interglacial 中文意思是什麼

interglacial 解釋
n. 名詞 ,adj. 形容詞 【地質學；地理學】間冰期（的）。

  1. This succession was based primarily on a series of deposits and events not directly related to glacial and interglacial periods, rather than on the more usual modern method of studying biological remains found in interglacial beds themselves interstratified within glacial deposits

    這一順序主要是根據與冰川期和間冰期沒什麼直接關系的一套沉積物或現象而排出的，現代更為通用的方法則是研究發現于間冰期河床的生物化石。
  2. 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。
  3. Abrupt changes in earth ' s climate system since last interglacial

    末次間冰期以來地球氣候系統的突變
  4. Sangamon interglacial stage

    桑洛蒙冰間期
  5. Changes in terrestrial carbon storage with global climate changes since the last interglacial

    生態系統的碳儲量與氣候變化
  6. We do not know whether we live in a postglacial period or an interglacial period

    我們不知道自己是生活在後冰川期還是生活于間冰期。
  7. Ice age when someone summed up the reason as the earth history to once had and interglacial stage

    有人把原因歸結為地球歷史上曾經有過的冰期和間冰期。
  8. The same thing happened 11, 000 years ago, just as the current interglacial period began

    1萬1000年前，也就是目前的間冰期剛開始的時候，也發生同樣的狀況。
  9. There is no conclusive evidence about the relative length, complexity, and temperatures of the various glacial and interglacial periods

    還無法確證不同冰川期與間冰期之間的相對長度、復雜性及溫度。
  10. In interglacial periods, such as at the present time, the global sea level rose to its present level and higher, and marine sediments were deposited

    幾次間冰期內（目前也正值間冰期） ，全球海平面升至目前或更高水平，並沉積了海洋沉澱物。
  11. Correlation of environmental and climatic change between qaidam basin gamma ray logging curve and guliya ice core 18o record since the last interglacial cycle

    柴達木盆地自然伽瑪曲線與古里雅冰芯記錄的末次間冰期以來氣候環境變化過程的對比
  12. During the current interglacial interval, co2 concentrations reached the expected peak around 10, 500 years ago and, just as anticipated, began a similar decline

    目前的間冰期，二氧化碳濃度在10500年前達預期的高峰，然後也如預期的開始下降。
  13. Current research projects deals with the influence of climate change and land use, the extent of the last interglacial and other glacier studies, basin analysis, vegetation changes etc

    當今的研究計劃處理氣候變化和土地使用的影響、最後的間冰期和其他冰河研究的范圍、盆地分析、植物變化等。
  14. Comparison of the characteristic parameters of immobile elements, such as ree, sc, th, ti etc and of the characteristics of sedimentology and mineralogy comes to a conclusion that the provenance of the sediment is different in the last glacial maximum and in the sub - interglacial stage, and they have the traits of mixed source. during the last glacial maximum the sediment in the outshelf of the southern east china sea was affected weakly by changjiang river and they are probably derived from the coast mountains of zhejiang - fujian province, which are near the southern east china sea

    通過對東海外陸架樣品的稀土元素和sc ， th ， ti等不活潑元素地球化學物源示蹤指標對比，再結合沉積學和礦物學特徵，判斷末次盛冰期與盛冰期以前的沉積物具有不同的物質來源，不同時期的沉積物都具有混合物源的性質，盛冰期東海南部外陸架沉積物受長江物源影響較小，可能來源於距東海南部較近的浙閩沿海山地。
  15. The holocene events, therefore, appear to be the most recent manifestation of a pervasive millennial - scale climate cycle operating independently of the glacial - interglacial climate state

    所以，全新世事件似乎是（距今）最近的千年氣候周期的傑作。這種常見周期（刪- -的運行）是獨立於冰期-間冰期交替氣候的
  16. Although a complex combination of all three orbital cycles controls co2 variations, the trends during previous interglacial intervals were all surprisingly similar to one another

    雖然二氧化碳的變化受到三種軌道周期的復雜組合所控制，但先前各個間冰期的趨勢都非常相似。
  17. 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。
  18. The results improve our understanding of the utility of tl as an indicator of sedimentary environment and provide insight into what types of ocean sediments are amenable for study. the comparison of the 18o with the tl cycles indicates that the tl dose display the expected coupling relation with interglacial and glacial climate cycles

    尤以位於東經90海嶺上的以遠洋沉積作用為主的md81349巖芯最為理想，陸源剝蝕產物在其沉積記錄中所佔比例較少，有孔蟲和超微化石為代表的遠洋成因的灰白色生物軟泥構成主要的沉積組分。
  19. In addition the average sedimentation rate was obviously higher in the interglacial period than in the glacial period in the drilling core ey02 - 1 in the north of mid - shelf

    而東海中陸架北部ey02 - 1孔間冰期時的平均沉積速率明顯高於冰期時的平均沉積速率。
  20. Over the past three million years, these regular changes in the amount of sunlight reaching the planet ' s surface have produced a long sequence of ice ages ( when great areas of northern hemisphere continents were covered with ice ) separated by short, warm interglacial periods

    過去300萬年間，陽光抵達地表的規律變化造就了一系列的冰期（北半球陸地大部份都由冰覆蓋） ，間隔著短暫、溫暖的間冰期。
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