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pliocene epoch中文是什么意思

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用"pliocene epoch"造句"pliocene epoch"怎么读"pliocene epoch" in a sentence

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  • 上新世

例句与用法

  • In the pliocene epoch , 5 . 3 million years ago , the primates continued to diversify
    在上新纪世纪, 5 . 3百万年前,大主教继续多样化。
  • They are all called yangping period denudation surface and were formed in the miocene epoch and the pliocene epoch
    鲁中南山地东部山顶部位的熔岩被分布面也相当于仰平期剥夷面。
  • Comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period , expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch , warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment
    通过对云南景谷盆地及陇川盆地新生代生物群特征的对比,探讨了新生代两大盆地环境演变:早中新世到上新世为湖盆发展期湖盆扩大萎缩期,气候为早期的千燥中新世早期的温暖湿润中新世中晚期的寒冷阴湿上新世的干燥,而中新世中晚期湖盆的扩大形成的半深湖深湖环境为油气的形成提供了有利条件。
  • Abstract : comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period , expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch , warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment
    文摘:通过对云南景谷盆地及陇川盆地新生代生物群特征的对比,探讨了新生代两大盆地环境演变:早中新世到上新世为湖盆发展期湖盆扩大萎缩期,气候为早期的千燥中新世早期的温暖湿润中新世中晚期的寒冷阴湿上新世的干燥,而中新世中晚期湖盆的扩大形成的半深湖深湖环境为油气的形成提供了有利条件。
  • The volcanic rock age and the age of the qiangtang formation determined the wudaoliang group between 20 - 5ma , discovering a flood of spore and pollen with ostracods fossils ( regard eucypris as principle ) , which are miocene epoches typical numerator , therefore wudaoliang group accumulate in miocene epoch is doubtless ; 9 - 2ma are the age of the suonahu formation based on the data of the esr , which were characteristic of later period in miocene epoch - pliocene epoch , spore and pollen with fossil all were miocene epoch period
    由火山岩和覆于其上的羌塘组的年龄限定五道梁群的沉积时间为20 - 5ma ,五道梁群中发现大量的孢粉和介形虫化石(以eucypris为主) ,分析认为它们都是中新世时期的典型分子,因此五道梁群的沉积时间为中新世是无疑的;唢呐湖组的esr测年数据范围为9 - 2ma ,代表中新世晚期?上新世时期,孢粉和化石都具有中新世时期的特征。
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