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为志的英文

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"为志"怎么读用"为志"造句

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  • tameshi

例句与用法

  • These experiences , and the contacts that scholars make in the uk , form a basis for each scholars future development
    这些经验,以及他们在英国建立的联系,为志奋领学者将来的发展提供了良好的基础。
  • 1 . the chevening programme was established in 1983 as the foreign and commonwealth office scholarships and awards scheme and took its new name in 1994
    1 .作为英国外交部的奖学金,志奋领项目始于1983年并在1994年正式更名为志奋领奖学金。
  • With a little pressing , she is made to admit that she ' s practicing so that she can at least make shiki ' s lunch for the upcoming culture festival
    被逼问了几句后,她被迫承认正在练习中,这样她就起码可以在即将来临的文化祭中为志贵做午餐了。
  • Pop singers alex fong and stephy tang reunite in this unofficial sequel to their last romantic comedy hit marriage with a fool . bo tang is trying to help her childhood friends untangle their problems in love
    心软的家宝答应了为志荣保守秘密,她只将事情告诉了与二人毫不相干的室友阿蚊miki饰。
  • English language teaching contacts scheme for china list is a british countil china on - line discussion group for chinese english language teaching professionals with an interest in developing themselves and sharing views on elt
    “中国英语教学研讨接触计划”是为志在发展自我、交流英语教学的中国英语教学职业人员而设立的英中在线研讨团体。
  • World journal s mission is to serve all overseas chinese by helping immigrants bridge the gap to mainstream america , keep in touch with their homeland and local chinese community news and improve their quality of life
    世界日报以服务所有海外华人为志职,一方面协助新移民跨越鸿沟,逐步迈向主流社会,另一方面满足其精神需求,增进生活品质,维系中华情感。
  • 2 . tazhong ancient uplift originated from normal fault in paleozoic , hydrocarbon formed in ordovician period , structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period , and it provided geologic background for the deposit of silurian - devonian stratum . tazhong uplift formed at the end devonian , ancient reservoir was destroyed and asphaltum sandstone formed , structure deformation more destroyed ancient reservoir in early permian , after then the major of structure deformation is regulation
    塔中隆起源于早古生代拉张背景下的正断层,寒武-奥陶纪为其烃源岩形成的重要时期;早奥陶世末-晚奥陶世末的构造反转是塔中隆起的主要形成期,同时也为志留系形成地层及复合圈闭提供了古地理背景;志留?泥盆纪塔里木盆地南北缘均转为活动大陆边缘,形成了大量的断裂和不整合;泥盆纪末塔中鼻状隆起基本定型,古油藏遭受破坏,形成了沥青砂岩;早二叠世晚期的构造变形使古油藏遭受进一步的破坏;二叠纪后构造变动主要以调节为主。
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