新沉積物 的英文怎麼說

中文拼音 [xīnchénjīwù]
新沉積物 英文
recent sediments
  • 新 : Ⅰ形容詞1 （剛出現的或剛經驗到的） new; fresh; novel; up to date 2 （沒有用過的） unused; new 3 （...
  • 沉 : Ⅰ動詞1 （沉沒; 墜落） sink 2 （沉下 多指抽象事物） keep down; lower 3 [方言] （停止） rest Ⅱ形容...
  • 積 : Ⅰ動詞（積累） amass; store up; accumulate Ⅱ形容詞（長時間積累下來的） long standing; long pending...
  • 物 : 名詞1 （東西） thing; matter; object 2 （指自己以外的人或與己相對的環境） other people; the outsi...
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. The principle of cyclic sedimentation applies to deposits dating from earliest paleozoic time to the holocene.

    旋迴沉積原理適用於始於最早的古生代迄至全新世的沉積物。
  2. New evidence from the sediments of huguangyan maar lake, southern china for the younger drays event

    河北平原沉積物中記錄的新仙女木事件
  3. Yet this succession was forced willy - nilly onto the glaciated parts of northern europe, where there are partial successions of true glacial ground moraines and interglacial deposits, with hopes of ultimately piecing them together to provide a complete pleistocene succession

    研究者們還將這一順序強行用於北歐的冰川地區? ?那裡只有局部地方存在著真正冰川底磧和間冰沉積物之間的交替排列? ?企圖最終拼湊起一個完整的更新世順序。
  4. It is thought that the holocene original sediments were the result of the aeolation in the area, but the stream action influence the formation of deuterogenic loess

    認為本地區全新世原始沉積物是風成的，但流水作用影響了次生黃土的形成。
  5. The time corresponding to the four parts along the section are as follows : the top lake - swamp sediments : holocene ; the uppart fine sand : later late pleistocene ; the middlepart sandy clay : middle - early late pleistocene ; the lowpart clayer silt : later - middle - pleistocene. the fossils and stone artifacts found in salawusu site should be formed during the last but one glacier, its age range is about 0. 13 - 0. 19 ma, and belongs to later middle - pleistocene

    分析q曲線與氧同位素曲線的一致性以及以上研究結果，包含薩拉烏蘇地層的這套沉積物的沉積時代為：頂部湖沼相沉積物：全新世；上部具交錯層理的細砂：晚更新世晚期；中部粉砂質粘土：晚更新世中期至早期；下部粘土質粉砂：中更新世晚期。
  6. At the end of late pleitocene, influenced by the climate of glacier period, the last great event of the region in the geological time was taken place so that the migration and extinction of organism species were resulted, loess accumulation was generally developed throughout the whole region, in the holocene, the most important environmental change was fluvial process, which was still influnced by two factors - neotectonics and palaeoclimatic changes

    更新世晚期末，受末次冰期氣侯的影響，本區發生了地史時期的最後一次大事件，造成了物種遷移和絕滅，全區廣泛發育黃土堆積。進入全新世，本區環境變化以河流作用最為顯著，沉積物主要分佈在各大水系的河谷中，構成一、二級階地和近代河床與河漫灘堆積。
  7. Secondly, granularity analysis of sediments of upper marine facies of holocene is done

    其次，對全新世海相層及其以上地層中的沉積物進行粒度分析，劃分垂向沉積序列。
  8. These greatly improve the quality of pge abundances in the earth ' s crust, crustal rocks and sediments published before 1980 ' s, and they are very important for theory geochemistry, exploration geochemistry and mine exploration of pges

    這種對地殼、巖石和沉積物中鉑族元素豐度值的新認識，對理論地球化學、勘查地球化學甚至鉑族元素礦產勘查工作都具有重要的意義。
  9. Io ' s surface is constantly being made and remade through the lava deposits streaming from its many active volcanoes

    木衛一的表面不斷的被其眾多的活火山湧出的熔巖沉積物重新塑造著。
  10. With the widespread and profound impacts of global change on the natural elements and progress, the society and economy, and even the human activities, the study of global change has become one of the most active frontiers in the current earth science research field. especially, climatic and environmental changes of holocene and human history is a very important time scale of the study of global change. however, the geographic surroundings and the natural environment of the southern margin of tarim basin, which lies in the hinterland of eurasia continent, are so special that it is difficult to obtain the proxies indicating its environmental evolution

    在多年來前人研究成果的基礎上，本文通過尼雅剖面年代解析度可達10a的沉積物質量磁化率、碳酸鹽碳同位素、粒度等氣候替代性指標及約特干剖面的地球化學元素、孢粉等氣候指標信息的結果分析，並結合達木溝、塔格勒等剖面的成果及相關資料，得出以下結論： （ 1 ） 、南疆塔里木盆地南緣中全新世6 . 7 3 . 0kab . p .以氣候溫暖偏乾的荒漠環境為總體特徵。
  11. And it is also possible to analyze the reservoir property in reservoir framework. taking the reservoir of zonation 6 - 10 in s32 of pucheng oil field in henan province as an example, we founded the detailed reservoir stratigraphic framework through base - level correlation. in the strata frame, sediment distribution and its development are discussed based on sediment volume partitioning and facies differentiation analysis

    依據基準面變化中的過程?沉積響應，分析沉積過程中沉積物體積分配及與其相伴生的相分異，進行等時地層對比，建立精細地層格架，預測儲層空間展布及其非均質性的思路為儲層精細描述提供了新的方向。
  12. Characteristics of the magnetic fabric of sediments in the northern margin of altun tagh mountain since the late cenozoic and its geological significance

    阿爾金山北麓晚新生代沉積物磁組構特徵及其地質意義
  13. Dredging operations will be carried out in the ponds to ensure that contaminated sediments are not inadvertently allowed into the new drainage channel

    池塘會進行挖泥作業，確保受污染的沉積物不會因疏忽而流入新的排水道。
  14. As there are less such materials in loess as fossil, plants, slag, etc, which could be used for dating, luminescence dating, especially optically stimulated luminescence dating, was extensively applied to aeolian deposits, for its dating materials were minerals, such as quartz and feldspar

    由於黃土中所含的化石、木質、炭屑等適于其它方法測年的物質很少，同時，全新世黃土受年輕有機碳和無機碳的影響較大，致使全新世黃土類沉積物的測年迄今仍缺少理想方法。
  15. Application of robust estimation methods to anomaly appraisal of stream sediment survey in xinhure area, inner mongolia

    穩健估計方法在內蒙古新忽熱地區水系沉積物測量異常評價中的應用
  16. The climate of this period is almost as warm and wet as the stage 5e of the last interglacial. the mean temperature is 2 - 4 c higher and the precipitation is much larger than that of the today, the holocene which we live in. while in the climatic records of deep ocean, antarctic and greenland ice - core, marine isotope stage ( mis ) 3 is a weakly warm period, though a little warmer than marine isotope stage ( mis ) 2 and marine isotope stage ( mis ) 4, evidently colder than the last interglacial and holocene favorable period

    末次冰期中期，即深海氧同位素第3階段的氣候在我國，尤其是青藏高原地區表現出明顯不同於深海沉積物和極地冰芯記錄的特徵：青藏高原古里雅冰芯的~ （ 18 ） o曲線表明3階段存在特強夏季風事件，其氣溫和降水接近於末次間冰期5e階段，超過全新世，其暖濕程度已經達到間冰期的程度；而深海氧同位素3階段在深海、南極、格陵蘭冰芯的氧同位素記錄中均為弱暖期，雖較2階段、 4階段溫暖，但顯著低於全新世大暖期和末次間冰期。
  17. Optical stimulated luminescence dating of late pleistocene terrace deposits in the eastern segment of the altyn tagh fault and its tectonic implication

    阿爾金斷裂帶東段晚更新世階地沉積物紅外釋光測年及其構造意義
  18. Abstract : the new approach, which is widely adopted by some count ries andregions to develop sediment quality criteria based on the biological ef fect database, is reviewed according to the newest information on developing sedi ment quality criteria in canada, florida ( usa ), australia, new zealand and hong kong special administrativ region. the new advances of this approach on development o f sediment quality criteria and application are also evaluated

    文摘:根據加拿大、美國佛羅里達、澳大利亞、紐西蘭、中國香港等國家和地區水體沉積物質量基準研究的最新資料，綜述了目前國際上廣泛採用的用於制定沉積物質量基準的新方法- -生物效應數據庫法，介紹了該方法制定基準研究和應用的新進展。
  19. In the sediment, bacteria belonging to the cfb ( cytophaga - flexibacter - bacterioides ) group and the - proteobacteria, - proteobacteria were the main groups. the 16s rdna diversity of 7th layer was different from that of other layers, including the analysis of rflp, gene type and the population of cfb group. and the population of - proteobacteria showed inverse ratio with that of cfb group

    基於以上的試驗，我們分析了企鵝糞便沉積物中微生物生態與環境變化和環境污染的關系並提出了沉積物中出現的異常在環境和氣候方面可能的解釋，初步建立了以分析企鵝糞便沉積物中微生物多樣性為手段的新的考察南極氣候變遷和環境污染的思路。
  20. Make a comprehensive view of all study results about the flood channel, a model of formation and evolution of the flood channels was proposed. according to this model, not all flood channels formed by ebb channels divided by sand spit develop toward death, some of them may be keeping the current situation or transform to the reserve channel with the change of runoff and sediment concentration from upper reach

    用gis方法計算1861 - 2002年新橋水道區域的沖淤變化，可定量表達漲潮槽在不同時間尺度形成演化規律，結合漲潮槽巖芯沉積物垂向的沉積特性變化，可闡明漲潮槽的形成機理與演化過程，並提出不同種類型漲潮槽的形成演化模式。
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