淺谷 的英文怎麼說

中文拼音 [jiāngǔ]
淺谷 英文
asatani
  • 淺 : 形容詞1 （從上到下或從外到里的距離小） shallow 2 （淺顯） simple; easy 3 （淺薄） superficial 4 ...
  • 谷 : 谷名詞1 （兩山或兩塊高地中間的狹長而有出口的地帶） valley; ravine; gorge 2 （姓氏） a surname 3 ...
  1. They came down to the river to drink oftener, and loitered about, grazing in that low canyon so much that we began to call it cow canyon.

    它們更經常地到河邊來飲水，到處徜徉，老在淺峽谷那裡吃草，以致我們都開始管那個地方叫牛峽谷了。
  2. The coqen basin in xizang lies between the bangong - nujiang suture zone and yarlung zangbo suture zone, and once extended northwards and southwards, respectively centred by the qiekan - goicang - asog rift zone as the center of deposition and subsidence during the middle jurassic to the early creatceous. ( 1 ) during the middle - late jurassic, the rift zone was occupied by deep - water turbidites, radiolarian siliceous rocks, shallow - water carbonate rocks, clastic rocks and basic - ultrabasic rocks, while both sides of it by littoral and shallow marine elastic rocks and carbonate rocks

    摘要位於班公湖怒江縫合帶與雅魯藏布江縫合帶之間的措勤盆地，在中侏羅世早白堊世期間具有以且坎古昌阿索裂谷帶為沉積、沉降中心向南北兩側展開的古地理格局：中晚侏羅世時期，裂谷帶內由深水濁積巖、放射蟲硅質巖和淺水碳酸鹽巖、碎屑巖巖片及基性超基性巖等組成；裂谷帶兩側由濱淺海相碎屑巖和碳酸鹽巖組成。
  3. The proportion that the sediment yield of the main gully accounts for the total sediment yield of the experimental watershed model is from48. 7 % to 66. 6 %, and the proportion that deposition sediment yield of main gully accounts for the total deposition sediment yield of the experimental watershed model is from64. 9 % to 99. 4 %. the developing process of topographic feature of the experimental watershed model. expanding the gully width and cutting down the gully bottom are the two chief forms of the topographic feature development

    流域模型地貌形態發育過程溝谷擴展和下切是流域模型地貌形態發育的主要形式，溝谷擴展發育主要發生在發育活躍時段，主溝所佔溝谷總面積比例在流域模型溝谷擴展發育過程中保持在60以上：主支溝下切發育在發育初期和發育活躍時段前期表現最為劇烈，其橫剖面為v字形，在發育初期和穩定時期時段呈現淺u字形和底部較為平坦的梯形，主溝的橫剖面發育明顯優先於各支溝。
  4. The railway, on leaving benares, passed for a while along the valley of the ganges. through the windows of their carriage the travellers had glimpses of the diversified landscape of behar, with its mountains clothed in verdure, its fields of barley, wheat, and corn, its jungles peopled with green alligators, its neat villages, and its still thickly - leaved forests

    從貝拿勒斯出發，鐵路穿過一段恆河山谷，天氣相當晴朗，窗外顯示出比哈爾千變萬化的美麗景色：青翠的高山，生長著大麥小麥和玉米的田野，棲居著淺綠色鱷魚的河川和池沼，整整的村莊和四季常青的森林，幾只大象和一些單峰的駱駝正在聖河裡洗澡。
  5. The sediments of the incised valleys show an upward - fining succession, and can be grouped into four sedimentary fades : gravel lag - deposit of in - channel to partly over bank sediments of a meandering river, flood plain - estuary, estuary - shallow marine, and estuary sand bar, based on lithology, paleontology, and sedimentary textures and structures

    根據巖石學、沉積結構和沉積構造特徵，本區下切河谷充填沉積物具有向上變細的沉積層序，可以劃分為4個沉積相類型：河床滯留沉積物到部分曲流河沉積體系的邊灘沉積、河漫灘河口灣沉積、河口灣淺海沉積和河口灣砂壩沉積。
  6. All the valley at my right hand was full of pasture - fields, and cornfields, and wood ; and a glittering stream ran zigzag through the varied shades of green, the mellowing grain, the sombre woodland, the clear and sunny lea

    我左側的山谷滿眼都是牧地玉米地和樹林。一條閃光的小溪彎彎曲曲地流過深淺各異的綠蔭，流過正在成熟的稻穀，暗淡的樹林，明凈而充滿陽光的草地。
  7. The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement, while the cover has undergone the evolution of intra - continental rife in permian, down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary. the main sediments are huge - thick volcanic rock, shallow intrusive rock and tuff in early permian, dark mudstone, marl and muddy dolostone in lucaogou formation in middle permian, huge thick volcanic rock, intruder in tiaohu formation in middle permian, miscellaneous sandy gravel, sandstone and gray mudstone in triassic ( the red is under the gray, and huge - thick dark gray, gray sandy gravel, sandstone, mudstone with coal layer in jurassic

    盆地基底由前寒武紀結晶基底和古生代褶皺基底組成，盆地蓋層則經歷了二疊紀的裂谷盆地、三疊紀?白堊紀的坳陷盆地和第三紀后的山間盆地的演化過程。盆地主要沉積了下二疊統巨厚火山巖、淺成侵入巖和凝灰巖；中二疊統蘆草溝組的暗色泥巖、泥灰巖、白雲質巖石以及條湖組的巨厚層火山巖、侵入巖；三疊系雜色砂礫巖、砂巖及灰色泥巖（下紅上灰） ；以及侏羅紀厚層深灰、灰色砂礫巖、砂巖、泥巖夾煤層。
  8. The main conclusions and cognitions are as follows : ( l ) rockmass weathering should be studied from either microcosmic and macrocosmic, microcosmic contain includes of mineralogy and of lithology, and in macrocosmic, weathering action damages integrality of rockmass, so studying rockmass structure can open out weathered degree of epigenetic - surface rockmass. ( 2 ] the dissertation sums up the characteristic indexes which can token weathered and unloaded degree, simultaneously, puts forth and summerizes several methods that classifies different weathered and relaxed zones of slope rockmass. ( 3 ) river valley epigenetic - surface reformation is controlled by rockmass structure, but weathering and unloading of rockmass is the direct cause which leads to different epigenetic - surface physical geology phenomena, for example, collapse, landslide, incline, dynam - relaxed and so on

    本文主要結論與認識為： （ 1 ）對于巖體風化的研究從微觀與宏觀兩方面入手，微觀方面重視對礦物學、巖石學的研究，宏觀方面，上升到巖體結構被改造的高度進行研究； （ 2 ）歸納了表徵巖體風化、卸荷程度的特徵指標並提出了劃分巖體風化、卸荷程度的幾種方法； （ 3 ）巖體結構控制著河谷淺表改造，但導致崩塌、滑坡、傾倒、松動等表生物理地質現象的直接原因乃是巖體的風化、卸荷。
  9. Here the landscape was whitey - brown ; down there, as in froom valley, it was always green

    這兒風景的顏色是一種淺褐色再往下就和佛盧姆谷一樣了，差不多成了青綠色。
  10. And i think he ' s trying to get into your slacks

    而他正想要進入你那小山間的淺谷
  11. Perfect landform : the course is characterized by shallow valleys and a rolling terrain, which is quite unique in china and exactly suitable for a golf course

    地形絕佳：具有淺谷及緩坡地形的高爾夫球場，擁有起伏適中的坡度，是國內難得一見的高爾夫球地形。
  12. I ve got other provision. they looked up the shallow valley at the mine, and beyond it, at the black - lidded houses of tevershall crawling like some serpent up the hill

    他們在那淺谷的上頭，遙望著煤礦場和礦場後面那些達娃斯哈的黑頂的屋宇，好象蛇似沿著山坡起著。
  13. European annual with pale rose - colored flowers ; cultivated flower or self - sown grainfield weed ; introduced in north america ; sometimes classified as a soapwort

    開有淺玫瑰紅花朵的一年生歐洲植物；谷地里自我受精或人工栽培；原產北美；有時歸皂莢屬。
  14. The inside is as impressive as the outside. from the tokyo metro hibiya line and toei subway asakusa line ginza ( about 2 minutes walk ) or from jr yurakucho ginzaguchi, go straight along harumi - dori, at the another side of ginza mitsukoshi

    東京地鐵日比谷線、都營地鐵淺草線東銀座站步行約2分鐘；或者由jr有樂町站銀座出口方面出晴海大道直進。
  15. Wave off into shallow waters, seabed by the friction effect change steep wave front, trough ice, water points trajectory showed reciprocating flow, but also to the shore into the flow speed usually return rate greater than offshore, the net result of sediment at the bottom to the shore handling, and was the shock waves on the shore with the water current - riviera online accumulation

    外海波浪傳入近岸淺水區，受到海底的摩擦作用，波鋒變陡、波谷變緩，水質點運動軌跡呈現往復流動，而且向岸進流速度通常大於離岸迴流速度，導致底部泥沙凈向岸搬運，並被激岸浪的上沖水流帶至海濱線上堆積。
  16. Based on the analysis of a large number of drillings, the static sounding and chemical data obtained from the present hangzhou bay coastal plain, this paper presents the sedimentary facies and architectures of the qiantangjiang river and taihu incised valleys, and the characteristics of shallow gas reservoir distribution

    摘要根據杭州灣沿海平原大量的鉆井、靜力觸探井和分析化驗等資料，研究了下切河谷（錢塘江和太湖下切河谷）充填物的沉積建造和沉積相，以及淺層生物氣藏分佈特徵。
  17. The environment in dhv is facing the serious vulnerable period in the history due to its nature situation of half - year dry period, fragile geological structure and shallow soil, and its social situation of over dense population and over farming

    由於乾熱河谷地區的地質結構不穩定、土層淺薄、人口膨脹、過度耕種，尤其長達半年的旱季等原因，導致該地區的生態環境處于極端的脆弱階段。
  18. From the tokyo metro marunouchi line, ginza line and hibiya line ginza, about 5 minutes walk. from toei subway asakusa line higashiginza, about 3 minutes walk. from jr yurakucho, about 8 minutes walk and from jr tokyo, about 10 minutes walk, along showa - dori

    由東京地鐵有樂町線和銀座1丁目站步行約3分鐘；由東京地鐵銀座線、丸內線、日比谷線東銀座站步行約5分鐘；由都營地鐵淺草線和東銀座站步行約3分鐘；由jr有樂町線站步行約8分鐘； jr東京站步行約10分鐘。
  19. The soils in the region were characterized by thin layer, weak structure, gravel / fragmental composition, compacted surface and drought, etc. soil water properties are important factors affecting vegetative rehabilitation in spite of low soil organic content and lack in soil nutrients

    乾熱河谷的土壤特徵表現為土層淺薄、土壤結構差、土壤石質粗骨性強或表土緊實、土壤乾旱等。雖然土壤有機質含量低、有效養分也較缺乏，但是土壤水分性質是植被生長恢復的關鍵制約因素。
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