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   episodic tectonic 在 地质学 分类中 的翻译结果: 查询用时:0.553秒
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episodic tectonic
相关语句
  幕式构造
    Sequence Stratigraphic Framework of Celaomiao Basin and Its Episodic Tectonic Evolution
    测老庙盆地层序地层格架与其幕式构造演化
短句来源
    The difference of types of rocks,chemical constitution and distribution characteristics is the result of episodic tectonic evolution in depressed stage.
    认为松辽盆地断陷期火山岩区域上为兴安岭群火山岩的一部分 ,纵向上可以划分为火石岭组和营城组两套火山岩旋回 ,它们在岩石类型、化学成分和分布规律上的差异 ,是断陷期幕式构造演化的反映。
短句来源
    The episodic tectonic activity made faults open and close alternatively;
    多幕式构造活动使断层开启与封闭交替进行 ;
短句来源
  “episodic tectonic”译为未确定词的双语例句
    The multiple episodic tectonic events and volcanic activities resulted in complex structural style, reservoir and oil/gas pool distribution.
    但区内驾掌寺断裂的多期不同性质的构造活动及其伴随的火山岩作用造成构造样式、储层发育及油藏分布十分复杂。
短句来源
    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
短句来源
    Episodic tectonic uplifts of Qinghai-Tibetan Plateau represent one of the most significant geologic events in the late Cenozoic, strongly imprinted on regional climate changes in and around the Plateau, and even on a global scale.
    柴达木盆地作为高原内部的一个巨型山间盆地,发育了连续、完整、巨厚的第四纪沉积,高分辨率的湖泊沉积物古气候变化研究对于加深高原内部气候变化历史的认识,探讨高原隆升在中更新世转型过程中的作用具有十分重要的意义。
短句来源
    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.
    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。
短句来源
    Genesis analysis suggests that the development of parasequences in the Dongying Formation was controlled by the 4th order episodic tectonic subsidence and the boundary of a parasequence is an abrupt accommodation changing surface in a view point of accommodation evolution.
    成因分析表明,东营组准层序的特征和形成受四级构造幕沉降作用控制,从沉积空间演化角度看,准层序边界是一个沉积空间突变面。
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  episodic tectonic
The multiple episodes of mineralization are coincident with episodic tectonic reactivations and associated magmatism along the northern margin of the North China craton.
      
The result shows that the mixed mantle convection model is able to simulate the episodic tectonic evolution of the Earth.
      


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。

Based on the sedimentary study, the present paper discusses the occurrence of large Ordos depositional basin during Early-Middle Jurassic including the present Ordos basin and Ningwu and Datong districts in Shanxi. Paleogeography of the original large Ordos basin was reconstructed and expounded in terms of the four deposition stages. The study on sediment filling in the basin reveales the episodic tectonic activity of downwarping, uplifting and redownwarping and the migration of depocenters, and interpretes...

Based on the sedimentary study, the present paper discusses the occurrence of large Ordos depositional basin during Early-Middle Jurassic including the present Ordos basin and Ningwu and Datong districts in Shanxi. Paleogeography of the original large Ordos basin was reconstructed and expounded in terms of the four deposition stages. The study on sediment filling in the basin reveales the episodic tectonic activity of downwarping, uplifting and redownwarping and the migration of depocenters, and interpretes the tectonic setting for basin formation and evolution. 

ReconstructionofEarly-MiddleJurasicLargeOrdosBasinandTectonicSeting*ChengShoutianFuXuehongHuangYanqiuFacultyofEarthResources,...

This paper mainly analyses the characteristics of the faults of the north and middle area in Huanghua subbasin and Qikou depression. According to the two schemetic maps of the faults from 3D seismic data, the extensional faults in this area trend mainly NE, NEE, EW, and minor other secondary direction. The episodic tectonic deformation development led to sharp differences among the strikes of the faults formed during different stages in south part of Qikou depression. The strikes of extensional faults...

This paper mainly analyses the characteristics of the faults of the north and middle area in Huanghua subbasin and Qikou depression. According to the two schemetic maps of the faults from 3D seismic data, the extensional faults in this area trend mainly NE, NEE, EW, and minor other secondary direction. The episodic tectonic deformation development led to sharp differences among the strikes of the faults formed during different stages in south part of Qikou depression. The strikes of extensional faults developed in different areas have preferential direction. Moreover, the faults developed in transverse transfer zones are extensional and its trends are pendicular to master fault. Based on paleostress analysis of the faults, the extension of Huanghua subbasin and Qikou depression are 3D radial and the transverse transfer zones are characterized also by 3D radial extension without transverse compression and strike slip shearing.

主要分析了黄骅坳陷中北区和歧口凹陷断裂构造特征。根据三维地震资料编制的T4和T0断裂纲要图表明,研究区断裂为伸展正断层,以NE向、NNE向和EW向断裂为主。在不同时期,歧口凹陷断层走向发生明显变化,由沙一下段NE向变为上第三系的近EW向。在不同地段,伸展断裂具有不同的优势方向。横向变换带上发育的断裂也为伸展断裂,具有与主断层垂直相交的方向。通过对断裂古应力分析,黄骅盆地是伸展型盆地,推测其伸展作用为三维放射状,横向变换带也具有三维伸展特征,不存在横向挤压和走滑剪切作用。

 
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