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   geomorphic feature 的翻译结果: 查询用时:0.062秒
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geomorphic feature
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  地貌特征
     This shows that satel-lite photographs reflect directly geomorphic feature, so do generally reflectdeep structural configuration.
     卫星象片直接反映地貌特征,因而也大体上反映深部构造轮廓。
短句来源
     Beginning with analysis on production costs component of geological survey project, through contrasting and analyzing the interrelation between physical & humane geography factors which influences planning-budget and regional adjustment coefficient and the factor of production costs component of geological survey project, the paper considers that geomorphic feature plays a leading role.
     本文从分析地质调查项目生产成本构成入手 ,对影响地质调查项目设计预算地区调整系数的自然、人文地理因素与地质调查项目生产成本构成因素之间的相互关系进行了对比分析 ,认为地貌特征在其中起了主导作用。
短句来源
     An analysis on the development character,geomorphic feature, seismic signature,etc of the Quaternary strata suggests that the area from Hefei to the west foot of the Fuchachan Mt is a relatively downcast zone,the area around Liangyuan town on the south margin of the Jianghuai watershed a modern upcast zone, and the area from the eastern Fuchashan Mt to Chaohu a relatively upcast zone.
     通过对合肥及其以东地区第四纪地层发育特征、地貌特征、地震等特征分析,认为合肥至浮槎山西麓为相对下降区,位于江淮分水岭南缘的梁园一带为现代上升区,浮槎山东部至巢湖一带为相对上升区。
短句来源
     So in this paper in terms of forcedynamic geologic process-dynamic geomorphic feature of cause of formation classification,on the basis of studying Hachinsion(1957)classification, we've put it further in order and given it more supplements,and as a result classified the global lake basins into authentic genetic types.
     为此,本文遵循营力—动力地质作用—动力地貌特征的成因分类原则,在研究了哈钦逊(1957)分类的基础上,进一步整理和补充,把全球的湖泊盆地进行了更符合实际的成因分类.
短句来源
     BaSed on the latest research achievement,this paper deals with the geomorphic feature,late Cenozoic stratum ,Volcano and basalt, main active fractures , neotectonics and spatial distribution of seismicity,and seis-motectonics of two Datong-Yanggao earthquakes in Datong downfaulted basin,also discusses the macroquakerisk of Datong downfaulted basin in future 10 years.
     以最新研究成果,全面、系统地阐述了大同断陷盆地的地貌特征、晚新生代地层、火山与玄武岩、主要活动断裂、新构造单元与地震活动的空间分布、大同-阳高两次地震的地震构造。 在此基础上探讨了今后10年左右的时间内,大同断陷盆地的地震危险性。
短句来源
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  地貌形态
     Because of the tectonic knickpoints and lithology knickpoints of the Jinsha River and the distinctions of the fluvial characters,there are some differences in the valley geomorphic feature and the TL datings of the terraces between Aoga reach and Yuzha reach,so the analysis of the terraces height relative to the Jinsha River do not make out.
     凹嘎河段和鱼鲊河段在河谷地貌形态和阶地堆积物形成年代上都有很大差异,其原因为金沙江河谷中存在着多级构造裂点或岩性裂点,两河段性质存在差异,所以该河段不宜做传统的阶地位相分析。
短句来源
  “geomorphic feature”译为未确定词的双语例句
     Scientific Planning and Strengthened Measures to Protect Geomorphic Feature
     科学规划,强化措施 做好地质地貌景观保护
短句来源
     Geomorphic Feature of Modern Dynamic Fault In the East Side of Maoshan Mt.
     茅山东侧断裂现代运动的地貌学特征
短句来源
     GEOMORPHIC FEATURE AND ORIGIN OF THE DELTAS AT THE EAST AND WEST MOUTHES OF QIONGZHOU STRAIT
     琼州海峡东、西口地貌特征及其成因初探
短句来源
     Bitter and salt water is due to ancient geographical environment,geomorphic feature,climate condition,geological structure and salt accumulation.
     苦咸地下水的形成是古地理环境、地貌、气候条件、地质构造和积盐作用共同导致的结果;
短句来源
     (2) There is a negative interrelation between the days of sandstorm and the percentage of coverage of vegetation, which varies due to the difference of geomorphic feature and the changes of season.
     沙尘暴日数与植被覆盖率之间呈现负的相关关系 ,这种相关关系在不同地貌类型区和不同季节有所差异 ;
短句来源
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  geomorphic feature
Lake Wales Ridge is the principal geomorphic feature of the region, with younger ridges, including Trail Ridge, occurring to the north and east.
      
Unit names are chosen to identify each unit by its primary characteristics or to show association with a major geomorphic feature.
      
The rift region shows a geomorphic feature of fault depression on the surface and deep structure exhibits uplifted in upper mantle.
      
For the geomorphic feature category, various types of water bodies were included from lakes and depressional wetlands to arroyos and desert washes.
      
Each category represents a geomorphic feature, and revegetation strategies vary by geomorphic feature.
      
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As a lofty mountain Nanshan stretches along the southern border of Kansu Corridor. In past two decades a few discussions had been given by some sdholars about its landforms and its quaternary glaciations. Based upon my field works and recent reports, we know that there are some close Connections existed between tectonic movements, geomorphic cycles and correlative deposits; and, Consequently, they may be mutually explained. according to the analysis of the facies and distribution of Cenozoic sediments,...

As a lofty mountain Nanshan stretches along the southern border of Kansu Corridor. In past two decades a few discussions had been given by some sdholars about its landforms and its quaternary glaciations. Based upon my field works and recent reports, we know that there are some close Connections existed between tectonic movements, geomorphic cycles and correlative deposits; and, Consequently, they may be mutually explained. according to the analysis of the facies and distribution of Cenozoic sediments, We Know that there a peneplanation developed on the older rocks of Nanshan till pper pliocene, and the red deposits which extended over the Nansban and its adjacent regions Were laden down in the same time. Probably laterly, a crusalt movement, which included mul iple uplifts, initiated. The present geomorphic features of Nanshan are possibly resulted from them. as the dissected summit-levels, the remnants of old peneplains Can be found on many mountain tops today. As regards quaternary glaciations of Nanshan, a more important sign ification should be ascribed to the uplifts of this mountain. Perhaps boh because of the uplifts and the Climatic changs, in Nanshan two glacio pluvial periods had occured in quaternary. When the glaciers expanded all of the mountain peaks and valleys. Later on, the glacio fluvial waters were Carrying much debris and forming sedimentary units, which have been called inland molasse formation, into piedmont plain. a distinct interval, which indicat a true interglacial stage, have been found in that formation. The following table shows the main geological changes of Cenozoic of Nanshan.

河西走廊之南延伸着雄伟的祁连山,在过去20年中一些学者曾对该山的地貌和其第四纪冰期作过一些探讨。根据本人的野外工作及最近的文献资料,我们看到,在构造运动、地貌循环和相关沉积三者之间有着紧密的联系,因而,它们可以相互解释。分析岩相和新生代沉积的分布,我们得知直到上上新世,祁连山进行着准平原化的过程,同时并沉积下红色沉积,它遍及祁连山内外。后来,地壳运动开始,它包括多次上升。现代的祁连山的面貌即是多次上升的产物。古准平原的遗跡,目前可在许多山顶发现。祁连山的第四纪冰期的发生,山地上升占有重要地位,可能正是由于上升和气候变化的同时作用,祁连山发生两次冰期——多雨时期。当时冰川遍及山峰和谷地,稍后,冰融水携带大量碎屑物质带入山足平原形成内陆磨拉石建造的沉积。在该沉积岩系中发现有一清楚的间断,这代表一次真正的间冰期。祁连山新生代的主要地质事件见84页附表。

The terrains discussed in the present paper are provided with polygenic geomorphic features. Studies on the effects of active tectonics and morphogenetic movement have given new vitality to the course of structural geomorphology. A large territory of China is situated at an active region geotectonicly between two big plates. Since the Late Cenozoic a large number of active faultshad divided the continent into a series of fault blocks of different sizes from high mountains and plateaus in western China...

The terrains discussed in the present paper are provided with polygenic geomorphic features. Studies on the effects of active tectonics and morphogenetic movement have given new vitality to the course of structural geomorphology. A large territory of China is situated at an active region geotectonicly between two big plates. Since the Late Cenozoic a large number of active faultshad divided the continent into a series of fault blocks of different sizes from high mountains and plateaus in western China to the east coasts. It is indeed the fault blocks of different amplitudes which have determined the basic framework of the morphotectonics of China. Moreover, the morphogenetic movements as well as the active faults had intersected or evencut off the oldtectonic lines and have been controlling the formation and development of the sedimentary basins and alluvial plains in central and East China. Many rivers either big or small had owed their existence to the new lineaments formed by the morphoteetonics some of which were in herited from the old structures and some were newly developed during the Quaternary. These characters mentioned above demostrate that Quaternary morphogenetic movement has been starting a new tectonic cycle in the development of the tectonic history of the Earth.

现代地貌具有多元性和多生性特征。研究活动构造与造貌运动对地貌发育的影响,赋予了“构造地貌学”新的活力。中国处在一个大陆板内构造活动区,晚新生代以来的活动断裂将中国地块从内陆到沿海划分为一系列的活动断块,断块的差异运动决定了中国地貌的基本格架。分析中国东部的活动构造和造貌运动,它们截切了老构造并控制了中国东部盆地、平原和河流的发育,使中国东部的盆地、平原与河流具有继承性、新生性和迁移性的特征,从而表明造貌运动标志着地球构造的发展进入了一个新阶段。

Since the Late Pleistocene, the movement of the northern segment of the Honghe fault zone has been different from that of the southern one. At the southern segment movement is primarily characteristic of single right-lateral shearing, whereas at the northern segment, of a compositive right-lateral shearing with faulted-depressional extension. With in the compositive zone in question appears an en-echolon fault pattern due to alternate shearing and fault-depression. From the southeast to the northwest, they are:...

Since the Late Pleistocene, the movement of the northern segment of the Honghe fault zone has been different from that of the southern one. At the southern segment movement is primarily characteristic of single right-lateral shearing, whereas at the northern segment, of a compositive right-lateral shearing with faulted-depressional extension. With in the compositive zone in question appears an en-echolon fault pattern due to alternate shearing and fault-depression. From the southeast to the northwest, they are: Ding Xiling shearing zone, Dali fault-depression,Xiashankou shearing zone, Eryuan fault-depression, Cibihu Lake shearing zone and Jianchuan fault-depression. Geomorphic feature of shear zone and fault-depression is completely different, the former appearing as a narrow valley and the latter, as a basin.This paper is focused on the determination of displacement rates and recurrence intervals of earthquakes of Dixiling shear zone and Dali fault-depression having remained since the late stages of Late Pleistocene. For Dixiling shearing zone, right-lateral displacement rate is 8mm/yr, and vertical slip rate is 1.8mm/yr, with a ratio of 4:1 and for Dili fault-depression, 5mm/yr and 9mm/yr, respectively, with a ratio of nearly 1:2. According to calculations of the parameters of fault displacement,we have found that recurrence intervals for magnitude 6.8 earthquake are 178±29 years. It is consistent with the recurrence interval (150±50 years)of M 6—7 earthquakes from historic seismic records in this area. It may be useful to immediate—long term earthquake prediction.

本文用地质方法确定了全新世以来红河断裂(北段)位错速率:狭谷段(定西岭)水平位错速率8毫米/年,垂直位错速率1.8毫米/年;宽谷段(大理)水平位错速率5毫米/年,垂直位错速率9毫米/年。据断裂位错参数计算,本区6.8级左右地震重复发生的时间间隔是178±29年;它与6—7级历史地震重复时间间隔150±50年在时间尺度上相当,这对地震中长期预报有参考价值。

 
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