构造沉降的英文

• tectonic descent
• tectonic subsidence

• "构造"英文翻译    structure; construction; con ...
• "沉降"英文翻译    subside; settle
• "大地构造沉降" 英文翻译 :    geotectonic subsidence
• "构造沉降部分" 英文翻译 :    structural saddle
• "构造沉降作用" 英文翻译 :    tectonic subsidence
• "构造沉没" 英文翻译 :    tectonic merging
• "构造沉积演化" 英文翻译 :    tectono-sedimentary evolution
• "火山构造沉陷" 英文翻译 :    volcano-tectonic subsidence
• "沉降" 英文翻译 :    1.(沉淀, 沉积, 沉陷) subside; settle 地面沉降 earth subsidence2.[地] sedimentation; (地基在建筑物荷重下发生的竖向变形) settlement
• "构造" 英文翻译 :    structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constitution; build; formation 句子构造 sentence construction; 这建筑构造奇异。 the building was of bizarre construction. 医生研究人体构造。 doctors study the structure of the human body.; 构造层 tectonosphere; 构造带 tectonic zone; 构造地震 tectonic earthquake; 构造地质学 geotectonics; tectonic geology; tectonics; structural geology; 构造风格 structural style; 构造复合 compounding of structures; 构造格局 tectonic framework; 构造谷 [地质学] structural valley; 构造结构 structural texture; 构造陆地 [地质学] tectonic land; 构造论 constructionism; 构造体系 tectonic system; structural system; 构造图 [地质学] constructional drawing; structure map; tectonic map; structure diagram; 构造型式 tectonic type; tectonic patterns; 构造学 tectonics; 构造序次 structural generation; 构造要素 structural element; 构造异常 structural anomaly; 构造原理 aufbauprinciple; 构造运动 tectonic movement; tectogenesis; 构造转向 [地质学] vergence; 构造作用 tectonism; 构造作用力 tectonic force
• "波(沉降)" 英文翻译 :    borros point
• "沉积；沉降" 英文翻译 :    deposition
• "沉降（作用）" 英文翻译 :    sedimentation
• "沉降，沉积" 英文翻译 :    sedimentation
• "沉降；地陷" 英文翻译 :    settlement
• "沉降；下垂" 英文翻译 :    sagging
• "沉降板" 英文翻译 :    diving plate
• "沉降比" 英文翻译 :    settlement factor; settling ratio
• "沉降槽" 英文翻译 :    cylindrical settler; hydroseparator; sedimentation cell; sedimentation tank; settlerstorer; settling ark; settling tank; settling vat; settling vessel; spin bath; subsider; thickener
• "沉降层" 英文翻译 :    sediment bed
• "沉降差" 英文翻译 :    differential settlement
• "沉降池" 英文翻译 :    sediment trap; sedimentation basin; sedimentation pond; sedimentation tank; settlerstorer; settling basin; settling bower; settling bowl; settling pit; settling pond; subsidence basin
• "沉降带" 英文翻译 :    geotectogene; su idencezone; subsidence zone; subsiding belt; zone of subsidence; zoneofsu idence
• "沉降袋" 英文翻译 :    sediment bag
• "沉降的" 英文翻译 :    sedimentary

• The formation and evolution of the sequence stratigraphy of the yanchang formation are governed by slow tectonic subsidence , warm humid climates , sediment supply and lake - level fluctuations
  延长组层序地层的形成与演化主要受控于当时缓慢的构造沉降、温湿气候、陆源碎屑物源供给及湖平面升降等地质因素。
• One of the frontier recearch of basin analysis in recent years is to analyze the tectonic subsidence history of depositional basins which occur in orogens at different geohistory stage , and to discuss the geodynamic processes involved with the basins
  摘要对造山带各地史阶段的沉积盆地进行构造沉降分析，进而探讨其地球动力学过程，是近年来盆地分析的前缘研究之一。
• By using the standard deviation method , the scaling properties described by the local fractal dimension d and crossover length tc of 48 measured landform profiles in different direction of 6 different studied landform sections are calculated
  负反馈机制表现的越明显；对于以构造沉降作用为主的盆地区而言，各个方向的地形剖线的分维值均显示出小于1 . 5的正反馈机制。
• Yanchang 4 + 5 sector to yanchang 3 sector lithofacies palaeogeography pattern was stable , because the constitution background was steady , and the source direction had no change , and supply was abundant . in those sectors the basin development was in lake retreat , and in the period of extinction gradually , and formatted construction delta deposit , but in yanchang 33 period the sedimentary speed were greater than construction speed , showing that overriding river mouth bars were abundant
  长4 + 5 ?长3期湖盆发展处于湖退、萎缩逐渐消亡时期，由于构造背景稳定，物源来源方向没有变化，物源供给充分，所以岩相古地理格局基本一致，形成建设性三角洲沉积，但长3 ~ 3期沉积速率大于构造沉降速率，表现为叠置河口砂坝极其发育。
• The tectonic subsidence curves on the southeastern margin of the yangtze plate are drawn out using of backstripping method for the basin formation and evolution . the basins located in the southern margin of the yangtze plate , in the basin dynamic computer simulation , is explored and constituted to be a typical foreland basin which is of not rather high mountain and thermal situation to be lower in this older orogeny belt
  在沉积盆地分析方面，基本查明扬子板块东南边缘早古生代被动大陆边缘沉积特征及沉积构造演化，同时运用反剥法技术对扬子板块东南大陆边缘沉积盆地形成，演化的构造沉降动力学进行探讨，运用计算机模拟方法，定量动力沉积学对扬子东南边缘奥陶纪到志留纪前陆地进行计算机模拟分析，探索并建立这个古老造山带前陆盆定量参数和动态定量模拟。
• Based on the studies in sea - level rise and response of coastal zone by domestic and foreign researchers , integrated with the essential characteristics of jiangsu coast and the radiate sand ridges , laid emphasis on the effects of sea - level rise on the radiate sand ridges and the tiaozini sands in it ' s center region , the following case were discussed in the paper . ( 1 ) the recent relative sea - level rise in the region of the radiate sand ridges found on the structural and sedimentary features of the radiate sand ridges , the rate of regional land subsidence was calculated ( structural , balanced and compressed subsidence were considered respectively ) . the latest assessment of global sea - level rise in the past century that was carried out by ipcc was cited
  本论文在总结国内外对海面上升及其对海岸带影响的研究基础上，结合江苏海岸及辐射沙洲区的基本特征，以相对海面上升对辐射沙洲及其中心部位的条子泥的影响为重点，讨论了以下几个方面的问题： ( 1 )辐射沙洲区近期的相对海面变化根据辐射沙洲区的构造和沉积特征，对区内地面沉降速率进行分项计算(包括构造沉降速率、均衡沉降速率和压实沉降速率) ，并引用ipcc最近对过去100年来全球绝对海面上升速率的评估。
• Compared to the basins in east guangxi , the basin of north guangxi is characterized by lower depositional and tectonic subsidence rate during rifting , longer thermal subsidence , later inflexion point from rifting to foreland buckling , as well as later inflexion point separating stable stage from active stage during foreland - buckling
  但与桂东大瑶山地区相比，桂北兴安地区在裂陷阶段的沉积速率和构造沉降速率明显偏低；热沉降阶段的持续时间偏长；裂陷阶段与前陆挠曲阶段的分界拐点偏晚；前陆挠曲阶段，由构造宁静期的缓慢沉降向构造活动期的快速沉降转化的分界拐点也偏晚。
• Kinematic models have predominance in predicting heat flow but weakness in simulating basin geometry ; kinematic - rheological models are adept in tectonic modeling , but identical with kinematic models in heat flow prediction ; dynamic models contain latent advantages and also some obstacles in tectono - thermal modeling
  运动学模型在预测盆地热流演化方面具有优势，但在预测构造沉降等几何形态方面存在一定的缺陷；运动学流变学模型的优势在于构造演化模拟，在热演化方面类似于运动学模型；动力学模型蕴含着潜在的巨大优势，只是目前还存在一些阻碍因素。