河流階地 的英文怎麼說

中文拼音 [liújiēde]
河流階地 英文
fluvial terrace
  • : 1 (天然的和人工的大水道) river 2 (指銀河系) the milky way system; the galaxy 3 (特指黃河) t...
  • : Ⅰ動1 (液體移動; 流動) flow 2 (移動不定) drift; move; wander 3 (流傳; 傳播) spread 4 (向壞...
  • : 名詞1. (臺階) steps; stairs 2. (等級) rank 3. [醫學] (耳蝸的三個螺旋管的任一個) scala 4. [數學] order 5. [地質學] stage
  • 河流 : rivers; stream
  1. On the basis of remote sensing technique ' s good characteristic with large - area, multi - time, multi - photograph variety, manifold abundant spectral information and high ground resolution, the fault tectonics frame, river geomorphy ( such as terrace, floodplain, shoal, etc ) and suspended load, etc. were explained after analyzed the fault tectonics, river geomorphy, characteristic in the tm image by gray bar statistics, primary component analyses, tm741 image integration, line convolve enhancement and model recognition etc. especially 9 piece of fault tectonics were explained in this thesis, in succession, the impacts of the factors severally were analyzed

    遙感技術具有大范圍、多時相、多片種、多層次、含有豐富的光譜信息及具有較高的面解析度的特點。本文利用該技術,運用灰統計特徵分析和主成分分析、 tm741多波段融合、線性卷積增強、模型提取等一系列遙感解譯分析方法,分析了斷裂構造、貌(、漫灘、沙洲)及懸浮物等在tm遙感圖象上的影像特徵,解譯出了安徽南部斷裂構造格架、貌和懸浮物的分佈,並新解譯出了9條近東西向的斷裂。
  2. The analysis on the development of alluvial and lake landform in fen river drainage basins

    中更新世中晚期以來汾段性發育及成因分析
  3. The material sources of the zhangxia loess which is exposed on the terraces in zhangxia of changqing region of jinan are complicated, including materials transported by northwestern current and eastern bohai bay current and the local pluvial sediments

    其中出露在的濟南市長清區張夏鎮的黃土物質來源復雜,既有西北氣、東部渤海灣氣搬運而來的物質,又有當生成的坡洪積碎屑物質。
  4. Dig jade is it leave riverbed in river valley terrace, do beach to refer to, ancient river and alluviation, diluvian gravel that fan have dig seeking and d jade gravel of the layer in front of the mountains the jade of these places is brought by the flowing water too

    挖玉是指離開床在干灘古道和山前沖積洪積扇上的礫石層中挖尋和闐玉礫。這些方的玉也是由水帶來的。
  5. It is indicated that the loess was mainly formed in late epipleistocene. and its sediment indexes can be compared with that of loess plateau roughly, though they have different formation causes and provenance

    研究表明,二級形成於13000 8500abp ,一級形成於4000 500abp ,漫灘是現代作用的產物。
  6. The ledo road and the pipeline went through some mostly uninhabited areas of burma with some of the most difficult terrain in the world, including tropical rain forest, torrential streams, terraces and canyons, jungle - covered mountains and swampy valleys

    利多公路和輸油管道線經過一些緬甸的主要是無人區的段,這些段有著世界上極端困難的理環境,如熱帶雨林、急面和峽谷、布滿叢林的山脈和多沼澤的谷。
  7. ( 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、通過高程?面積分析、襲奪綜合分析、黃土的碳- 14測年與沉積指標分析及環境考古方法,本文重點研究了魯中南山第四紀貌發育的格局與過程。
  8. At the end of late pleitocene, influenced by the climate of glacier period, the last great event of the region in the geological time was taken place so that the migration and extinction of organism species were resulted, loess accumulation was generally developed throughout the whole region, in the holocene, the most important environmental change was fluvial process, which was still influnced by two factors - neotectonics and palaeoclimatic changes

    更新世晚期末,受末次冰期氣侯的影響,本區發生了史時期的最後一次大事件,造成了物種遷移和絕滅,全區廣泛發育黃土堆積。進入全新世,本區環境變化以作用最為顯著,沉積物主要分佈在各大水系的谷中,構成一、二級和近代床與漫灘堆積。
  9. Normally water resources is affected by human activities and climatic change, but it is affected mainly by climatic change in runoff forming regions located in the high and middle mountainous area in the northwestern china. river runoff in the hexi inland arid region all originates from the qilian mt. area and the change of mountainous runoff resulted from global weather warming up and will bring an important effect to the development of society and economy in the hexi region. so the response on mountainous runoff and its changing trends are analyzed on the basis of the measured data of precipitation, air temperature, and discharges observed from some weather and hydrologic stations in the studied area. the results show that seasonal variation of mountainous runoff in the hexi inland region is mainly affected by the river ' s geographical location and supply source, and the yearly change by precipitation and that in the west of the region by air temperature besides precipitation. there are some obviously regional differences in the influences of climatic change on surface runoff in the hexi inland arid region, that is, rivers runoff in the west of the hexi area have been increasing and rivers in the east part have been decreasing, and the rivers runoff in the central part presented slowly increase trend, such as the heihe river, but it is not quite obvious

    一般情況下,水資源的變化主要受氣候變化和人類活動的影響,但在位於我國西北內陸乾旱區的中高山帶,徑的形成主要受前者的影響.甘肅省的西內陸乾旱區是該省重要的工農業生產和經濟開發區,這里各項社會和經濟活動與出山徑的變化都有著十分密切的關系.因此,筆者根據有關水文氣象臺站的降水、氣溫和徑觀測資料,分析了以黑、昌馬、西營等主要為代表的西內陸區出山徑的變化特徵與規律.結果表明,西內陸區出山口徑的季節變化主要受理位置和補給來源的影響,而年際變幅則受山區降水量年際變化及變幅的影響十分明顯.目前,梨園以西水量處于上升段,梨園以東的則處于下降的段;以黑鶯落峽水文站年徑為代表的走廊中部區的出山口徑正處於1990年開始的枯水段的上升段.但總體而言,西內陸乾旱區出山口徑的變化相對比較穩定.預計今後若干年內,西內陸乾旱區東段出山口徑的變化以偏枯為主,中段、西段出山口徑的變化以平水或平水偏豐為主
  10. ( 5 ) by analyzing the terrace in the lacustrine sediment of the ancient barrier lake, diexi, minjiang river, forming of the terrace is not only because of the intermittent arising of the tectonic movement, but also because of descend of the eroding normal covering resulting from destroying of the barrier lake

    ( 5 )通過對岷江疊溪古堰塞湖湖相沉積中的河流階地分析可知,的形成不僅僅是由於新構造運動的間歇性抬升作用,由於堰塞湖的潰決引起洪水下泄,導致侵蝕基準面的下降也可以形成
  11. Here one can admire the river terraces, eroded caves, the stratum surface, the table mountain terrain, crumbling cliffs, while places like qingshuiguan, the old ferry crossings, the ancient trees and the old paths along the yellow river give the ancient qingling mountain cliffs a human touch

    這里可欣賞河流階地,側蝕洞穴,層剖面,方山貌,重力崩塌貌… …清水關,古渡口,古樹落,黃古道又給遠古清冷的山崖增添了人文氣息。
  12. This theme selected weihe river round tianshui, jinhe river round binxian, bahe river round lantian and luohe river round luochuan to study the evolutionary model of river terraces in the mid - tail of weihe river. we have built the cross - section of each river, and analyzed the evolution of each river terrace in the mid - tail of weihe river according to the velocity of downcuting and lateral erosion

    本論文以天水渭南鎮段渭、彬縣段涇、藍田段灞和秦家段洛為例建立渭中下遊河流階地演化模式,以形成年代為標尺,根據下切速度和側蝕速度對渭中下游各的演化過程進行了分析。
  13. However, people studied the riverway mainly by field survey and landform map contrast before. because of the limits of man ' s field view and complexity of field survey route, it is a difficult bottle neck for people to make synthetical analysis on geological structure, yangtze river shoal, floodplain, terrace, and microcosmic suspended load on macroscopical scale

    而以往的道研究大多數是通過面調查和形圖室內對比分析來研究的(少數運用航片) ,由於受人的視域范圍及調查工作路線的布置的復雜度影響,對區域宏觀尺度下的質構造、長江沙洲、漫灘、微觀領域的懸浮物等作綜合性的研究便成為了瓶頸。
  14. The initial people pick up beautiful and d the jade in the riverside, later again will arrive in the rivers fishes for the egg circular the sub - jade, again afterwards dug out these early rivers chongjiwu center from the river valley step gravel the beautiful jade ; again along the river traced subsequently discovers the growth bound primary in the rock yukuang

    最初人們在邊拾起美麗的和闐玉,以後又到中撈取卵圓形的子玉,再后來從谷的砂礫中挖出那些早期沖積物中的美玉再沿追溯繼而發現了生長在巖石裹的原生玉礦。
  15. Based on analysis of magnetic effect mechanism of alluvial cohesive soil, according to the distribution and character of river alluvial cohesive soil of first and second terrace of yongjiang river of nanning, pore water chemical characteristic, especially total iron content in pore water and holding form of iron ion in pore water, this text preliminarily divides the river alluvial cohesive soil of first and second terrace of yongjiang river of nanning into two magnetic effect region : reinforced region and weaker region of magnetic effect

    摘要在分析粘性土磁效應機理的基礎上,根據? 、級沖積相粘性土的分佈及其特性和孔隙水化學特性,尤其是孔隙水中的總鐵含量以及鐵離子的賦存形式,將南寧市邕江? 、級沖積相粘性土初步劃分為磁效應強化區、磁效應較弱區兩個磁效應區。
  16. The same grade terrace height beside the river is surveyed at almost the same level, proved that the hidden fault under the river never moved after

    經測量兩側相對應的同級面處在相同的高度上,證明自晚更新世大凌三級形成以來位於大凌床底部的隱伏斷裂沒有過活動。
  17. The dalinghe hidden fault, as an example in this paper, is just located under the dalinghe river, so the activity of this hidden fault can be defined by comparing quaternary layers and terraces beside the river hidden fault. based on spore analysis of 17 layers and several

    以大凌隱伏斷裂為實例,根據斷裂位於大凌床底部的特點,通過對比斷裂兩側的第四紀層和,對隱伏斷裂的活動性進行研究。孢粉分析和
  18. Nowadays the real estate and construction of highway are flourishing in fujian province. a lot of projects are built on a site of the mountain area or along the rivers

    福建省房產業和高速公路建設正處在蓬勃發展段,但由於處山區、極其發育,許多建設工程都在山、江邊等高窪不平的帶建設與施工。
  19. On the basis of the typical weather situation in huaihe river basin in 1998, the paper analyses the features of the land temperature of huaihe river basin in the four stages of the 1998 s meiyu of yangtze

    最後結合1998年淮域試驗加密觀測期間的主要天氣形勢,分析了江淮梅雨4個段相對應的面溫度的特徵。
  20. The evolution of the river terraces in the mid - tail of weihe river has these characteristics

    中下游區各的各級的形成時間大致是同步的。
分享友人