风成砂的英文

• airborne sand
• anemoarenyte
• anemosilicarenite
• blown or aeolian sands
• eolian ore sand
• wind-blown sand

• "风"英文翻译    wind
• "成"英文翻译    accomplish; succeed
• "砂"英文翻译    sand; grit
• "风成砂金矿" 英文翻译 :    eolian gold placer
• "风成砂矿" 英文翻译 :    eolian placer
• "风成砂岩" 英文翻译 :    aeolian sandstone; anemoarenyte
• "风成砂屑石灰岩" 英文翻译 :    eolian calcarenite
• "成砂" 英文翻译 :    blown sand
• "风成" 英文翻译 :    aeolian; aeolic; wind driven (ocean) circulation
• "合成砂" 英文翻译 :    synthetic sands
• "河成砂" 英文翻译 :    fluvial sand
• "半合成砂" 英文翻译 :    semi synthetic sand; semi-synthetic sand
• "冰成砂平原" 英文翻译 :    glacial sand plain
• "海成砂矿" 英文翻译 :    marine placer
• "河成砂矿" 英文翻译 :    stream placer
• "河成砂纹" 英文翻译 :    alluvial sand ripples
• "湖成砂矿" 英文翻译 :    lake placer; lakebed placer
• "混成砂铸型" 英文翻译 :    compo-mold
• "混成砂铸造" 英文翻译 :    compo-casting
• "风成尘" 英文翻译 :    eolian dust; windblown dust
• "风成的" 英文翻译 :    aeolic (aeolian); wind-induced; windborne
• "风成浪" 英文翻译 :    wind wave; wind-generated waves; wind-induced wave
• "风成流" 英文翻译 :    wind-driven current
• "风成丘" 英文翻译 :    eoliandune
• "风成沙" 英文翻译 :    aeolian sand; eolian sand

• As regards sk ( bias angle ) and kg ( kurtosis ) values , the fluvio - lacustrine facies or palaeosols increases considerably compared with the aeolian sands . the former displays positive bias and the latter often approximately symmetrical distribution with only a minority negative bias
  就sk和kg变化而言，河湖相或古土壤值较之风成砂明显增高，前者呈正偏，后者常常表现近对称分布，仅少数呈负偏。
• Mz , a , sk , kg and sc / d ( ratio of the sum of silt and clay to sand ) of fluvio - lacustrine , palaeosols and aeolian sands constitute an interlocking , multi - fluctuation process curve with peak and valle y values : the < & value of mz , o and sk values often increase accordingly from aeolian sands to its overlying fluvio - lacustrine facies or / and palaesols , the kg value heightens , too , and the sc / d value also basically consists with its change steps
  河湖相和古土壤与风成砂的mz 、 、 sk 、 kg以及sc d (粉砂粘土之和与砂的比值)构成一峰谷交替、犬牙交错的锯齿状多波动过程线：常常是由风成砂至上覆河湖相或和古土壤， mz的值、 、 sk值相应增大， kg相应增高， sc d值亦与之变化步骤基本一致。
• The general characteristics of the grain - size distribution of different sedimentary facies , es pecially the variations of the parameters mz ( mean particle diameter ) and o ( standard deviation ) clearly show that the fluvio - lacustrine facies and palaeosols usually become finer in particles and worse in sorting than the aeolian sands
  该剖面不同沉积相粒度的一般分布特征尤其是粒度参数? mz 、的变化明显表现出，河湖相或古土壤通常要较风成砂颗粒细化，分选相对较差。
• This paper , based on the grain - size analysis and the comparative result of the mz - o scatter gram of ancient aeolian sands in milanggouwan section with the modern dunes in mu us desert , holds that fossil eolian dunes are a proxy of the dune activation , and be regarded as " desert process " , while the overlying fluvio - lacustrine and palaeosols on the dunes are regarded as inter - desert process
  文中根据粒度分析及古今砂丘的mz ?散点图比较结果，认为古代风成砂丘特别是古流动砂丘是砂丘活化的体现，视为“沙漠期” ，而砂丘上覆的河湖相沉积与古土壤发育则可视为“间沙漠期” 。
• Grain - size accumulation percentage of the aeolian sands in the past 150 ka in milanggouwan section is mainly characterized by the aeolian palaeo - mobile dune sands , which are composed of majority fine sands and minority very fine sands . there is n ' t almost any silt and clay . those of the fluvial facies , especially the lacustrine facies and palaeosols , are mainly composed of very fine sands and also contain some quantities of silt and clay
  米浪沟湾剖面150kabp以来风成砂的粒度累积百分含量以古流动砂丘砂物质为主，其中以细砂含量最高，极细砂为次，几乎不含粉砂与粘土；河流相、特别是湖沼相与古土壤以极细砂含量占优势，且具一定含量的粉砂和粘土。