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balance profile
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  平衡剖面
     The<1/2 000 slopes at depths of 5-10 m mark the sea area of the balance profile, while the <1/1 500 slopes mark development toward the balance profile.
     本海域5—10m海区的坡度小于1/2000,是平衡剖面海域的标志; 坡度小于1/1500,是向平衡剖面发育的标志。
短句来源
     Based on the principles of balance profile. 9 structural profiles of Yanqi Basin are restored.
     根据平衡剖面原理,对焉耆盆地9条构造剖面进行了构造复原。
短句来源
     From area geology, physics of the Earth and remote sensing data, under the guidance of the theory of plate tectonics ,with the help of method of basin analysis, associated with the method of balance profile, the area geology background of Jiangling depression is studied comprehensively, the characters of basin structure, the evolution of basin model and the episode of basin-forming are researched, the Jiangling depression is analyzed completely and dynamically.
     从区域地质地球物理及遥感资料入手,以板块构造理论为指导,以盆地分析方法为手段,结合平衡剖面等方法,综合研究江陵凹陷的区域构造地质背景,开展盆地结构特征、盆地原型演化与成盆期研究,对江陵凹陷进行了整体和动态分析,认为江陵凹陷是受公安—松滋断层和丫角—新沟咀断层控制形成的凹陷型断陷盆地。
短句来源
     This paper uses balance profile restore method to study the structural subsidence of horizontal extension in different sedimentary period and its genesis mechanism of Baiyinchagan Sag, discusses the sedimentary filling evolution and development characteristic, and determines their relation to hydrocarbon migration, reservoir formation and accumulation.
     通过平衡剖面恢复等方法,对白音查干凹陷在各个沉积时期的水平伸展作用、构造沉降作用及其成因机制进行了研究,进而研究了凹陷的沉积充填演化和烃源岩的发育特征,探讨并明确了它们与油气运移、成藏、富集的关系,指出了今后的勘探方向。
短句来源
     3. Based on the regional tectonic setting and sedimentary sequence evolution, the structural physics modeling and balance profile reversion are first carried out. Its results approve the Yanqi basin is a Mesozoic-Cenozoic compressive basin(revival foreland basin) in the Tianshan composite orogenic belts.
     3、首次进行了系统的平衡剖面反演和构造物理模拟正演,结合区域构造背景及盆地沉积层序演化,排除了侏罗纪为拉张盆地的假设,认为焉耆盆地属于天山复合造山带内的一个中新生代山间挤压盆地(再生前陆盆地)。
短句来源
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  “balance profile”译为未确定词的双语例句
     The tires designed with the Tire Entire Configuration Optimum(TECO) theory presented by Shanghai Double-coin Truck Tire Company and the classical Balance Profile theory respectively were investigated using the proprietary FEA software developed by Harbin University of Technology combined with the indoor endurance test.
     以哈尔滨工业大学开发的有限元专用软件并结合室内耐久性试验,研究轮胎整体结构优化设计理论(TECO)和平衡轮廓设计理论所设计的轮胎。
短句来源
     The results of both FEA and test showed that the dynamic properties of the tire designed with TECO theory were better than those with the classical Balance Profile theory.
     有限元分析和试验结果均表明:使用TE-CO理论所设计的轮胎力学性能优于平衡轮廓设计理论所设计的轮胎。
短句来源
  相似匹配句对
     Flow Balance Analysis for Plastics Profile Extrusion Process
     塑料异型材挤出成型的流动平衡分析
短句来源
     On Pragmatic Balance
     论语用平衡
短句来源
     Beauty of Balance
     平衡之美
短句来源
     Profile on GMP
     浅谈对GMP的认识
短句来源
     The role of the restoration profile for the water balance of the cover systems was focussed on.
     重点介绍保护层(营养层)厚度对覆盖系统水平衡的影响。
短句来源
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  balance profile
The present findings indicate a Th2-over-Th1 cytokine balance profile in RA blood.
      
The other concerns the reaction of a given glacier to different variations in its mass balance profile.
      
Temperature and Mass Balance Profile of a Sulfuric Acid Test.
      
Second the resulting water resources are balanced for each balance profile with water demand.
      


In this study, water level depths indicated in maps of 1855, 1934, 1959, and 1984 were interpolated into present-day Yellow Sea average sea water level. A comparative analysis study was made of the erosion-accumulation evolutionary trends of the Taoerhe Bay and the Huang-he River after its course was shifted. Results of analysis suggest that when the Huanghe River emptied into the Taoerhe Bay, the coastline rapidly moved seaward with accumulation. After it changed its course, in the initial stage, the tidal...

In this study, water level depths indicated in maps of 1855, 1934, 1959, and 1984 were interpolated into present-day Yellow Sea average sea water level. A comparative analysis study was made of the erosion-accumulation evolutionary trends of the Taoerhe Bay and the Huang-he River after its course was shifted. Results of analysis suggest that when the Huanghe River emptied into the Taoerhe Bay, the coastline rapidly moved seaward with accumulation. After it changed its course, in the initial stage, the tidal flat was strongly eroded and scoured, but with lapse of time, the rate of erosion gradually slowed down. After the coastal balance profile was completed, development of the coastline became stable with slight accumulation or with erosion and accumulation here and there. It is proposed here that 1) when erosion-accumulation rate was ≤0.056 km/a, stability of coastline was marked by rapid development of shell bank; 2) when erosion-accumulation rate was ≤ ±0.084 km/a, the coastline trended to be stable when the shell bank began to develop. The<1/2 000 slopes at depths of 5-10 m mark the sea area of the balance profile, while the <1/1 500 slopes mark development toward the balance profile. Conclusions derived from this study are of great significance for an understan-ding of the evolutionary trends of development of the modern Huanghe River Delta and are useful information for the development and construction of the coastal regions along the Taoerhe Bay.

将1855年、1934年、1959年、1984年的海图的深度基准面换算成为当地黄海平均海水面,把它们的深度变化转换成泥沙的冲淤变化。研究了套尔河湾海域及黄河改道后三角洲的冲淤演化规律,行水时是快速淤进;改道后,初期是强烈的侵蚀和冲刷,随着时间的推移,其速率均逐渐减慢,达到岸滩平衡剖面塑造后,发育为轻微淤进或此冲彼淤的稳定海岸。提出:冲淤速率≤0.056km/a,贝壳堤迅速发育是海岸稳定的标志;冲淤速率≤±0.084km/a,贝壳滩开始发育是海岸向稳定演化的标志。本海域5—10m海区的坡度小于1/2000,是平衡剖面海域的标志;坡度小于1/1500,是向平衡剖面发育的标志。这对认识近代黄河三角洲的冲淤演变以及对套尔河湾海岸的开发建设,都具有重要意义。

The evolution of the Kongxi structural belt can be mainly divided into three periods by using the balanced profile technique to restore paleostructure during the Middle Late Triassic. The gentle fold deformation developed in Paleozoic and the detachment thrust maybe emerged as a result of the gently swelling shortness produced in Ordovician System during the late Triassic end or before Jurassic system deposited . The thrust structure deformed in the Permo Carboniferous strata, and then, the erosion...

The evolution of the Kongxi structural belt can be mainly divided into three periods by using the balanced profile technique to restore paleostructure during the Middle Late Triassic. The gentle fold deformation developed in Paleozoic and the detachment thrust maybe emerged as a result of the gently swelling shortness produced in Ordovician System during the late Triassic end or before Jurassic system deposited . The thrust structure deformed in the Permo Carboniferous strata, and then, the erosion happened in the top of Paleozoic. During Jurassic and Cretaceous, the thrust belt was covered with terrigenous deposits and became a "buried hill" in the topography. In the Lower Middle Jurassic the thrust structure lightly gradually deformed. When it deposited, the front of some thrust faults permeated into Lower Middle Jurassic. After the Lower Middle Jurassic deposited, regional structure inversed, during the Upper Jurassic Lower Cretaceous deposited in the extensional basin. After that, a Paleogene rifting basin - Huanghua basin was superposed on the buried hill. The Kongxi structural belt is comprised in the Cangdong normal fault, the Kongxi thrust, the normal fault of the west slope of the Kongdian relief and fault bend synclines.

通过平衡剖面技术复原古构造演化 ,并结合区域构造分析 ,可将孔西构造带的发育过程大致分为三个构造变形阶段 :晚三叠世末期为挤压褶皱变形期 ;晚三叠世沉积后至侏罗系沉积前为逆冲构造变形期 ;早—中侏罗世为逆冲构造“轻度”渐进变形期。晚侏罗世以后 ,区域构造作用发生反转。随着晚侏罗—早白垩世、早第三纪裂陷盆地的发育 ,孔西构造带作为潜山构造被掩埋。裂陷盆地时期的伸展构造对孔西构造带前第三系的逆冲构造基本上没有大的改造

Based on the principles of balance profile. 9 structural profiles of Yanqi Basin are restored. The results show that Yanqi Basin is in weakly compressive status in early Yanshanian with smaller amount of structural deformation, while main deformation is concentrated in late Yanshanian and Xishanian, but the deformation is weaker in Xishanian than that in Yanshanian. On the plane, deformation is stronger in west than that in the east of the basin. Mesozoic-Cenozoic evolution of the basin is divided...

Based on the principles of balance profile. 9 structural profiles of Yanqi Basin are restored. The results show that Yanqi Basin is in weakly compressive status in early Yanshanian with smaller amount of structural deformation, while main deformation is concentrated in late Yanshanian and Xishanian, but the deformation is weaker in Xishanian than that in Yanshanian. On the plane, deformation is stronger in west than that in the east of the basin. Mesozoic-Cenozoic evolution of the basin is divided into 3 stages, such as weak compression and syn-deformation stage in early Yanshanian, strong compression stage in late Yanshanian and face to face compression stage in Xishanian.

根据平衡剖面原理,对焉耆盆地9条构造剖面进行了构造复原。结果表明,燕山早期焉耆盆地处于弱挤压状态,构造变形量相对较小,而主要的变形量集中于燕山晚期和喜山期,但喜山期变形稍弱于燕山晚期。平面上盆地西部变形量较大,东部变形量较小。盆地中、新生代的演化划分为3个主要阶段:燕山早期弱挤压与同生变形阶段,燕山晚期强烈挤压阶段,喜山期对冲挤压阶段。

 
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