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生物地层的英文

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"生物地层"怎么读用"生物地层"造句

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  • biostratum

例句与用法

  • Trilobites were rapidly evolving forms and are of widespread use in biostratigraphic studies .
    三叶虫是进化迅速的种型,并广泛用在生物地层学的研究上。
  • Pliocene micromammalian biostratigraphy of nihewan basin , with comments on the stratigraphic division
    泥河湾盆地上新世小哺乳动物生物地层学及相关问题讨论
  • From these characteristics of biostratigraphy , lithostratigraphy and chronostratigraphy , the oil shales in shuanghu area are similar to those in early toarcian europe
    生物地层、岩石地层、年代地层来看,双湖地区的油页岩与欧洲早toarcian期广泛分布的黑色页岩有很好的可对比性。
  • Biostratigraphic zonation and mark - fossil erection should be based on restoring evolutionary pedigrees or occurrence sequences , and the boundary should be confirmed at the horizon of their " first appearance "
    生物地层学研究一定要以恢复演化谱系或发生序列为基础,界线化石标志应该选在其“首现”层位。
  • Ch . 2 biostratigraphy features , distribution and assemblage of three group fossils from many of the 7 geological setions , including conodont , coral and foraminifera fossils , have been comprehensively discussed . and a series of fossil assemblages can be recognized
    生物地层研究综合各剖面上获得的古生物资料,按牙形刺、珊瑚和有孔虫化石等三大类论述了它们的特征、分布和组合特点,进而在鲁班石地区划分建立了牙形刺生物化石组合带。
  • The main fruits of study are as follows : ( 1 ) a complete stratigraphic framework of middle - upper jurassic series is set up through systematic stratigraphic study of middle - upper jurassic by the analysis of lithostratigraphy , biostratigraphy and chronostratigraphy on five groups of middle - upper jurassic series in the studied area
    主要成果表现在以下五个方面: ( 1 )通过对研究区中?上侏罗统五个组进行岩石地层、生物地层和年代地层分析,系统进行中?上侏罗统地层学研究,建立了研究区中?上侏罗统完整的地层格架。
  • To reconstruct the evolution and variability of the east asian monsoon during the late cenozoic on millennial , orbital and tectonic time scales . 3 . to identify and better understand the links between tectonic uplift , erosion and weathering hemipelagic deposition , and climate change , including the evolution of the asian monsoon and the neogene global cooling
    Odp184航次1999年2月至4月间在中国南海进行钻探取样,通过钻取半远洋沉积,以期说明南海的新生代历史,包括它的生物地层学、岩石地层学、年代学、古气候学和古海洋学;重建千年级的晚新生代东亚季风的发展和演化、轨道和构造时间尺度;识别和更好地理解构造抬升、侵蚀和风化、半远洋沉积和气候变化,包括亚洲季风和晚第三纪的全球变冷。
  • In this paper , the authors prove the sedimentary environment of every lithostratigraphic unit of devonian , and precisely divide the geomorphic units of petrologic paleogeography of that period , based on the multiple division and detailed study to the petrostratigraphy , biostrtigraphy and sequence stratigraphy of devonian in hubei and its adjacent provinces
    摘要通过对湖北及邻省泥盆纪岩石地层、生物地层与层序地层进行多重划分对比和详细研究,以大量实际资料确定该时期各岩石地层单位的沉积环境,准确划分出该时期岩相古地理地貌单元。
  • Their distribution of deposition control lithology subtle trap , die - out around paleo - uplift the distribution of subtle traps in the slope , subtle trap forms along faults and above and beneath unconformity boundary . through exploring and studying in huanghua depression many years , we gradually summarize a series of methods and technologies for subtle trap exploration , they are precise stratigraphy correlation on the basis of sequence stratigraphy , including micromarker correlation , element logging , high frequent cycle stratigraphy and precise sequence stratigraphy , besides conventional biography stratigraphy , logging correlation . through using facies analysis method , the type and distribution of reservoir are determined
    在黄骅坳陷通过多年的摸索和引用,逐渐形成了一套系统的隐蔽油气藏的研究方法和技术,它们是以层序地层学为代表的地层精细划分方法,用来解决地层划分及归属问题,除常规的生物地层学、岩电特征对比方法外,创新性的运用了包括微标志层划分方法、元素测井方法、高频旋回对比方法及精细层序地层划分方法等四种精细地层划分方法。
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