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浅海沉积的英文

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"浅海沉积"怎么读用"浅海沉积"造句

英文翻译手机手机版

  • neritic deposit
  • neritic sediments
  • neriticsediments
  • shallow sea deposit
  • shallow-sea deposit
  • shallowseadeposit

例句与用法

  • The effects of sound field by sediment in shallow water
    关于浅海沉积层对声场影响的讨论
  • For estuary - shallow marine and estuary sand bars , became the sedimentary conditions are no longer favourable , no sand ridge sediments were formed
    对于河口湾浅海沉积和河口湾砂坝沉积而言,由于沉积条件不再有利,没有形成沙脊沉积。
  • According to the regional geology and the character of the lithofacies and well - logging facies , 4 kinds of sedimentary facies and 3 kinds of depositional system : marine system , delta system and fluvial system have been identified . the sedimentary facies of taiyuan formation is marine faceis , up to sanxi formation , the sedimentary facies is delta facies , the xiashihezi formation hel and he2 member are braided river facies , he3 member is meandering river facies . the mains types of sandstone of taiyuan formation are lithic quartzarenite and quartzarenite ; the mainly types of sandstone of sanxi formation and xiashihezi formation is litharenite
    通过对20余口井2000多米岩心的观察和对40几口井的测井数据解释、对比,在研究区目的层段识别出了12种基本岩相和9种测井相类型,在区域沉积背景和单井相划分的基础上,根据岩相和测井相组合特征,在太原组?下石盒子组划分出4种沉积相和若干沉积微相,并进一步划分为3类沉积体系:滨浅海沉积体系、三角洲沉积体系和河流沉积体系。
  • 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
    根据岩石学、沉积结构和沉积构造特征,本区下切河谷充填沉积物具有向上变细的沉积层序,可以划分为4个沉积相类型:河床滞留沉积物到部分曲流河沉积体系的边滩沉积、河漫滩河口湾沉积、河口湾浅海沉积和河口湾砂坝沉积。
  • Assemblage ) represented the coastal shallow - water environment ; factor 2 ( protelphidium tuberculatum assemblage ) represented the alongshore cold - water current area or cold shallow sea environment ; factor 3 ( elphidium magellanicum assemblage ) represented the sh allow sea ( < 20 - 30m depth ) deposit ; factor 4 ( ammonia ketienziensis assemblage ) represented the shallow - sea water more than 50m depth ; and factor 5 ( buccella frigida assemblage ) represented the colder - water sea environment ; and the distribution of factor load accorded with the character of benthic foraminifer community
    Q型因子分析揭示ey02 - 2孔5种有孔虫组合,分别对应滨岸盐沼环境、黄海沿岸流冷水分布区、高潮坪浅海沉积环境、水深大于50m的现代浅海环境及较冷的沉积环境。因子载荷的分布与有孔虫群落特征吻合较好。南黄海有孔虫含量? ?水深转换函数关系式有一定的局限性,并不能在南黄海陆架地区推广使用。
用"浅海沉积"造句  

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