陡溝 的英文怎麼說

中文拼音 [dǒugōu]
陡溝 英文
dougou
  • 陡 : Ⅰ形容詞（山勢峻峭; 坡度大） steep; precipitous Ⅱ副詞（陡然; 突然） suddenly; abruptly
  • 溝 : 名詞1 （挖掘的水道或工事） channel; ditch; gutter; trench 2 （淺槽;似溝的窪處） groove; rut; furr...
  1. Component and identification of depositional systems on the steep slope and gentle slope of a half - graben of the huagou sag in the dongying depression

    花溝地區單斷湖盆陡坡帶和緩坡帶沉積體系的組成與識別
  2. 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。
  3. Analytic method for computing sediment concentration in eroding rills on steep slope

    確定陡坡細溝侵蝕含沙量的解析方法
  4. Lie of the mountain precipitous vigorous and rough, strange mountain different peak, glacier and cliffside spring in the gully, size high mountain lake and wide one forest, meadow, various kinds of exotic flowers and rare herbs, rare birds and animals, form scene, mountain region of plateau, that show unique characteristics

    四姑娘山山勢陡峭蒼勁粗獷，山溝內奇山異峰冰川飛泉，大小高山湖和廣闊的森林草地，各種奇花異草珍禽異獸，構成了獨具特色的高原山地風光。
  5. The pivilion is lying on the adamellite of craggedness with freely ravins. it ' s the best place to look at the sunrise

    望海樓所在地主要巖性為24億年左右形成的二長花崗巖，山勢陡峭，溝壑縱橫，是蒙山觀日出的最佳之處。
  6. Mt. haizi is well - grown due to glacier process in the a quarterary period age of man. a vast of longstanding glacier remains stretch in the distance with steep valley wall and flat valley bed. the valley is typically formed " u " shape

    海子山第四世紀冰川作為極為發達，古冰川遺跡分佈廣泛，在夏塞峰德南坡幾條溝均為古冰川穀，谷壁陡立，谷底平坦，為典型的「 u 」型冰川。
  7. With the comparison of potential ravine and real ravine, it can reflect the developing tendency of ravine in this area. through positioning with gps and investigation in this area, we can divide the potential ravine of this area into three forms, that is parallel ravine area steep ripe ravine area and evenness swamp area. it can provide scientific reference for forest management and tree planting, and it is a new theory to prevent soil and water loss, and carry through the ravine controlling by people

    在數字化生成的帽兒山地區dem基礎上，通過二次開發生成的潛在溝系，具有與現實溝系高度的吻合性，並通過與現實溝系的比較，能客觀的反映出該地區溝系發生、發展的趨勢，藉助于gps的定位及實際踏查研究，可將帽兒山地區的潛在溝系劃分為平行溝系區、陡坡顯溝區和平坦沼澤區三種類型，可為合理的森林經營和植樹造林提供科學的借鑒，並為防止水土流失，進行溝系治理提供了新的理論依據。
  8. The solidity dykes is the basic guarantee. with the heightening of the dykes of the yellow river every year, it became higher and steeper. there are many rills and puddles on the dyke slopes

    由於黃河大堤逐年加高，大堤形成了高且陡的土坡，每逢暴雨後，在黃河大堤堤坡和戧坡區常有條條水溝以及戧臺區的、水穴（浪窩） 。
  9. And we pointed out the evolution of the first group which is the biggest level from north to south basically is limited by shaanbei syncline structure, the evolution of second group which is the mid - level form east to west or from west to east basically is limited by the bedrock joints, the evolution of the last one, which belongs to small level is limited by loess joints

    經過分析和研究，認為黃土圾區是以厚層黃上體為載體的特殊地貌景觀，其自身溝道發展演化具有特殊性，以魚鱗狀黃土崩塌為主的高角度陡傾河谷的加寬發展方式為特點，構成洛） 11式河谷發展演化模式。
  10. Because there are so many cypress trees and the valley is too much narrow, your view will be blocked when climbing

    登山者在柏林山溝內一路攀登，山陡溝窄，視線受阻。
  11. Most deep ocean basins range in depth from about 4 to 6 kilometers, with some narrow trenches near pacific ocean basin margins dropping to as low as 11 km below sea level

    大多數海盆在深度上從4公里到6公里左右，在太平洋附近海盆邊緣有些狹窄海溝可以陡降到海平面以下11公里處。
  12. Rising middle mountains abounds with steep slops and cliffs and monoclinical middle mountains high slants. this make them easy to collapse in high slants and slope failure usually happens in acclinal slopes. regional geology structure exerts an obvious constraints on the water system of the dazhaigou - haizigou valley

    斷塊隆升中山坡面多陡坡和峭壁，單斜中山的逆傾坡以峻坡為主，易產生林金沙江白鶴灘水電站庫區大寨溝、海子溝流域泥石流形成環境與流量研究料崩塌，而單斜中山的順傾坡上易形成滑坡。
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