陸架 的英文怎麼說

中文拼音 [liùjià]
陸架 英文
continental shelf
  • 陸 : 陸數詞（六的大寫） six （used for the numeral 六 on cheques, etc. to avoid mistakes or alterations）
  • 架 : Ⅰ名詞1 （用來放置東西或支撐物體等的東西; 架子） frame; rack; shelf; stand 2 （毆打; 爭吵） fight;...
  1. Pre - cenozoic groups in the shelf basin of the east china sea

    東海陸架盆地的前新生界
  2. The fit between the continental shelves is even better than that between the coastlines.

    大陸架之間的契合程度比海岸線之間的契合程度更甚。
  3. How do people define the continental shelf ?

    人們怎麼確定陸架的范圍的？
  4. The water above the continental shelf is moved by the tides and by estuarine currents.

    潮流和河口流使大陸架上的海水流動。
  5. The sea floor of this continental shelf usually undulates gently, rising occasionally to the surface in offshore banks or island.

    這個大陸架海底通常緩慢起伏，偶爾以岸外的砂洲和島嶼的形式露出水面。
  6. Outer continental shelf delimitation facing a challenge

    外大陸架劃界面臨挑戰
  7. Delimitating the chinese continental shelves - ways and issues

    中國周邊大陸架的劃界方法與問題
  8. At the end of the continental shelf

    位於大陸架的末端
  9. Spawning ground of nemipterus bathybius in northern continental shelf waters of south china sea

    南海北部陸架區海域深水金線魚的產卵場
  10. Briefly talking on jurisprudential basis of the rights and interests of continental shelf of the east china sea

    我國東海大陸架權益的法理基礎淺論
  11. Internal tides generated over some kinds of topographies ( such as continental slope and shelf, ridge topography ) are investigated by using of the transforms introduced in this dissertation

    利用提出的坐標變換研究了若干亞臨界地形上（如陸架陸坡地形、海山地形）內潮的產生。
  12. This continental slope usually starts at a place somewhere near the 100 - fatheom mark and in the course of a few hundred miles reaches the true ocean floor at 2, 500 - 3, 500 fathoms

    大陸架慢坡一般是從差不多100英尋水深的地方開始的，一直延伸到幾百英里遠深達2 ， 500至3 ， 500的地方，那裡才是真正的海底。
  13. A sets of transforms are introduced in this dissertation, by using of which some kinds of topographies, such as continental slope and ridge, can be converted into flat bottom. the processing simplifies the generation of internal tides and reflection of internal waves over those kinds of topographies

    針對海洋中的一些地形，如陸架陸坡地形、海山地形、海溝地形，提出了一組坐標變換，該變換可以將這些海底地形變換成平底，從而使得在這些特徵地形上內波的傳播和內潮的產生問題得到很大的簡化。
  14. Under the hydrodynamitic condition in the outshelf heavy minerals are enriched to a certain extent. they are of horablede - epidote assemblage and contain some authigene ( pyrite and glauconite ). the content of stable mineral is small and mineral maturity index ( trzg / hp ) is low

    在外陸架水動力的作用下，重礦物有一定富集，重礦物以角閃石?綠簾石礦物組合為特徵，含有一定量自生礦物（黃鐵礦和海綠石） ，穩定礦物少，礦物成熟度低。
  15. Benthic foraminifer fauna, ams14c dating and acoustic sub - bottom profile was analyzed in the core ey02 - 2 and ey02 - 1 drilled from the muddy deposit in the middle southern yellow sea and the mid - shelf of north east china sea. considering the results of core qc2 ? dz4 and the standard oxygen isotope curves, we discussed the late - quaterenary paleo - environment evolution, benthic foraminifer fauna, paleo - climate, the climate events and water mass in postglacial period, average sedimentation rates, paleo - water depth, origin of sediments, average sea level rise rate in the shelf of south yellow sea and east china sea. at last we discussed the condition of sea level rise in the east china, green house effect and the protection of coastal zone

    本文根據南黃海中部泥質區和東海中陸架的兩個鉆孔巖芯的古生物、 ams ~ （ 14 ） c測年、淺地層剖面等，參考qc _ 2 、 dz _ 4成果及標準氧同位素曲線探討了黃東海陸架晚第四紀古環境演化、底棲動物群特徵、古氣候、冰後期以來氣候事件、古水團、沉積速率、古水深、沉積物源、海平面平均上升率，討論目前中國東部海平面上升的狀況、溫室效應及海岸帶保護。
  16. 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種有孔蟲組合，分別對應濱岸鹽沼環境、黃海沿岸流冷水分佈區、高潮坪淺海沉積環境、水深大於50m的現代淺海環境及較冷的沉積環境。因子載荷的分佈與有孔蟲群落特徵吻合較好。南黃海有孔蟲含量? ?水深轉換函數關系式有一定的局限性，並不能在南黃海陸架地區推廣使用。
  17. Large modern-day aircraft utilizes either bicycle or tricycle landing gears.

    大型的現代飛機不是採用雙輪式著陸架，就是採用三輪式著陸架。
  18. ( iii ) by c - 14 dating, size and sediment indexes analysis, the malan loess is studied which is the main component of the second terrace in csmasp

    認為張夏黃土與青州黃土具有相似的成因和物源，但與洛川等地的典型黃土和萊州灣沿岸的陸架黃土有明顯差異。
  19. Results as following : in the east china sea and the yellow sea, zooplankton showed higher diversity in the low latitude and warm species occurred mainly in the south of 31 n, five communities were distinguished by twinspan method, based on data of species composition and environmental factors. they are : i ) yellow sea neritic community ( f ) with indicator species of labidocera euchaeta in autumn and centropages mcmurrichi in spring ; ii ) yellow sea central community ( hc ) with indicator species of themisto gracilipes, calanus sinicus and euphausia pacifica, the latter two species occurred only in autumn ; iii ) east china sea continental shelf mixed water community ( k ) with indicator species such as rhincalanus cornutus and pterosagitta draco which were confined in waters with high temperature and salinity, iv ) yellow sea and east china sea mixed water community ( he ) and v ) east china sea inshore mixed water community ( m )

    根據twinspan等多元分析結果，比較各組群的浮遊動物種類組成和環境特徵，可將東、黃海浮遊動物群落分為5個，黃海沿岸群落（ f ） ，指示種秋季為真刺唇角水蚤，春季為墨氏胸刺水蚤；黃海中部群落（ hc ） ，指示種以細長腳蟲戎為主，秋季還有中華哲水蚤和太平洋磷蝦；東海外陸架高溫高鹽群落（ k ） ，指示種為角錨哲水蚤、飛龍翼箭蟲等多種狹布型暖水種類；黃東海交匯區群落（ he ）和東海近岸混合群落（ m ） ，兩群落包含多種生態類型種類，其中溫帶近岸低鹽種在he中較多，廣布性暖水種在m群落中較多。
  20. Many research such as clay minerals, suspend in the sea, the grain size trend analysis of surface sediment, poc 6 cu and 8 c13 in bottom sediments etc. showed that : the yellow sea warm current divided the south yellow sea into two, the terrestrial material of modern sediment on the west shelf plain mainly came from the modem yellow river suspend carried by the alongshore current, and the sediment difference between the west and east side of yellow sea trough was represented by the sedimentation thickness in postglacial period, sedimentation stratum, and oxygen isotope record

    粘土礦物、碳酸鹽、粗碎屑、海域懸浮體、表層沉積物粒度趨勢分析、 poc c ~ （ 13 ）及底質沉積物的c ~ （ 13 ）等多方面研究表明：以黃海暖流為主導，南黃海堆積陸架平原西側現代沉積物陸源物質主要源於黃海沿岸流攜帶的現代黃河懸移物質，黃海槽東西兩側的沉積差異主要表現在冰消期以來沉積厚度、沉積層序、氧同位素記錄上。
分享友人
分享到 Line

分享到臉書