地貌发育的英文

• geomorphic development

• "地貌"英文翻译    the general configuration of ...
• "发育"英文翻译    growth; development; auxe; e ...
• "地貌发生" 英文翻译 :    morphogenesis
• "地貌发生力" 英文翻译 :    morphogenetic force
• "地貌发生幕" 英文翻译 :    morphogenic phase
• "地貌发生学" 英文翻译 :    genetic morphology; genetic physiography; genetical morphology; geomorphogeny
• "地貌发展史" 英文翻译 :    geomorphic history
• "生物地貌发生因素" 英文翻译 :    biologic morphegenic factor
• "地貌" 英文翻译 :    (地表各种形态的总称) the general configuration of the earth's surface; topographic feature; landforms; lay of land; relief; land features of terrain; configuration of the ground; ground form◇地貌表示法 hypsography; relief representation; 地貌成因区 formkreis; formenkereis
• "发育" 英文翻译 :    growth; development; auxe; engender; grow; develop gradually by a process of growth and change 发育健全 physically well developed; 促进发育 accelerate growth; 密切注视幼儿智力的发育 intently watch the development of the infant mind; 粗劣的食物妨碍儿童的发育。 poor food arrests the natural growth of children. 婴儿发育情况良好。 the baby is coming on well.; 发育不良 [医学] stunk; dysontogenesis; maldevelopment; 发育不全 hypoplasia; atelia; ateliosis; ateleiosis; dysgenesis; stuntedness; atelo; aplasia; hypoplasty; hypogenesis; hypoplasis; agennesia; agenesia; agenesis; underdevelopment
• "地貌版" 英文翻译 :    relief plate
• "地貌的" 英文翻译 :    geomorphic; geomorphological
• "地貌甸" 英文翻译 :    geomorphic survey; geomorphicsurvey
• "地貌法" 英文翻译 :    geomorphologic method
• "地貌面" 英文翻译 :    morphologic unit
• "地貌区" 英文翻译 :    geomorphologic region; morphologic province; morphologicprovince
• "地貌图" 英文翻译 :    geomorphologic map; geomorphological map; geomorphologicalmap; profiler
• "地貌学" 英文翻译 :    [地质学] geomorphology◇地貌学家 geomorphologist; 地貌学论文 geomorphology
• "地物；地貌" 英文翻译 :    ground feature; land feature
• "古地貌" 英文翻译 :    ancient landform
• "廉地貌" 英文翻译 :    fluvial geomorphology
• "微地貌" 英文翻译 :    microrelief; microtopography
• "小地貌" 英文翻译 :    microtopography
• "地貌 地貌学 地形学" 英文翻译 :    geomorphy
• "冰崩地貌" 英文翻译 :    ice disintegration feature

• Morphological accumulation of karst cave and landform development in guizhou
  岩溶洞穴形态沉积与贵州地貌发育
• Granite geomorphic development of granite and expedited soil erosion in hengshan mountain area
  衡山土壤加速侵蚀与花岗岩地貌发育问题研究
• Tectonic movements took important roll for the evolution of alluvial landforms of the kuitun river in the northern front of the tisnshan mountains
  北天山的构造活动对奎屯河山前地貌发育起到了至关重要的作用。
• ( 2 ) by altitude - area analysis , comprehensive study on river captures , c - 14 dating , loess indexes a analysis and method of environmental archaeology , the quaternary geomorphologic evolution in csmasp is researched thoroughly
  二、通过高程?面积分析、河流袭夺综合分析、黄土阶地的碳- 14测年与沉积指标分析及环境考古方法，本文重点研究了鲁中南山地第四纪地貌发育的格局与过程。
• ( 4 ) it is the largest area of the danxia landfonn of the northwest of the yunnan province in china . there are three landscape areas include liming scenery spot , luoguqing scenery spot and shibaoshan scenery spot . it takes three scenery spots as a action research for analysis of the zig - zag pattern caused by joints , weathering , tectonic activity and magma activity
  第四，针对中国最大的丹霞地貌分布区?滇西北，以黎明黎光、罗古箐、石宝山丹霞地貌景区进行实证研究，初步分析了滇西北丹霞地貌发育的特点?大面积的龟裂现象主要由两组节理和风化作用形成的，构造、岩浆活动也对龟裂的形成起了一定作用。
• Zhengzhou mining to cross - new federated , site , opened , hunan , withdraw the army and some other cities ( and counties ) and the outskirts of zhengzhou coal tenure and forecasts 193 million tons of resources , and karst landscape development , groundwater and unusually rich bauxite resources , suitable for the construction of large power plants and aluminum plant
  郑州矿区地跨新密、登封、新郑、巩义、偃师等市（县）及郑州郊区，煤炭保有及预测资源量193亿吨，且岩溶地貌发育，地下水及铝矾土资源异常丰富，适合兴建大型电厂和铝厂。
• Based on the data of vector topographic map , the geomorphologic evolution stage of csmasp is studied with the aid of maplnfo and arc view . it is indicated that the research area is in the middle age and old age according to the davisan stage determine of geomorphologic evolution . the uplift and denuded amount in the period of neo - tectonics and the elevation of denudation surface of lincheng period ( mainly in quaternary ) are also discussed
  根据高程分析结果，认为鲁中南山地主要处于流域地貌发育的壮年、晚年期，并对鲁中南山地第四纪构造抬升量与侵蚀速率、各流域临城期山麓剥夷面的分布高度等相关问题进行了理论探讨，从理论上证明了鲁中期剥夷面难以存在。