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episodic tectonic movements
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  “episodic tectonic movements”译为未确定词的双语例句
     Matching with the episodic tectonic movements, the evolution of the slope-breaks is also multi-stage and episodic, and their scale is related to the range and intensity of tectonic movements.
     坡折带的演化规律与构造活动的阶段性演化或幕式构造作用相对应,也表现出多期性、幕式活动和差异性活动的特点,而且坡折带规模与构造活动大小有关.
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  相似匹配句对
     TECTONIC CHARACTERISTICS AND EPISODIC EVOLUTION OF THE NORTHERN FAULT
     松辽盆地北部断陷盆地构造特征与幕式演化
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     Episodic tectonic movement and evolutional character in Jianghan basin.
     江汉盆地幕式构造运动及其演化特征
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     Criticize and Tectonic
     批判与建构
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     Tectonic in Architecture
     论建筑中的结构造型
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     MECHANISM AND REGULARITY OF EPISODIC RESERVOIRING
     幕式成藏的机理和规律探讨
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Hot fluid activity within the crust is indeed the crustal fluidization,which is afrontier scientific subject emphasized and developed in the latest over ten years.Fluid is the most active geological agent within the crust where it can transmit energy and transfermaterial.Fluid action can affect and control directly tectonism,sedimentation,lithogene-sis,ore formation and other geological processes.The study on fluid action within thecrust may lead to the establishment of the completely new geoscience theory.Hydrocarbonmigration...

Hot fluid activity within the crust is indeed the crustal fluidization,which is afrontier scientific subject emphasized and developed in the latest over ten years.Fluid is the most active geological agent within the crust where it can transmit energy and transfermaterial.Fluid action can affect and control directly tectonism,sedimentation,lithogene-sis,ore formation and other geological processes.The study on fluid action within thecrust may lead to the establishment of the completely new geoscience theory.Hydrocarbonmigration belongs to hot fluid activity occurred in the sedimentary basins,which runsthrough each stage of hydrocarbon generation,migration,accumulation and dissilation,controls directly the formation of hydrocarbon reservoirs,affects tectionic activities andlithogenesis in sedimentary basins,Research resluts of hydrocarbon migration can be usedfor reference in understanding the fluid activity of crust.Discontinuous episodic expulsionmechanism of hydrocarbons indicates metamorphic fluid activity in the deep parts of crustin episodic manner,produce episodic tectonic movements.Taking the action of deep fluidactivity into account,it is necessary to re-evaluate inorganic origin,thermal degradationabout hydrocarbon generation and hot watermigration of hydrocarbons in the deep parts ofbasin。

地壳中的热流体活动实际就是地壳流体作用,是最近十多年来才被认识到并发展起来的前沿科学。地壳流体起着传输能量和搬运物质的作用,是地壳中最活跃的一种营力,直接影响和控制着整个地壳的构造、沉积、成岩和成矿等作用。通过对地壳流体的研究可能产生全新的地质科学理论。油气运移是发生在沉积盆地中的热流活动,它贯穿在整个油气的生成、运移、聚集和散失过程中,直接控制着油气藏的形成并影响着盆地中的构造活动和成岩作用。研究油气运移可以为研究整个地壳流体提供一个窗口和借鉴。不连续的幕式排烃机理可以使人们联想到地壳深部的变质流体也可能呈幕式活动并产生幕式的构造运动。在深部流体活动的作用下有必要对石油的无机成因学说、热降解机理和深盆热水运移等问题重新进行评估。

The oil and gas pools found in Bohai Bay Basin can be divided into four types, i.e., anticline pool, faulted block pool, unconformity pool and lithological pool. Their distribution is controlled by tectonic events. The structural styles of a basin determine the type and distribution of the pools, episodic tectonic movement controls their vertical superimposition, and tectonic migration result in their distribution differentiation horizontally.

渤海湾盆地已发现的油气藏可分为背斜型、断块型、不整合型和岩性型四大类,它们的分布受构造作用的控制。盆地构造样式决定着油气藏的类型和分布,构造作用的阶段性影响着油气藏的垂向叠置关系,构造迁移导致了油气藏分布的平面差异。

The Qiongdongnan basin involved from a fault basin into a downwarped basin .and is filled with very thick sediments. of this suite sediments, 14 sequences can be recognized in the Lower-upper Tertiary .with 6 sequences being formed in faulting stage and 8 being formed in down warping. In faulting stage .the de velopment of sequence was mainly controlled by episodic tectonic movement, and the sequence consists of coarse clastic sediments deposited in alluvial fan, river, lake, fan-delta and clastic littoral...

The Qiongdongnan basin involved from a fault basin into a downwarped basin .and is filled with very thick sediments. of this suite sediments, 14 sequences can be recognized in the Lower-upper Tertiary .with 6 sequences being formed in faulting stage and 8 being formed in down warping. In faulting stage .the de velopment of sequence was mainly controlled by episodic tectonic movement, and the sequence consists of coarse clastic sediments deposited in alluvial fan, river, lake, fan-delta and clastic littoral environments. In the down-warping stage,the formation of sequence was mainly controlled by global change of sea level .and the sequence is characteristic of typical passive continental margin and includes lower systern tracts. Pro gressive system tracts and high system tracts. The lower system tracts conslsts of basln botton fan. slope fan and submarine channel sediments,and progressive and high system tracts consist of delta system,clastic littoral system,carbonate platform reef system and neurotic shelf systems.

琼东南盆地的发展经历了由断陷到坳陷的演化过程,盆内充填了巨厚的沉积地层,该套地层在上、下第三系内可识别出14个层序,断陷期6个坳陷期8个。断陷期层序发育主要受控于幕式构造运动,层序由冲积扇、河流、湖泊、扇三角洲和碎屑滨岸体系沉积的粗碎屑岩组成。坳陷期层序发育主要受控于全球海平面变化并具有典型被动大陆边缘特征,低位域由企底扇、斜坡扇和海底水道沉积组成;海进体系域和高位体系域由三角洲、碎屑滨岸、碳酸盐台礁和浅海陆架体系沉积组成.

 
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