湖平面 的英文怎麼說

中文拼音 [húpíngmiàn]
湖平面 英文
lake levels
  • 湖 : 名詞1 （被陸地圍著的大片積水） lake 2 （指湖州） short for huzhou3 （指湖南、湖北） a name referr...
  • 平 : Ⅰ形容詞1 （沒有高低凹凸 不頃斜） flat; level; even; smooth 2 （高度相同; 不相上下） on the same l...
  • 面 : Ⅰ名詞1 （頭的前部; 臉） face 2 （物體的表面） surface; top 3 （外露的一層或正面） outside; the ri...
  1. For the first week ， whenever i looked out on the pond it impressed me like a tarn high up on the side of a mountain ， its bottom far above the surface of other lakes ， and ， as the sun arose ， i saw it throwing off its nightly clothing of mist ， and here and there ， by degrees ， its soft ripples or its smooth reflecting surface was revealed ， while the mists ， like ghosts ， were stealthily withdrawing in every direction into the woods ， as at the breaking up of some nocturnal conventicle

    在第一個星期內，無論什麼時候我凝望著湖水，湖給我的印象都好像山裡的一泓龍潭，高高在山的一邊，它的底還比別的湖沼的水平面高了不少，以至日出的時候，我看到它脫去了夜晚的霧衣，它輕柔的粼波，或它波平如鏡的湖面，都漸漸地在這里那裡呈現了，這時的霧，像幽靈偷偷地從每一個方向，退隱入森林中，又好像是一個夜間的秘密宗教集會散會了一樣。
  2. Because ancient lakes on the south coastal plain of laizhou bay lie in transitional area between sea and land, they receive the influence of sea level changes, river diversion, diastrophism and the activities of human beings, so the course of formation and change of ancient lakes are very complicated

    該區的古湖泊，處于海陸交互的復雜環境中，受到海平面變動和氣候變化的深刻影響，同時也受到河流變遷、地質構造變動、人類活動的影響，其形成與演變過程十分復雜。
  3. Hangzhou yuhang chengnan line factory organized in 1993, was located the beautiful hangjiahu plain of hangzhou yuhang disctrict linping town, the close neighbor no. 320 national highways and the huhang highway near linping exit, the geographical position superior, the transportation was extremely convenient, this factory area amounted to 2, 500 square meters, the floor space reaches 700 even aspects, at present the staff has 29 people, technical personnel had 3, the factory main equipment has the dye vat, the system line machine and so on the special - purpose supplementary equipment, the fixed asset more than 2 million yuan, at present main production ribbon product and so on black silk ribbon line, nylon line, real silk thread, produces high mainly sells to hangzhou, shanghai, and the peripheral locality, the product quality deeply user communities ' faith, this factory by the science management, the rich experience and the advanced technology and the craft, had guaranteed this factory product high level, the high quality, simultaneously continuously pursue the good prestige, take the customer demand foundation of as the enterprise survival, welcome the new old customer to come this factory service discussion, communal development

    杭州餘杭成楠制線廠創辦於1993年，位於美麗的杭嘉湖平原杭州市餘杭區臨平鎮，緊鄰320國道及滬杭高速公路臨平出口處，地理位置優越，交通十分方便，該廠佔地面積達2500平方米，建築面積達700平方面，目前職工有29人，其中技術人員有3名，工廠主要設備有染缸、制線機等專用配套設備，固定資產200多萬元，目前主要生產絳綸線、尼龍線、真絲線等產品，產高品主要銷往杭州、上海、及周邊地區，產品質量深受廣大用戶的信賴，該廠以科學的管理，豐富的經驗及先進的技術和工藝，保證了該廠產品的高水平、高品質，同時一直追求良好的信譽，以客戶的需求為企業生存之本，歡迎新老客戶前來該廠業務洽談，共同發展。
  4. Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area

    詳細的沉積相研究發現，紅獅地區第三系發育有沖積扇、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇7種主要沉積相類型，並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖，以較高的時間解析度揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律，比如在北部的凹陷陡坡背景下，上升半旋迴低水位期通常發育有水下扇、湖底扇等陡岸近源特徵的沉積體系，下降半旋迴高水位期，扇三角洲相粗碎屑巖由北向南進積;在南部的凹陷緩坡背景下，上升半旋迴主要發育辮狀河流相，下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相沉積和鹽類沉積。
  5. Compared c13 & o18 isotope analysis curve with lake level curve, further analyzed palaeoenvironment

    通過分析、對比碳氧同位素曲線與湖平面升降曲線，對古沉積環境的變化規律有了進一步的認識。
  6. On the basis of the feature of paleostructure, paleogeography and lake level fluctuation in chang - 6 to chang - 8 oil - bearing layers, this text researchs paleogeographic feature and evolution. chang - 8 stages are the early days of lake basin outspread, chang - 7 stages are steadies stage of lake basin outspread, chang - 6 stages are shrinkage of lake basin, the lake level slowly droping, lake strandline moving eastward

    根據古構造、古地理、湖平面升降等特點研究了長_ 6 ?長_ 8期巖相地理特點及其演化，長_ 8期是湖盆擴大的初期；長_ 7期為湖盆擴大階段中穩定期；長_ 6期為湖盆擴大階段中開始萎縮，湖平面繼續緩慢下降，湖岸線向東遷移。
  7. Located in the middle section of xiuhe river, and striding yongxiu county and wuning county, talin lake covers an area of 308 square kilometers and possesses 997 peculiar and difform islands

    柘林湖位於修河中部，地跨永修、武寧兩縣，湖區面積308平方公里，有997座大小不一、形態各異的島嶼，被譽為「一級空氣、一級水質的休閑度假樂園。 」
  8. The fall of global sea level during the last glacial maximum enhanced the fluvial gradient and river cutting, resulting in the formation of the large - scale qiantangjiang river and taihu incised valleys which were subsequently filled and rapidly buried in the post - glacial period, with the paleointerfluve being exposed to air on both flanks of the incised valleys

    末次冰盛期，海平面下降的幅度大，增加了河流梯度、加強了下切作用，形成了錢塘江和太湖下切河谷，隨后在冰後期被充填和埋藏，下切河谷的兩側為暴露地表的古河間地。
  9. That the black mudstone deposited in deep water interbedded with salt and gypsum deposited in shallow water shows that during the sedimentation of 3 ( superscript rd ) and 4 ( superscript th ) sub - member, the lake level changes frequently

    也正是由於湖平面變化頻繁，在沉積中心的周圍主要物源方向上形成一系列低水位期的砂體。
  10. Depositional cycles on basin scale have been interpreted as the result of depositional response to tectonism such as episodic rifting, polyphasic compressive flexural subsidence and reversion, and differential subsidence of fault blocks ; while the formation of high frequency sequences was attributed to variation in lake level and sediment supply

    盆地規模的沉積旋迴多是盆地幕式裂陷、多幕擠壓撓曲沉降、多期構造反轉、斷塊差異沉降等構造作用的沉積回應；高頻層序單元的發育則主要與湖平面和沉積物供給量的變化有關。
  11. The maincharacter of pollen assemblages in the site was the peaks of typha in the final stage of the liangzhu culture and dominant proportion of typha in the maqiao culture, denoting large water areas around the site

    該遺址孢粉記錄表明，良渚文化晚期和馬橋期出現大量的香蒲，遺址周圍池塘沼澤面積較大。 2 、太湖流域新石器時期文化遺址的興衰與地勢、氣候、海平面的變化以及太湖碟形湖盆體系的發育密切相關。
  12. Combined with the existing problems of the national key project - linhuaigang flood - control project, this paper systematically studied the theories of sluice structures design foundation model modern calculation methods of both plane and spatial sluice structures ; at the same time, static and dynamic analysis of he spatial structure of the jiang tang lake ' s flood - entry sluice was studied using the finite element method

    本論文結合國家重點水利工程臨淮崗洪水控制工程中遇到的實際問題，系統地研究了水閘結構的設計理論、地基模型、平面和空間水閘結構的現代計算方法；並對姜塘湖進洪閘空間結構進行了有限元靜動力計算分析。
  13. The formation and evolution of the sequence stratigraphy of the yanchang formation are governed by slow tectonic subsidence, warm humid climates, sediment supply and lake - level fluctuations

    延長組層序地層的形成與演化主要受控于當時緩慢的構造沉降、溫濕氣候、陸源碎屑物源供給及湖平面升降等地質因素。
  14. In the present paper, a complete attribute and spatial database on anpsp is designed and created in three different levels of scale, hang - jia - hu plain ( 1 : 250000 ), pinghu city ( 1 : 50000 ), and field experiment ( 1 : 2000 ). based on the gis technique, especially webgis technique ( arcims, arcsde ), an agricultural non - point source pollution information system ( anpspis ) has been established in order to serve the management, planning and decision - making of anpsp in hang - jia - hu water - net plain

    本文以太湖流域杭嘉湖地區的1 250000 （杭嘉湖平原） 、 1 50000 （平湖市） 、 1 2000 （樣板區）三種不同比例尺的系統研究為例，建立了一整套農業面源污染的屬性和空間數據庫，通過利用gis及其相關技術，特別是webgis技術（ arcims 、 arcsde ）的應用，建立了一個基於webgis的農業面源污染信息系統（ anpspis ） 。
  15. High frequency lake - level change of 3rd member of shahejie formation and prediction of lowstand sand body in dongpu depression

    東濮凹陷沙三段高頻湖平面變化及低位砂體預測
  16. The climate controls different types of sequences by affecting the relations between rainfall and evaporation

    氣候通過降雨量和蒸發量的關系影響湖平面，進而控制層序類型。
  17. Experimental process shows that variance of underwater distributary channel and declining rate of lake plane are closely related to moving intension of motive soleplate

    實驗過程顯示，水下分流河道的變遷與湖平面的下降速率及活動底板的運動強度密切相關。
  18. For tianjin olympic center stadium project, parameters determination of a natural lake used as cooling pond and the layout plan of the lake were introduced, including the flow scheme of recirculating cooling water system, calculation of heat released from cooling pond, engineering arrangement for the lake, and the lake water treatment, etc

    摘要結合天津奧林匹克中心體育場工程，介紹了利用天然湖作為冷卻池的參數確定及湖平面設計，具體包括冷卻循環水系統流程、冷卻池排熱量計算、冷卻湖的工程布置、湖水水質處理等。
  19. The integrated study of heavy mineral, palaeocurrent direction, and sedimentary facies distribution has disclosed that the detritus are derived chiefly from the southeast and east - northeast during the deposition of the yanchang formation in the late triassic. the variations in the palaeocurrent directions have consequences for the development and distribution of the sequence stratigraphy and sedimentary facies of the yanchang formation. the major and trace element analyses of the mudstones from the yanchang formation also show that the lake waters would be freshened to brackish

    初次通過泥巖常、微量元素測試資料和沉積學分析得出，延長期富縣探區湖泊水體屬于淡水-微鹹水，微量元素含量及其比值在剖面上的變化對延長期湖平面升降和氣候的演變具有良好的響應，湖平面升降、氣候演變對層序地層的發育有著直觀而又重要的影響。
  20. Rhythmicility or periodicity of the depositional strata is influenced by the fluctuation of sea - level to a certain extent, but it must be the response of depositional course to the structural activity in extensive significance

    研究表明，沉積巖層的韻律性或旋迴性特徵在一定程度上受海（湖）平面變化影響，但從更加廣泛的意義上來看，應是沉積過程對于區域地質背景波動的響應，其主控因素是構造波動。
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