晚更新世 的英文怎麼說

中文拼音 [wǎngēngxīnshì]
晚更新世 英文
epipleistocene
  • 晚 : 名詞1 （晚上） evening; night 2 （姓氏） a surname Ⅱ形容詞1 （時間靠後的; 遲） far on in time; la...
  • 更 : 更副詞1. （更加） more; still more; even more 2. （再,又） further; still further; furthermore
  • 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 （...
  • 更新 : renew; replace; renovate; update; renewal; angenesis; restoration; regeneration; kainogenesis; tu...
  1. Environmental changes since late - pleistocene in north - bank of yangtze river, nanjing

    南京江北地區晚更新世以來環境演變研究
  2. The carbonate content varied from 0 to 34. 55 % in the column of drilling core ey02 - 2, the higher carbonate content related to materials of modern and old yellow river in postglacial period, while the peak carbonate content related to the shell fragment in the sediment, the dissolved cycle appeared to be the carbonate dissolved cycle of the atlantic mode

    Ey02 - 2孔柱樣碳酸鹽含量在0 - 34 . 55之間變化，呈現大西洋型caco _ 3溶解旋迴，冰後期以來碳酸鹽高含量與高碳酸鹽的現代黃河和廢黃河物質有關，而中晚更新世碳酸鹽極高含量與貝殼含量有關。
  3. The radiocarbon ages of charcoal and their implication derived from ciergou site along the haiyuan strike - slip fault

    永定河上游晚更新世晚期以來的堆積階地年代測定
  4. There were no coastal sand bar formation process for generating the qilihai lagoon, and its predecessor is a deflation low - lying land formed during the last stage of late pleistocene, so the qilihai lagoon is not a lagoon scientifically

    七裏海也不是科學意義上的?湖，它沒有形成海岸沙壩這一?湖形成的過程，其前身是晚更新世末期由風暴活動形成的風蝕窪地。
  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. The longdong river capture between yufu river and daxin river in jinan city, took place in the early quaternary, when the denudation surface of yangping period has already formed and the quaternary tectonic upheaval began to start. the yiyuan river capture between yihe raver and dawen river, was formed in holocene

    濟南龍洞河流襲奪是仰平期剝夷面形成后，魯中南山地第四紀構造抬升初期發生的襲奪現象；沂源河流襲奪則是在晚更新世晚期至全新世發生的襲奪現象。
  7. There were two conventional 14c ages, 9965 + 110 years on charcoal grains from the upper strata and 14550 + 450 years on fossil bones from the lower part. thus zhangkou cave was considered being late pleistocene to early holocene in time

    已測定上部地層炭屑和下部地層骨化石的常規~ （ 14 ） c年齡分別為9965 110和14550 450年，發掘者據此認為該地點的年代為晚更新世末至全新世早期。
  8. There were three times of sea - level fluctuation corresponding to the paleo - climate evolution, which had formed the sediments of alternative sea and river facies

    晚更新世以來的三次海平面升降變化造成了濰河下游地區海陸沉積環境交替，形成了巨厚的海陸交互相沉積層。
  9. As one of the typical environmental disasters at south strand plain in laizhou bay, occurrence, development and variation of salt - water intrusion have close relationship with paleo - environmental evolution since late pleistocene, and with modern environmental change and human activities

    摘要通過對萊州灣南岸鹹水入侵較嚴重地濰河下游地區晚更新世以來沉積特徵及現代自然環境條件變化的分析，探討了沉積相對鹹水入侵產生及空間范圍特徵的環境機理。
  10. Field investigation reveals that the latest time when yumen fault, western part o f qilian mountains was active is the end of the late pleistocene, and that the fa ult is coincident with other faults around west jiuquan basin. it is also found t hat yumen fault had not simply restricted to dip - slip motion ， strike - slip moti on is indicated. the results suggest that west jiuquan basin block might have rot ated clockwise

    新的證據顯示，位於祁連山西段酒西盆地南部的玉門斷裂的最新活動時代為晚更新世末，併兼有一定的走滑分量這一結果表明，酒西盆地塊體周邊斷裂的活動具有同時性的特點，酒西盆地塊體可能發生過順時針旋轉
  11. The eastern yantai - weihai segment is a mid pleistocene segment on which no late pleistocene offset has been found

    東段煙臺威海段為中更新世活動段，沒有發現晚更新世地層錯斷現象。
  12. Formed. the average crust up rate in this area from

    晚更新世以來這一地區的地殼平均上升速率為0 . 200 . 28mm a 。
  13. Preliminary study on late pleistocene phreato - magmatic eruptions in northern hainan island

    瓊北地區晚更新世射氣巖漿噴發初步研究
  14. The discovery and its significance of late quaternary involution in the area of lower reach of qingshuihe river, ningxia, china

    寧夏清水河下游晚更新世冰卷泥的發現及意義
  15. 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
  16. The same grade terrace height beside the river is surveyed at almost the same level, proved that the hidden fault under the river never moved after

    經測量河流兩側相對應的同級階地面處在相同的高度上，證明自晚更新世大凌河三級階地形成以來位於大凌河床底部的隱伏斷裂沒有過活動。
  17. In the recent years the study on the loess - palaeosol sequence has obtained many achievements that have attracted the attention of the world, but it mainly relies on the indirect physical and chemical proxies

    近年來在探索東亞更新世尤其是晚更新世的環境演化規律方面取得了令世界矚目的成果，但其研究多採用間接理化替代性指標。
  18. We have carried out 230th / 234u dating on several intercalated calcite samples. the results show that the capping flowstone layer and the second one are holocene in time. the fourth flowstone layer is of an age of 55 ka, and the fifth one 110 ka

    新生碳酸鹽鈾系法測年顯示，張口洞堆積所代表的時間跨度比原認為的長得多，這一結果支持我國中、晚更新世人類遺址原有年代框架被總體壓縮的觀點。
  19. The analysis of grain size of later pleistocene loess covering on the northern slop of tian shan mountains and ili basin shows that the tian shan loess is composed mainly of silt, accounting for 60 - 70 %, and some clay, accounting for 15 - 20 %

    摘要天山北坡和伊犁盆地晚更新世典型黃土剖面粒度分析表明，天山黃土以粉砂為主，佔60 - 70 %左右，粘粒含量一般在15 - 20 %之間。
  20. Because of those, the paper systems analysis the complicated geological environment, the character of rock mass ' s stress field and the stability of landslide on the right bank, in addition, the paper also deeply studied the geological engineering problem after the dam was builded in order to provide science datum for engineering decision, and elicited several conclusion : ( 1 ) the character of rock mass ' s stress - strain and new structure stress fieldrfrom the middle of q3 to today, the direction of the maximal principal stress has already changed to the sn, the stress - strain action and three direction of stress have been changed from " potential positive break " to " potential slide "

    同時通過以上的分析研究本文得出了以下主要的結論與認識： （ 1 ）最新構造應力場與地殼巖體應力?形變作用的現今特徵：自晚更新世（ q _ 3 ）中期以來，區域應力場的最大主應力（ _ 1 ）作用方向轉為近南北向（ n10 w ）作用並一直持續至今，地殼巖體的三向應力狀態及應力?形變作用經歷了由早期的「潛在正斷型」轉變到近期的「潛在走滑型」兩個不同的發展階段。
分享友人
分享到 Line

分享到臉書