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世古的英文

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"世古"怎么读用"世古"造句

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  • seko

例句与用法

  • Preliminary studies on holocene climatic in fuping , shaanxi province
    陕西富平全新世古气候的初步研究
  • Continues the director s powerful account of ordinary cambodians , this time focusing on those who live among the ruins of angkor wat
    来到吴哥窟,见证《花样年华》的秘密、赞叹惊世古建筑群以后,你可发现叫卖纪念品的小孩没上学?
  • What is more importatnt : satisfying a thousand desires or conquering just one ? in the majestic setting of the himalayas , the brilliant young monk tash . .
    故事描述貌美聪慧的山城少女琶玛锺丽缇饰,偶遇僧人达世古桑饰,竟燃起他纯真而原始的欲念,她不惜
  • According to the characters of the palynoflora , the late triassic palaeoecological , palaeoclimatic and palaeogeographic characters as well as the sedimentary environments in the region were discussed
    根据孢粉植物群的特征探讨了该区晚三叠世古生态、古气候、古地理和沉积环境。
  • Paleontologists have uncovered a wealth of whale fossils spanning the eocene epoch , the time between 55 million and 34 million years ago when archaic whales , or archaeocetes , made their transition from land to sea
    古生物学家已经找到了丰富的始新世古鲸化石,也就是现生鲸豚的祖先;他们发现古鲸是在5500 ~ 3400万年前的始新世,从陆栖动物演变成海栖动物的。
  • The geological setting of chengjiang biota firstly , the pattern of chinese tectonic has been cited , which can help us to understand the place of china in the world clearly and easily . secondly , the lower cambrian of china and the early cambrian geomorph of eastern yunnan have been included
    澄江生物群的地质构造背景首先介绍了中国区域大地构造格局,其次是关于中国的寒武系和滇东地区早寒武世古地理概貌的论述,紧接着是澄江化石库的古地理概貌。
  • According to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field , including lithology , size distribution , sedimenta ry structure , geochemistry and paleontology etc . , the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt . it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal . the peat flat is the important paleoenviron ment for coal accumulation . the tidal channel destroys the coal bed . the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
    根据肥城煤田石炭系太原组的岩性、粒度分布、沉积构造、地球化学及古生物等沉积特征,将该区晚石炭世古地理划分为碳酸盐开阔台地和潮坪环境,认为太原组形成于潮汐作用为主的陆表海海岸,泥炭坪是成煤的重要古地理环境,潮渠对煤层有一定的破坏作用,地壳的脉动性振荡作用是控制沉积环境演化和聚煤作用的主要因素。
  • Abstract : according to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field , including lithology , size distribution , sedimenta ry structure , geochemistry and paleontology etc . , the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt . it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal . the peat flat is the important paleoenviron ment for coal accumulation . the tidal channel destroys the coal bed . the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
    文摘:根据肥城煤田石炭系太原组的岩性、粒度分布、沉积构造、地球化学及古生物等沉积特征,将该区晚石炭世古地理划分为碳酸盐开阔台地和潮坪环境,认为太原组形成于潮汐作用为主的陆表海海岸,泥炭坪是成煤的重要古地理环境,潮渠对煤层有一定的破坏作用,地壳的脉动性振荡作用是控制沉积环境演化和聚煤作用的主要因素。
  • The study results can be summerized as following aspects : ( 1 ) the basic settling curve of this basin was broken - line shape of seven sections in which upper jurassic , lower cretaceous , eocene , oligocene and neogene corresponded with the decline ones representing five episodic clear subsidences of this basin , late cretaceous to paleocene and early miocene corresponded with the rising ones reflecting the uplift and denudation of this basin . ( 2 ) the subsidence of this basin migrated from the east to the west , from mesozoic to cenozoic
    研究表明: ( 1 )北黄海盆地的基本沉降曲线型式为7段折线状,其中晚侏罗世、早白垩世、始新世、渐新世、新近纪为曲线下降段,代表盆地5幕较明显的沉降;晚白垩世古新世以及中新世早期为曲线上升段,反映盆地的抬升剥蚀。
  • The palaeogeographic research indicate that the palaeogeographic outline of the study area recorded the evolution from a sedimentary basin in which the shallow - water carbonate platform sediments and deep - water terrigenous clastic submarine fan developed from southeast to northwest and northeast during the late triassic through a submarine sheet - like model composed of deep - water sandy turbidite and fine - grained turbidite during the early jurassic to a terrigenous clastic barrier coast during the middle and late jurassic and finally to the coal - bearing delta sediments during the late cretaceous
    古地理分析表明,研究区晚三叠世古地理轮廓是一个从东南向西北和东北方向由浅水碳酸盐台地及深水陆层海底扇沉积共同发育的沉积盆地;早中侏罗世,演变成为一个由深水砂质浊积岩和细屑浊积岩组成的水下席状体沉积;进入中晚侏罗世,其古地理表现为一个陆屑浅海有障壁海岸;到了晚白垩世,研究区表现为以含煤沉积为特征的三角洲相沉积。
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