the East China Sea shelf basin-Okinawa trough fault system shows that the formation age became younger in the west.
      
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mploying the fractal and renormalizational group theories,the essay has established fractal percolation inodels of the rift system umder complex geological conditions,The computation of the fractal dimensions of the actual fault systems reveals that faults are closely related to the connection and per-colation between developed rifts,which may solve some difficult problems in exploring and opening up newoil-gas fields.

运用分形与重正化群理论,建立了复杂地质条件下裂缝系统的分形渗流模型.计算了实际断层系统的分维后揭示了断层与裂缝发育带以及储集空间的连通性与渗流性的密切联系.解决了勘探开发中的某些疑难问题.

The tectonic evolution of Bohai Bay basin province can be divided into two stages of rifting and post-rifting. and basically completed a cycle of taphrogenesis.The riftingstange during Paleogene is composed of three extensional periods which correspond theformations of Kongdian and 4th number of Shahejie,3rd number of Shahejie,and 2nd-1stnumbers of Shahejie and Dongying. There are obvious disparity in tectonic styles andkenematics between the three extensional periods.The evolution of extensional tectonics caninclude...

The tectonic evolution of Bohai Bay basin province can be divided into two stages of rifting and post-rifting. and basically completed a cycle of taphrogenesis.The riftingstange during Paleogene is composed of three extensional periods which correspond theformations of Kongdian and 4th number of Shahejie,3rd number of Shahejie,and 2nd-1stnumbers of Shahejie and Dongying. There are obvious disparity in tectonic styles andkenematics between the three extensional periods.The evolution of extensional tectonics caninclude 2 paths:(1) from domino systems to listric systems and ramp-flat normal faultsystems:(2)from non-rotation normal fault systems to listric systems and ramp-flat normalfault systems.

渤海湾新生代盆地经历了早第三纪裂陷沉降和晚期第三纪-第四纪后裂陷热沉降两个阶段。基本完成了一个完整的裂陷作用旋回。早第三纪裂陷作用包括三个裂陷伸展期,它们分别相当于孔店级-沙四段、沙三段、沙二段-沙一段-东营组等三套地层的发育时期,各裂陷伸展期的构造运动学特征有一定的差异,反映在伸展构造样式的变化上,大致可归纳为由多米诺式正断层系统向铲式正断层系统、坡坪式正断层系统的演化序列及由非旋转平面式正断层系统向铲式正断层系统、坡坪式正断层系统的演化序列两个演化模式。

The basic structural style of lishui-Jiaojiang Say is extensional structure. The extensional movement happened in Late Cretaceous-Paleocene was charaterized by episodic progrssive extension. Different parts of extensionalstructures in the study area have different characters: the extensional rates change for small in the North to big in the south, and the period largest extension of in the south part was earler than that in the North part. Since Late Cretaceous, the evolution of extensional structural style...

The basic structural style of lishui-Jiaojiang Say is extensional structure. The extensional movement happened in Late Cretaceous-Paleocene was charaterized by episodic progrssive extension. Different parts of extensionalstructures in the study area have different characters: the extensional rates change for small in the North to big in the south, and the period largest extension of in the south part was earler than that in the North part. Since Late Cretaceous, the evolution of extensional structural style could be classified into two orders: the evolution of domino-style normal faults to the listric or ramp-flat normal fault system in Lishui Sag; the evolution of groben-horst system controlled bynonrotational planar normal faults to listric or ramp flat normal fault in Jiaojiang Sag. The extensional movement controlled the distribution of sedimentary sequences and systems, and the spatial distribution of source-reservoir-cap rockassemblage. The fault basin architecture can be divided into three-layers structure, and also, oil and gas are distributedin three lagers. The oil-gas pools of Lishui-Jiaojiang Sag are distributed mainly in the rift-depressed sequence. The oilgas pools of self-generation and self-reservoiring should be the main target of exploration in Lishui-Jiaojiang Sag.

丽水、椒江凹陷基本的构造样式是伸展构造,伸展运动主要发生在晚白垩世-早第三纪古新世,伸展运动过程具“幕式”渐进伸展的特点。研究区不同构造部位其伸展特征不同,表现为伸展率南大北小、最大伸展期南早北晚的特征。晚白垩世以来的伸展构造样式的演变大致可归纳为两个序列:丽水凹陷的断裂构造系统演变是由多米诺正断层系统演变为铲式或坡坪式正断层系统;椒江凹陷的断裂系统的演变是由非旋转的平面式正断层控制的地堑-地垒系统演变为铲式或坡坪式正断层系统。伸展运动控制着沉积序列、沉积体系的分布,从而控制着生储盖组合的空间展布。裂陷盆地在结构上可以归纳为三层结构(即基底、裂陷期层序和裂陷后层序),油气呈三层楼式分布。丽水、椒江凹陷地区主要的油气分布在裂陷期层序本身,自生自储式油气藏应是寻找的主要目标。

 
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