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meandering river
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  “meandering river”译为未确定词的双语例句
     1. Definitely brought forward that H2 and H3 lied in the transition zone from braided river to meandering river in the research area.
     主要成果与创新如下: 1、明确提出H2、H3 段研究区为辫状河向曲流河的过渡区。
短句来源
     There are 16 kinds of lithofacies identified in Damagang deposit of modern Nenjiang river:Gm,St1,St2,Ft,Ssd,Sh,St,Stcb,Shcs,Sw,Sm,Fw,Fm,Fsc1,Fsc2,Mm and Mpr. Five kinds of subfacies and six kinds of sedimentary microfacies were developed well,including fluvial flood-plain microfacies,crevasse-splay microfacies,natural levee microfacies,point bar microfacies of the meandering river,and flood-plain microfacies and mid-channel bar microfacies of the braided river.
     在现代嫩江大马岗沉积体内部 ,共识别出 16种岩相 ,即 Gm,St1,St2 ,Ft,Ssd,Sh,Stcb,Shcs,Sw,Sm,Fw,Fm,Fsc1,Fsc2 ,Mm及Mpr,发育五种亚相、六种沉积微相 ,即曲流河的河漫滩沉积微相、决口扇微相、天然堤微相、点坝微相、辫状河的溢岸微相及心滩微相。
短句来源
     A Study on Internal Architecture of Channel Sand in Meandering River
     曲流河道砂体内部建筑结构研究
短句来源
     The model needs only data for river geometric, inflow processes and sediment parameters, and can simulate the flow velocity fields for both water surface and cross_section for rivers with different geometric conditions including the flow features of meandering river.
     该模型只需要河流几何形状、入流条件以及泥沙级配参数 ,能够模拟出不规则几何形态的河道断面流速分布及平面流场分布 ,并且对于弯道水流特征与泥沙输送 -沉积特征也能得到较好的表现。
短句来源
     Guantao Formation reservior in Zhuang 106 well-block is the subtle lithological reservoir formed in meandering river environment.
     老河口油田桩106地区馆陶组是曲流河道砂体成藏.
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  相似匹配句对
     The Jinjiang has developed into a meandering river.
     同时荆江已演变为典型的弯曲河道 ,成为防洪的重点地段。
短句来源
     Research on mechanism of evolution for meandering river
     蜿蜒性河流演变机理研究
短句来源
     River Engineering
     河流工程
短句来源
     Nanxi River
     楠溪江
短句来源
     (6)meandering reach;
     ⑥宽滩蜿蜒河段;
短句来源
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  meandering river
Selection of water intake site on a curvilinear stretch of a meandering river
      
This paper describes the influence of natural levee overbank deposition on riverine grasslands along the meandering River Dinkel (The Netherlands).
      
Biotic Factors: Lessons Drawn From Rotifers in the Middle Loire,a Meandering River Monitored From 1995 to 2002, Duri
      
The planned restoration of the Kissimmee River ecocystem will backfill approximately 35 km of flood control canal (C-38) that cuts through the meandering river channel, re-establish natural flow patterns, and restore the river/floodplain ecosystem.
      
The architecture of a sandy braided-meandering river system: an example from the lower triassic Soiling Formation (M.
      
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Different opinions with some idea expressed in“The Analysis of the Two Types of Fluviatile Facies Reservoirs and Their Production Performances in the Gudao Oilfield”by Li Xingguo et al(“Petroleum Exploration and Development”No.2, 1982)are presented in this paper.Main points emphasized in this paper are: 1.3 kind of paleorivcrs systems were existed in this area:meandering river, anastomosed river and braided river.Guan 3-4 series were deposited from mea- ndering river systems,Guan 5-6...

Different opinions with some idea expressed in“The Analysis of the Two Types of Fluviatile Facies Reservoirs and Their Production Performances in the Gudao Oilfield”by Li Xingguo et al(“Petroleum Exploration and Development”No.2, 1982)are presented in this paper.Main points emphasized in this paper are: 1.3 kind of paleorivcrs systems were existed in this area:meandering river, anastomosed river and braided river.Guan 3-4 series were deposited from mea- ndering river systems,Guan 5-6 were deposited from anastomosed river,while Guan 7-10 were deposited from braided river.Guan 5-6 were deposited from ana- stomosed river system instead of braided river system as expressed by Mr.Li et al. 2.A detailed description on the depositional characteristics of the main pay horizon Guan 3-6 series is given.Emphasis has been given on the complexities and differences between the depositional facies of Guan 3-4 series and Guan 5-6 series.The self-potential and microlog plots can't be classified simply as“be- ll-shaped”or“tube-shaped”. 3.A preliminary analysis,based on the different depositional facies of Guan 5-6,Guan 3-4,on their development results has been given,it has been empha sized that the difference in the sub-facies instead of that of in-layer heteroge- neity is the main cause.

本文对李兴国和周宪城同志在本刊1982年第2期上发表的“孤岛油田两类河流相储集层及其开发效果分析”一文,提出了不同看法。本文认为:孤岛油田馆陶组河流沉积可分三种类型:馆3—4组为曲流河,馆7—8组为辫状河,特别强调了馆5—6组为网状河而不是辫状河;同时对孤岛油田主要含油层组——馆3—6组的曲流河和网状河的沉积特征作了较为细致的阐述;并根据不同类型河流的沉积特征,对馆5—6组比馆3—4组开发效果要好,进行了初步的解释,所强调的不是层内非均质性差异,而是不同亚相对整个开发层系的影响。

The Wuyi Mountain is situated in the south of Chongan County, Fujian Province. It covers an area of 60 km~2, and the altitude is between 180 m and 720 m. The length of the famous Jiuqu River is 9.5 km. The Wuyi Mountain was originally a plain of denudation. It developed into a lake basin by the subsidence of the earth's crust in the early Cretaceous period. The thickness of the deposit in the lake has reached 1500m. Owing to uplifting in the late Tertiary period, a monoclinic block mountain was formed. The Wuyi...

The Wuyi Mountain is situated in the south of Chongan County, Fujian Province. It covers an area of 60 km~2, and the altitude is between 180 m and 720 m. The length of the famous Jiuqu River is 9.5 km. The Wuyi Mountain was originally a plain of denudation. It developed into a lake basin by the subsidence of the earth's crust in the early Cretaceous period. The thickness of the deposit in the lake has reached 1500m. Owing to uplifting in the late Tertiary period, a monoclinic block mountain was formed. The Wuyi Mountain has developed into the following morphological types under the control of the geological structures and the morphological development: cuesta, block mountain, hill, gentle hill, flat-bottomed alley valley, depressed valley, terrace, etc. The Jiuqu River developed mainly along east-west and north-south strike faults, and so, it is a very meandering river.

武夷山位于福建崇安南部,面积60平方公里,山区海拔180~720米。著名的九曲溪全长9.5公里。武夷山原为剥蚀区,白垩纪初期断落下陷成为一个长条形湖盆。湖盆堆积层厚达1500米。新第三纪湖盆被挤压回升,形成单斜断块山。武夷山受构造和发育过程影响,形成以下地貌类型:单面山、块状山、丘陵、缓丘、平底巷谷、坳谷、二级阶地、一级阶地、砾石边滩和心滩、河道等。九曲溪主要是沿东西和南北向断裂发育,比较曲折。

The Wuyi Mountain is situated in the south of Chongan County, Fujian Province. It covers an area of 60 km~2, and the altitude is between 180 m and 720 m. The length of the famous Jiuqu River is 9.5 km. The Wuyi Mountain was originally a plain of denudation. It developed into a lake basin by the subsidence of the earth's crust in the early Cretaceous period. The thickness of the deposit in the lake has reached 1500m. Owing to uplifting in the late Tertiary period, a monoclinic block mountain was formed. The Wuyi...

The Wuyi Mountain is situated in the south of Chongan County, Fujian Province. It covers an area of 60 km~2, and the altitude is between 180 m and 720 m. The length of the famous Jiuqu River is 9.5 km. The Wuyi Mountain was originally a plain of denudation. It developed into a lake basin by the subsidence of the earth's crust in the early Cretaceous period. The thickness of the deposit in the lake has reached 1500m. Owing to uplifting in the late Tertiary period, a monoclinic block mountain was formed. The Wuyi Mountain has developed into the following morphological types under the control of the geological structures and the morphological development: cuesta, block mountain, hill, gentle hill, flat-bottomed alley valley, depressed valley, terrace, etc. The Jiuqu River developed mainly along east-west and north-south strike faults, and so, it is a very meandering river.

武夷山位于福建崇安南部,面积60平方公里,山区海拔180~720米。著名的九曲溪全长9.5公里。武夷山原为剥蚀区,白垩纪初期断落下陷成为一个长条形湖盆。湖盆堆积层厚达1500米。新第三纪湖盆被挤压回升,形成单斜断块山。武夷山受构造和发育过程影响,形成以下地貌类型:单面山、块状山、丘陵、缓丘、平底巷谷、坳谷、二级阶地、一级阶地、砾石边滩和心滩、河道等。九曲溪主要是沿东西和南北向断裂发育,比较曲折。

 
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