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geomorphic feature
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  地貌特征
    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
  地貌特征
    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。
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  “geomorphic feature”译为未确定词的双语例句
    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。
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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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On the basis of comprehensive methods of geophysical exploration, geology and boring to prospect geomorphic features, stratigraphy and structural conditions, the paper begins with the research of earthquake-geology and Quaternary geology and earthworks structure, analyses and appraises the earthquake response and earthquake-resistant conditions.

在综合利用物探、地质、钻探等方法查明工作区内地貌、地层及构造条件的基础上,从地震地质、第四纪地质及土体结构研究入手,对区内分析划出的地震基本烈度Ⅶ度区地震反应及抗震条件进行了分析、评价和区划,并提出了对策和建议.

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。

The geomorphic features of the Changjiang Estuary are characterized by the multi-order bifurcations, active submerged sandbars, mid-channel sandbars, creeks and riffle. Our study indicates the saltwater intrusion has the following four forms: l) direct intrusion from the outer sea; 2) saltwater intrusion by tidal flooding, 3) water exchange between creeks or shallow water channel, 4) salt water upstream from other waterways. These results complicate temporal and spatial changes in salinity. A high chioriulty...

The geomorphic features of the Changjiang Estuary are characterized by the multi-order bifurcations, active submerged sandbars, mid-channel sandbars, creeks and riffle. Our study indicates the saltwater intrusion has the following four forms: l) direct intrusion from the outer sea; 2) saltwater intrusion by tidal flooding, 3) water exchange between creeks or shallow water channel, 4) salt water upstream from other waterways. These results complicate temporal and spatial changes in salinity. A high chioriulty concentration zone exists between the Liuhekou to the Sidongkou along the South Branch. The salinity value during neap tider or ordinary tide is higher than that of during spring tide.

长江河口具有分汊、心滩、串沟和江心沙岛等地貌形态,系典型的潮汐分汊河口。咸潮入侵形式有外海直接入侵、倒灌、漫滩归槽和浅滩通道水体交换等四种类型,形成其特有的盐度时空变化规律,导致南支主槽存在一个氯离子含量比其上下游均要高的高氯度带,以及大潮期盐度低,小潮或寻常潮期间盐度反而高等特殊现象。

 
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