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tidal flat中文是什么意思

  • 潮成平地
  • 潮漫滩
  • 潮坪
  • 潮平
  • 潮埔,海埔地
  • 潮滩
  • 潮汐平地
  • 潮汐平原
  • 潮汐滩地
  • 滩涂(海涂)

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  • 例句与用法
  • The sediment of tidal flat affect tidal creek greatly too , especially affect the development of curve current of tidal creek . on the upper tidal flat , the clay is abundance , and the sediment is much more viscous , so the curve current develops well
    滩面沉积物的组成对潮沟的发育也有较大的影响,尤其是潮沟曲流的发育,愈向潮滩的上部,粘土的含量愈多,沉积物的粘结作用也越强,潮沟越易发育曲流。
  • ( 4 ) lt is eh that impact on the vertical distribution of heavy metal over tidal flat . at boundary of redox layer , there is the biggest enrichment of heavy metals . but the characteristic of distribution may be modified by plant activities in the tidal flat
    在高潮滩出现明显的富集,一般比中、低潮滩高出20 70 ,而中、低潮滩各元素的含量比较接近,不存在明显的差异,水动力作用是影响沉积物中重金属元素垂岸分布的主要因素。
  • Water surfaces and tidal flats used by units under ownership by the whole people , water surfaces and tidal flats owned by collectives , and those owned by the whole people but used by units under collective ownership may all be contracted to collectives or individuals to develop aquaculture
    全民所有制单位使用的水面、滩涂,集体所有的水面、滩涂和集体所有制单位使用的全民所有的水面、滩涂,可以由集体或者个人承包,从事养殖生产。
  • According to lithology , color , size of grain , sedimentary structure , and fossil types , the matuo formation vertical lithofacies are grouped into four types , represented tidal flat circumstance dominated by tide and shoreface circumstance dominated by wave , respectively
    根据岩性、颜色、颗粒粒径、沉积构造以及所含有化石类型,可以将雁石坪地区玛托组划分为4个岩性组合,它们分别代表以潮汐作用为主的潮坪?海湾环境和以波浪作用为主的滨面环境。
  • Sedimentary environment in benxi stage from east to west were respectively shallow - sea muddied continental shelf , barrier island , lagoon and tidal flat . most area in taiyuan stage was distributed by shallow - sea continental shelf , but the northern and southeastern part were scattered by clastic tidal flat and carbonate tidal flat . sedimentary environment in shanxi stage , in the middle and late shihezi stage was deltas and lake
    马5晚期研究区发育蒸发台地相和局限台地相;本溪期自东而西发育浅海泥质陆棚、障壁岛、泻湖及潮坪相;太原期大部分地区发育浅海陆棚沉积,北部和西南部则发育碎屑岩潮坪和碳酸盐潮坪沉积;山西期和石盒子中晚期为三角洲和湖泊沉积环境;石盒子早期广泛发育辫状河三角洲和湖泊沉积。
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