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带展的英文

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"带展"怎么读用"带展"造句

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  • bandspread

例句与用法

  • The distributing and promising prospects are different among them . 4 . the series of j ~ k , t3x2 and t3x4 belong to independent water bearing systems
    三个系统的平面分布、有利区带展布和成藏主控因素具显著差异。
  • Research shows that the production problem is related to serious reservoir heterogenity , which is dominated by the distribution of depositional facies
    研究认为该生产问题与储层内严重的非均质性有关,而储层的非均质性则明显受沉积相带展布规律的控制。
  • The distribution of depositional facies in bonan sag is very complex , which include five depositional systems , such as salt lake of deep water , transgressive fan delta , proximal turbidite fan , slump turbidite fan , distal turbidite fan
    洼陷内的沉积相带展布比较复杂,发育有深水盐湖、水进型扇三角洲、近岸浊积扇、滑塌浊积扇及带供给水道的远岸浊积扇等5种沉积体系。
  • ( 3 ) on the basis of study of sedimentary thickness change of each formation , analysis of provenance a nd p aleo - current d irection , s tudy o f d istribution o f s edimentary facies b elt a nd analysis of vertical phase sequence , lithofacies and paleogeography are analyzed and the sedimentary history of five stages of middle - upper jurassic series is renewed in the studied area
    ( 3 )在中?上侏罗统各组沉积厚度变化研究、物源区分析、古流向分析、沉积相带展布研究和垂直相序分析基础上,进行了岩相古地理分析并恢复了研究区中?晚侏罗世五个阶段的沉积历史。
  • During the early stage of middle permian , the studied area is dominant , from north to south , of alluvial fans , braided stream , braided delta plain , braided delta front and littoral deposits , while the extension of sedimentary facies belts in the middle and the late stage of middle permian is as the same as that of shanxi stage
    中二叠世早期,研究区由北向南依次为冲积扇、辫状河、辫状河三角洲平原、辫状河三角洲前缘和滨浅湖所占据。中二叠世中晚期,沉积相带展布顺序与山西期相同。
  • Based on the variation of light / heavy mineral components of sedimentary rocks , the typomorphic characteristics of various debris , the cathodoluminescence color of quartzes , the direction of paleocurrent and the extension of sedimentary facies , two source direction of the studied area in carboniferous and permian can be recognized , one is in bayanwusu , wulan ' ge ' er and hetaoyinshan area north of hangjinqi in the north margin of ordos , another is alashan area in the northwest margin of ordos
    在深入研究本区沉积岩轻、重矿物组分的变化、各种岩屑的标型特征、石英阴极发光颜色、古水流方向及沉积相带展布等基础上,认为研究区石炭?二叠纪的物源方向主要有两个,分别为:北缘杭锦旗以北的巴彦乌苏、乌兰格尔及河套阴山地区;以及研究区西北缘的阿拉善地区。
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