早更新世 的英文怎麼說

中文拼音 [zǎogēngxīnshì]
早更新世 英文
eopleistocene
  • 早 : Ⅰ名詞1 （早晨） morning 2 （姓氏） a surname Ⅱ副詞（很久以前） long ago; as early as; for a long ...
  • 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. Early pleistocene chalicothere fossils from huangjiawan, zhen ' an, shaanxi, china

    記陜西鎮安早更新世的兩種爪獸化石
  2. 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。
  3. Touke stratum was laid down in the pliocene and early pleistocene epochs. it is some 1500 meters thick on average, and rich in fossils. the fossil beds of tsailiao creek in tsochen were made famous by the discovery there in 1971 of the skull of " tsochen man.

    也由於左鎮鄉的地質為上新世至更新世早期的頭?山層，平均厚度為一千五百公尺，此層中含有豐富的海相濱海相淡水相等各類化石群，隨著地殼隆起而露出成陸。
  4. 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。
  5. The challenge for educators is to restructure the curriculum to make maximum use of the new technologies so that students can learn better and prepare themselves for the information - rich world they now confront

    對教育工作者提出的要求，就是要調整學校的課程來最大限度地使用新的技術，以便學生能夠學得更好，並為他們現在所面臨的信息豐富的世界而早作準備。
  6. Preliminary results indicate that the tuozidong deposits possibly belong to the early pleistocene to early middle pleistocene that the upper tuozidong deposits containing mammal fossils were probably formed during warm climate

    初步研究表明駝子洞堆積可能是跨早更新世與中更新世早期的地層，其上部含哺乳動物化石的堆積可能反映了偏暖的氣候環境。
  7. Twelve deep and great faults are developed in daqing city and its adjacent areas, they include nenjiang fault, keshan - da ' an fault, fuyu - zhaodong fault and the second songhuajiang fault etc, and they have been active in different degree since early pleistocene

    大慶市及鄰區斷裂發育包括嫩江斷裂、克山-大安斷裂、扶余?肇東斷裂、第二松花江斷裂等12條深大斷裂，在早更新世以來均有不同程度的活動。
  8. For years, sheng meei machine mfg., co. has under chairman mr. pin lee competent leadership, excellent performance of everyone in sheng meei and reliable quality of these machines, sheng meei mfg., co. has now become one of the largest knitting machinery manufacturers in the world. the distinct machine quality and sophisticated function, advanced performance at highest reliability has won industrial confidence and popularity, and had also made sheng meei machine mfg., co, s name being announced fooicially as one of the top 500 enterprises in taiwan. zhang jia gang sheng meei machine co., ltd. is located in china main sweaters shopping center situated in a golden triangle of south jiang su province in miao qiao town. the factory is just twenty kilometers away from zhang jia gang harbor and shang hai porby east, and adjacent to nan tong harbor by north, a perfect location with convenient access to all inland transportation

    三十多年來，總公司秉執著永續經營的理念和宗旨，在不進步就是落伍的原則下，不斷地創新與超越，從早期製造銷售各式手搖編織機，至一連串自行開發出全新全自動多功能的電腦自動編織機及提花機，躍居為世界一流水準的電腦毛及編織機製造廠。多年來，在董事長李賓先生的領導下，全體同仁群策群力，本著誠信踏實創新突破之精神，努力經營，不但產品行銷國內各地，而且遍及亞洲美國中東中南美洲與非洲等國家和地區，深受客戶的肯定信賴與喜愛。今日的盛美公司，更是世界數一數二的手搖及全自動毛衣編織機製造廠，躍居世界領先地位。
  9. Early - pleistocene mammalian fauna of huangjiawan, zhen ' an, shaanxi, and its companioned plants

    陜西鎮安黃家灣早更新世哺乳動物群及其伴生植物
  10. Discovery and study of the early pleistocene river and lake facies stratum in bukedaban area of the western segment in the eastern kunlun mt

    東昆侖西段布喀達坂峰地區早更新世河湖相地層的發現及初步研究
  11. The present longmenshan foreland basin lies between the longmenshan thrust belt and the longquanshan fault. the dayi conglomerate at the bottom of the chengdu basin, although people of the past having studied a certain degree, hasn " t same sugest

    大邑礫巖的地質時限為上新世-早更新世，時代界定在4 . 6ma - 0 . 82ma之間，顯示該區第三紀與第四紀之間是連續沉積的，其間不存在構造事件。
  12. This process would accelerate as china s market became more open and transparent. another reason was the closer economic partnership arrangement between hong kong and the mainland cepa, covering trade in goods, trade in services and trade and investment facilitation and providing a new platform for companies to enter the mainland market earlier than china s wto timetable

    另一個原因是《更緊密經貿關系安排》涵蓋商品、服務交易、促進投資及貿易活動以及提供一個新的平臺，讓商營機構能早於中國所簽訂的世界貿易組織時間表，打進中國?場。
  13. This process would accelerate as china s market became more open and transparent. another reason was the closer economic partnership arrangement between hong kong and the mainland ( cepa ), covering trade in goods, trade in services and trade and investment facilitation and providing a new platform for companies to enter the mainland market earlier than china s wto timetable

    另一個原因是《更緊密經貿關系安排》涵蓋商品、服務交易、促進投資及貿易活動以及提供一個新的平臺，讓商營機構能早於中國所簽訂的世界貿易組織時間表，打進中國?場。
  14. 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。
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