河口坝的英文

• estuary dam
• river mouth bar

• "河口"英文翻译    the mouth of a river; estuar ...
• "坝"英文翻译    dam dyke; embankment
• "堵口坝" 英文翻译 :    closure dam
• "缺口坝" 英文翻译 :    notch dam
• "湾口坝" 英文翻译 :    baymouth bar
• "河口" 英文翻译 :    [地理学] river mouth; stream outlet; estuary; outfall◇河口地貌 estuarine geomorphy; 河口港 estuary harbour; 河口湖 estuarine lake; 河口泥沙 estuary sediment; 河口生态学 estuarine ecology; 河口生物 estuarine organism; 河口湾 firth; frith; estuary; 河口淤积 estuary sedimentation
• "河口；河口湾" 英文翻译 :    estuarine
• "河口河口" 英文翻译 :    kuala; muara; river mouth
• "冰河口" 英文翻译 :    ice stream
• "波河口" 英文翻译 :    foci del po
• "草河口" 英文翻译 :    caohekou
• "叉河口" 英文翻译 :    bifurcation area
• "大河口" 英文翻译 :    dahekou
• "关河口" 英文翻译 :    guanhekou
• "灌河口" 英文翻译 :    guanhe kou
• "河、河口" 英文翻译 :    esteiro; kuala
• "河口, 港湾" 英文翻译 :    estuary
• "河口、口" 英文翻译 :    mahana
• "河口，江口" 英文翻译 :    estuaries
• "河口；流出" 英文翻译 :    debouch
• "河口层" 英文翻译 :    estuarine deposite
• "河口潮" 英文翻译 :    estuary tide
• "河口岛" 英文翻译 :    innis
• "河口的" 英文翻译 :    estuarial; estuarine
• "河口段" 英文翻译 :    estuary

• Physical simulation of formation process in distributary channels and debouch bars in delta
  三角洲分流河道及河口坝形成过程的物理模拟
• The more favorable reservoir sandbodies are submerged distributary channel sandbodies and debouch bar sandbodies on delta front
  较有利的储集砂体为水下分流河道或河口坝砂体。
• As getting incision of underwater distributary channel in different period , debouch bar keeps short time and low - development
  由于受到不同期水下分流河道的切割，河口坝保持时间较短而欠发育。
• The main sedimentary microfacies are submerged distributary channel , debouch bar , submerged natural levee and flood - plain splay . the research shows that the physical property of subermerged distributary channel sandbodies are the best and debouch bar comes second
  长4 + 52长62油层砂体的沉积微相类型主要有水下分流河道、河口坝、水下天然堤和水下决口扇等，其中水下分流河道砂体的物性相对最好，其次为河口坝砂体。
• And the delta genetic unit includes distributary channel , distributary bay , small lake of delta plain , swamp , distributary estuary bar , frontal delta mud and sandy density flow and so on . the fluvial system is composed of channel , channel side and flooding basin
  其成因相包括分流河道、决口扇及决口河道、分流间湾、三角洲平原小型湖、沼泽、分流河口坝、前三角洲泥及砂质重力流等；该区河流体系由河道、河道边部及泛滥盆地等沉积组合构成。
• Even if the same genetic face , the velocity is very different because of different location . for example , the velocity of the vicinity and beyond of estuary bar is respectively 238 . 33mm / ka and 0 . 89 mm / ka . the paper has also related the deposital velocity of delta with quite deep lake of eogene of jiyang basin and the okinawa trough of quaternary and contemporarily shore
  即使是同一成因相，其所处的位置不同，沉积速率也有较大的差距，如分流河口坝(近端)与分流河口坝(远端)的沉积速率分别为238 . 33mm / ka和0 . 89mm / ka 。
• The south part was slope and deep floor of the lake , and the north part was a broad shallow - water platform of the latchstring shore . in the north part , chang - 6 and chang - 7 oil - bearing beds of yanchang formation were typical shallow - water platform delta with an incomplete progradational sequence , in which the delta plain facies were well developed and the river - mouth bars were not developed
  受沉积基底地形的严格控制，发育于浅水台地背景上的延长组长7 ?长6油层组表现出典型的浅水三角洲沉积特征，具有发育的三角洲平原沉积，而前缘河口坝不发育，剖面上难以形成完整的进积序列。
• The most favorable reservoirs of study formatioms in study area are delta river mouth bar sand body and sublacustrine fan sand body . the sublacustrine fan sand body region developed in each sand group and the river mouth bar sand body region developed in gao 5 sand - group are the most favorable regions of developing lithologic traps
  研究区研究层段的最有利储层是三角洲河口坝砂体和湖底扇砂体，各砂组发育的湖底扇砂体区和高5砂组发育的河口坝砂体发育区是形成岩性圈闭最有利的场所。
• According to the abundance well logging , mud logging and core analysis data , gaotaizi reservoir has been classified into four sand group with the principle of cycle comparison and classified control . based on the detailed study of lithologic character , sedimentary structure , paleontologic fossils , depositional sequence , rock association and logging data , the microfacies of the studied area are divided into such seven types : subaqueous distributary channel microfacies ; river mouth bar microfacies ; subaqueous interdistributary channel microfacies ; subaqueous crevasse channel microfacies ; subaqueous natural barrier microfacies ; distal bar microfacies ; delta front sheet sand microfacies . the characteristic of each sedimentary microfacies are described detailedly
  通过研究大量测井、录井资料和岩芯资料，依据“旋回对比，分级控制”的原则，把研究区高台子油层划分为g 、 g 、 g 、 g四个砂层组。通过对研究区岩性、沉积构造、古生物、沉积序列、岩石组合及测井曲线特征进行研究的基础上，认为研究区高台子油层属于三角洲前缘亚相沉积，并将研究区沉积微相划分为：水下分流河道、河口坝、水下分流河道间、水下决口扇、水下天然堤、远砂坝、席状砂等七种微相类型。
• Using sedimentary facies analytical and formation inverse technique , the depositional characteristics and distribution of dujiatai formation of this area were described , disclosing that delta front facies and prodelta facies were mainly developed in dujiatai formation . material source are mainly from southern and northeast of the working area . sand types are mainly of delta front subwater distributaries channel sand body , river mouth bar and sheet sand body with large degree of planar variation
  2 .采用沉积相分析及储层反演预测技术，对新齐14井区杜家台油层储层沉积特征及展布特征进行了详细描述，揭示出本区主要目的层杜家台油层属t -扇二角洲沉积，发育扇三角洲前缘亚相及前扇三角洲亚相，物源主要来自于工区南部及东北部，发育的砂体类型土要为扇三角洲前缘水下分流河道砂体、河口坝砂体及席状砂砂体。