新漸成說 的英文怎麼說

中文拼音 [xīnjiānchéngshuō]
新漸成說 英文
neo-epigenesis
  • : 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 (...
  • : 漸副詞(逐步; 漸漸) gradually; by degrees
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  • : 說動詞(說服別人聽從自己的意見) try to persuade
  1. After implanted in host bone, bioceramics not only can play the role of bracket for bone growing but also can degrade and afford osteoblasts enough calcium and phosphate ions. so it will induce the new bone growing, participate in the vital process of host bone, and finally integrated with the host bone and become a portion of the organic new bone

    生骨組織出現在材料內部,明生物陶瓷植入宿主骨后,不僅本身能作為骨生長的支架引導骨生長,而且能逐被降解、吸收,參與宿主骨的生長,並最終與宿主骨融為一體,為有生命的生骨組織。
  2. He said, " we expect the health cost to continue to grow, due to an increasing and aging population, advances in technology and rising public expectations

    :由於人口增長和老化、科技日月異及市民的要求日提升,我們預計,香港的醫療本將會不斷上漲。
  3. At a press conference held in shanghai on 21 march, michael von zitzewitz, chairman of the board of management of messe frankfurt gmbh, said, " with the founding of our new subsidiary in shanghai, we are taking account of the growing significance of china in terms of the international fair sector "

    我們在上海立子公司是看準了中國在國際展覽業上的地位日重要。法蘭克福展覽有限公司總裁薜弭劭先生於3月21日法蘭克福展覽有限公司,上海子公司立的訊息布會上
  4. The comparison of cenozoic basalts and their mantle xenoliths from both sides of the taihangshan gravity lineament reveals that : ( 1 ) cenozoic basalts from western and eastern north china display opposite temporal trends, suggesting lithospheric thinning in western north china during the cenozoic and lithospheric thickening in eastern north china ; ( 2 ) the lithospheric mantle in the west is mostly late - archean to proterozoic in age, whereas that in the east has a modern age with minor proterozoic age ; ( 3 ) the crust mantle transition in the west is considerably thicker than in the east, probably due to different extents of magmatic underplating

    摘要通過對比華北太行山重力梯度帶兩側生代玄武巖及其中幔源包體的分,發現: ( l )華北東、西部生代玄武巖具有相反的演化趨勢,生代以來西部巖石圈逐減薄,而東部巖石圈逐加厚; ( 2 )西部巖石圈地幔組相對復雜,年齡多為晚太古代元古代;而東部巖石圈地幔組相對單一,年齡多為現代值,少數為元古代; ( 3 )西部殼幔過渡帶較厚而東部較薄,反映兩地不同的巖漿底侵作用程度。
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