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yangtze gorges
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  长江三峡
     With the data of first motion observation in the Yangtze Gorges and its vicinity (N 28°~34°,E 108°~114°) from 1974 the fault plan solutions of 40 earthquakes (Ms≥2.1)and the local and sublocal stress fields as well as the mean faultting characteristices are determined.
     使用长江三峡及邻区(北纬28°-34°,东经108°-114°)1974年以来的初动观测资料,确定了Ms≥2.1的40次地震的断层面解、该区的区域应力场和分区应力场及平均错动性质。
短句来源
     According to the identification of the sequence boundaries and the analysing results of biota and sedimentary facies on the Early Paleozoic stratigraphies, three mesosequences (SME1, SME2 and SME3), six sequence assemblages (SSA1, SSA2, SSA3, SSA4, SSA5, SSA6), and twenty-one sequences at least or T-R cycles (transgression-regression cycle) can be recognized in the Yangtze Gorges area.
     根据层序界面的识别,结合沉积相和生物群特点分析,指出长江三峡地区早古生代时期大致可识别出3个中层序(SME1,SME2和SME3),6个层序组(SSA1,SSA2,SSA3,SSA4,SSA5和SSA6)和21个层序或T—R旋回(海进-海退旋回)。
短句来源
     Simulation Analysis of Groundwater Seepage Field on the Fengjie Reservoir Bank Slope of the Yangtze Gorges Project
     长江三峡工程奉节库岸斜坡地下水渗流场模拟分析
短句来源
     Characteristics of Drought/flooding in the Yangtze Gorges and Climate Prediction
     长江三峡地区夏季旱涝特征及气候预测
短句来源
     Motion of Gravels as Bed Load in the Yangtze Gorges
     长江三峡河段的卵石推移质运动
短句来源
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  长江三峡地区
     According to the identification of the sequence boundaries and the analysing results of biota and sedimentary facies on the Early Paleozoic stratigraphies, three mesosequences (SME1, SME2 and SME3), six sequence assemblages (SSA1, SSA2, SSA3, SSA4, SSA5, SSA6), and twenty-one sequences at least or T-R cycles (transgression-regression cycle) can be recognized in the Yangtze Gorges area.
     根据层序界面的识别,结合沉积相和生物群特点分析,指出长江三峡地区早古生代时期大致可识别出3个中层序(SME1,SME2和SME3),6个层序组(SSA1,SSA2,SSA3,SSA4,SSA5和SSA6)和21个层序或T—R旋回(海进-海退旋回)。
短句来源
     Characteristics of Drought/flooding in the Yangtze Gorges and Climate Prediction
     长江三峡地区夏季旱涝特征及气候预测
短句来源
     Study on the Steeped Landform in the Yangtze Gorges Area
     长江三峡地区层状地貌研究
短句来源
     DEVONIAN SEQUENCE STRATIGRAPHY AND SEA LEVEL CHANGES IN THE YANGTZE GORGES AREA
     长江三峡地区泥盆纪层序地层及海平面变化
短句来源
     New U-Pb zircon ages from the Ediacaran(Sinian) System in the Yangtze Gorges:constraint on the age of Miaohe biota and Marinoan glaciation
     长江三峡地区埃迪卡拉(震旦)系锆石U-Pb新年龄对庙河生物群和马雷诺冰期时限的限定(英文)
短句来源
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  三峡地区
     According to the identification of the sequence boundaries and the analysing results of biota and sedimentary facies on the Early Paleozoic stratigraphies, three mesosequences (SME1, SME2 and SME3), six sequence assemblages (SSA1, SSA2, SSA3, SSA4, SSA5, SSA6), and twenty-one sequences at least or T-R cycles (transgression-regression cycle) can be recognized in the Yangtze Gorges area.
     根据层序界面的识别,结合沉积相和生物群特点分析,指出长江三峡地区早古生代时期大致可识别出3个中层序(SME1,SME2和SME3),6个层序组(SSA1,SSA2,SSA3,SSA4,SSA5和SSA6)和21个层序或T—R旋回(海进-海退旋回)。
短句来源
     Characteristics of Drought/flooding in the Yangtze Gorges and Climate Prediction
     长江三峡地区夏季旱涝特征及气候预测
短句来源
     Study on the Steeped Landform in the Yangtze Gorges Area
     长江三峡地区层状地貌研究
短句来源
     DEVONIAN SEQUENCE STRATIGRAPHY AND SEA LEVEL CHANGES IN THE YANGTZE GORGES AREA
     长江三峡地区泥盆纪层序地层及海平面变化
短句来源
     New U-Pb zircon ages from the Ediacaran(Sinian) System in the Yangtze Gorges:constraint on the age of Miaohe biota and Marinoan glaciation
     长江三峡地区埃迪卡拉(震旦)系锆石U-Pb新年龄对庙河生物群和马雷诺冰期时限的限定(英文)
短句来源
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  “yangtze gorges”译为未确定词的双语例句
     Study on Management System of Environment Geology Calamity in the Yangtze Gorges Reservoir Area
     三峡工程库区环境地质灾害的管理系统
短句来源
     On the basis of a systematic collection and study of Late Ordovician Tangyagraptus (graptolite) in eastern Yangtze Gorges area, the genus Tangyagraptus is reclassified into 3 species, i.e., Tangyagraptus typicus , T.
     本文通过对峡东奥陶系五峰组笔石Tangyagraptus的系统采集和研究 ,认为该属以厘定为 3个种为宜 :Tangya graptustypicus,T .
短句来源
     Programming Practices of Urban Water Supply Network of the Yangtze Gorges Reservoir Region
     三峡库区城市供水管网的规划设计实践
短句来源
     poumoti, Conochitina sp. A, Conochitina sp. B, Lagenochitina cf. combazi and Cyathochitina sp. Among them,Conochitina symmetrica of the Adelograptus--Clonograptus Zone to the T. approximatus Zone (Paris &Mergl, 1984)is basically identical with the specimens found in the corresponding or a little higherhorizon in the eastern Yangtze Gorges.
     pomoti,Conochitina sp.A,Conochitina sp.B,Lagenochitina cf.
短句来源
     Upon the background of the Yangtze Gorges reservoir, remote data acquisition scheme based on ActiveX and OPC is presented.
     最后结合库区的应用背景,设计了一种基于ActiveX和OPC的远程数据访问方案。
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  yangtze gorges
The thickness of the Hamajing Member varies from 20 m to 100 m in the Yangtze Gorges area.
      
Macrofossil biota from upper Doushantuo Formation in eastern Yangtze Gorges, China.
      
Grabau proposed the term Sinian for a discrete system of sedimentary rocks underlying Lower Cambrian strata in the Yangtze Gorges region of China.
      


In the Yangtze Gorge,the earliest Cambrian deposits are well-developed and

本文系统地描述了湖北西部早寒武世最早期的单板类、腹足类和节壳类计42种,分属于31属、14科、7超科、6目,其中包括2新目、3新超科、7新科、25新属和39新种。建立了下寒武统最底部的单板类、腹足类的三个化石组合;依据化石组合特征讨论前寒武系与寒武系界线的划分与对比。节壳类的发现,对探讨软体动物门的起源、演化提供了线索。

The flow resistance in the reach of The Yangtze Gorge from Fengjie to Xiangxi varies along the river with different stages and depends on the compositions of the bed material, the asperities of the banks and the features of channel shape.The flow resistance is mainly composed of bed and bank resistance for reaches with little changes in cross-sections along the course, and of bed, bank and form resistance if such changes do exist. Einstein method is employed in separating the bed and bank resistance. Form...

The flow resistance in the reach of The Yangtze Gorge from Fengjie to Xiangxi varies along the river with different stages and depends on the compositions of the bed material, the asperities of the banks and the features of channel shape.The flow resistance is mainly composed of bed and bank resistance for reaches with little changes in cross-sections along the course, and of bed, bank and form resistance if such changes do exist. Einstein method is employed in separating the bed and bank resistance. Form resistance can be treated as a loss due to sudden contraction or enlargement.The results of such an analysis indicate that the bank roughness coefficient nw vary within the range of 0.04-0.22 ( 0.10-0.22 for narrow valleys with an average of 0.14 and 0.04-0.12 for broad valleys with an average of 0.07 ). Bed roughness coefficient nb are within the range of 0.018-0.043.The energy gradient due to changes in cross-sections along the river course can be as much as 40-70% of the total energy loss.

本文对三峡奉节至香溪河段在各级流量下沿程各段的综合糙率系数进行了计算与分析.讨论了三峡河道水流阻力和综合糙率的组成.顺直河段水流阻力主要由床面阻力和边壁阻力组成,非顺直河段水流阻力由床面阻力、边壁阻力和河槽局部阻力组成.提出了山区河道顺直河段与非顺直河段糙率系数的计算方法,并用实测资料作了验证.

Based on studying the feature of seismogenic structure and the neotectonic setting as well as on analysing deep-seated structure conditions of the Easter Yangtze Gorge, some geological structure signs of the weak earthquake are discussed in this paper.The Yangtze Gorge is referred to a weak earthquake area in accordance with data up to now. The seismic activities in the region mainly occurred on the surface of East Gorge, so the dependence of relations between them is close and obvious in space...

Based on studying the feature of seismogenic structure and the neotectonic setting as well as on analysing deep-seated structure conditions of the Easter Yangtze Gorge, some geological structure signs of the weak earthquake are discussed in this paper.The Yangtze Gorge is referred to a weak earthquake area in accordance with data up to now. The seismic activities in the region mainly occurred on the surface of East Gorge, so the dependence of relations between them is close and obvious in space As these seismogenic structures are located in the neotectonic background of the whole upheaval and merely dissect the upper crust, there are features of weak earthquake with small intensity, low frequency and shallow focus.In accordance with the seismotectonic relations mentioned above, the signs of geological structure of the weak earthquake in this area may be summarized as follows:1. The seismogenic structures belong to a fault lying in a shallower layer of the crust, which has had no evident dislocation since Quaternary Period.2. The regional neotectonic movements are mainly characterized by continual uplift and subsidence of arched flexures as a whole. Usually the broken river terrace, the dismembered denudation surface and the geomorphic gradient belt do not appear.3. The tectonic deformation in the newly-formed sediments is not obvious. It is generally short of Quaternary fold and fault.

本文通过对长江三峡东段发震构造特征,新构造环境和深部构造条件等与地震活动相关性的分析给出了识别弱震区的地质构造标志。

 
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