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geomorphic feature
相关语句
  地貌特征
    Geomorphic Feature and Geological Calamity in Nihewan Reserve Zone
    泥河湾保护区地貌特征与地质灾害
短句来源
    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
    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
    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
  地貌特征
    Geomorphic Feature and Geological Calamity in Nihewan Reserve Zone
    泥河湾保护区地貌特征与地质灾害
短句来源
    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
    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
    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
  “geomorphic feature”译为未确定词的双语例句
    We propose in this paper that recent activity along a fault zone can be directly identified based on activity sequence of the strong earthquake and multiplesurvey on the geodetic network across the fault zone,and then the active segment can be determined in combination with geomorphic feature and variation of ground water level.
    以一次强震活动序列、跨断层大地测量网的复测、直接鉴定断层新活动、并结合地形地貌和地下水位变化等途径来划分断层运动的区段。
短句来源
    In this paper, the basic biological feature of Panshan basin was introduced from aspects of sedimentary layer, geomorphic feature and tectonics,and indicated that Panshan basin is a relative individual tectonic body in comparison with Yan-Huai basin.
    从沉积地层、地貌和构造等方面概述了矾山盆地的基本地质特征。 提出矾山盆地是延——怀盆地中的一个相对独立的构造盆地。
短句来源
    Intermittent flood crevasse is the main factor in the formation to Wencunjia crevasplayi adeep crevasse pond and the directional extansion of braided channels passing by hills and holows is the important geomorphic feature of the crevasse splay.
    阵发性洪水决口是文村甲决口扇形成的主要因素。 决口深潭和岗洼相间辫状水道断续定向延伸是其重要的地貌标志。
短句来源
    This paper researches geomorphic feature of active fault on the remotesensing images,discussed analysing method, procedure and result of the active faulton remote sensing images of different kinds and scales.
    本文以遥感信息作为研究活动断裂的依据,探讨了利用不同种类、不同比例尺遥感图像分析活动断裂的方法、程序和效果。
短句来源
    This paper interprets the uneven distribution of the earthquake damage of the 7.0 scale quake in Lijiang on Fed 3,1996, including earthquake intensity, earthquake damage of building in extreme seismic area and surface damage, etc. We regard the multi factor intiuence of broken form of earthquake origin istructure, active fault, thick new sediments, geomorphic feature and building base, etc as the main cause of the uneven distribution of the earthquake damage.
    笔者描述了1996年2月3日丽江7.0级地震的地震烈度、极震区房屋震害、地表破坏等地震灾害分布的不均匀性特征,并分析了震害分布不均匀性的主要原因是由发震构造破裂方式、活动断裂、巨厚的新沉积层、地形地貌、地基基础等多种因素的影响所造成。
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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