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delta system中文是什么意思

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用"delta system"造句"delta system"怎么读"delta system" in a sentence

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  • 三角接线制

例句与用法

  • This complex is located near the intersection of northeast-trending littoral marine bars and a southeast-trending delta system .
    该复合体位于北东走向的滨海沙坝与南东走向的三角洲体系交汇处附近。
  • Eustatic lake level and source change had resulted in intercalation development in braided delta system
    湖面的升降和物源的摆动使辫状三角洲沉积体系中发育夹层。
  • Distributary mouth - bar sandstones in the progradational delta system and distributary channel and transgressive sheet sandstones in lowsfand prograding complex are excellent reservoirs ,
    层序岩性油藏大面积分布,已形成凹陷内大面积含油的局面。
  • Because of yizheng orogeny in late cretaceous , braided delta system of anfeng was formed by rifling in subei basin and rising of sedimentary base level
    摘要受晚白垩世仪征运动的影响,苏北盆地拉张断陷,沉积基准面上升,从而形成了比较完整的安丰退积型辫状三角洲沉积体系。
  • By looking into the cores , analyzing of granularity and ichno - fossils , the paper has ascertained the basin as a normal fluvial delta deposital system , which amends the former view that believed the basin should be a fan - delta system
    通过本区大量的岩心观察、粒度分析、遗迹化石分析,修改了前人认定的其为扇三角洲沉积体系的观点,将其确定为正常的河流三角洲体系。
  • There are 5 depositional systems in the region . they are : panhe and jishan delta systems coming from chengning heave near the northwest border of the region , shuangfen delta located in southwest part of the region coming from luxi dome , qudi fan - delta located in the southeast of the studying area and the sub - fan near fault or fan - delta of the southern part of the region
    确定了沙三段沉积时期发育的五种沉积体系类型,即来自凹陷西北边界埕宁凸起的盘河三角洲体系和基山三角洲体系、来自鲁西隆起、分布在凹陷西南部的双丰三角洲体系、东南部的曲堤(扇)三角洲体系,南部的近岸水下扇/扇三角洲体系。
  • There are 5 depositional systems in the region . they are panne and jishan delta systems coming from chengning heave near the northwest border of the region , shuangfeng delta located in southwest part of the region coming from luxi dome , qudi fan - delta located in the southeast of the studying area and the sub - fan near fault or fan - delta of the southern part of the region . based on the study of sedimentary facies and depositional systems , 11 lithological traps are predicted
    在等时地层格架内对沙三段各中期基准面旋回内的沉积相和沉积体系进行了详细研究,确定了沙三段沉积时期发育的五种沉积体系类型,即来自凹陷西北边界埕宁凸起的盘河三角洲体系和基山三角洲体系、来自鲁西隆起、分布在凹陷西南部的双丰三角洲体系、东南部的曲堤(扇)三角洲体系,南部的近岸水下扇/扇三角洲体系。
  • According to the regional geology and the character of the lithofacies and well - logging facies , 4 kinds of sedimentary facies and 3 kinds of depositional system : marine system , delta system and fluvial system have been identified . the sedimentary facies of taiyuan formation is marine faceis , up to sanxi formation , the sedimentary facies is delta facies , the xiashihezi formation hel and he2 member are braided river facies , he3 member is meandering river facies . the mains types of sandstone of taiyuan formation are lithic quartzarenite and quartzarenite ; the mainly types of sandstone of sanxi formation and xiashihezi formation is litharenite
    通过对20余口井2000多米岩心的观察和对40几口井的测井数据解释、对比,在研究区目的层段识别出了12种基本岩相和9种测井相类型,在区域沉积背景和单井相划分的基础上,根据岩相和测井相组合特征,在太原组?下石盒子组划分出4种沉积相和若干沉积微相,并进一步划分为3类沉积体系:滨浅海沉积体系、三角洲沉积体系和河流沉积体系。
  • From csql to csq5 , the barrier system was the main system . from psql to psq5 , the carbonate ramp was the main system and from psq6 to psq8 the main system was fluvial and fluvial - delta system in brackish basin . from psq9 - psql2 , the main system turned to the fluvial - delta system
    晚石炭世csq1 ? csq5层序以碎屑海岸障壁?泻湖和碳酸盐缓坡沉积体系为主;早二叠世早期psq1 ? psq5层序以碳酸盐缓坡沉积体系为主,早二叠世晚期psq6 ? psq8层序以半咸水盆地河流、河流三角洲沉积体系为主;中二叠世psq9 ? psq12为陆相冲积扇、河流、湖泊三角洲沉积体系。
  • From sedimentology symbol such as rock assembled , sediment gradus , sandstone grading analysis , protogene sedimentary structure , ichnofossile and logging facies etc and palaeoenvironment background , it is confirmed that shen84 - an12block s34 segment is braid river delta system , not fan delta system ( abrupt slope ) . then it can be more partition as braid river delta plain sedimentary assembled , delta front sedimentary assembled and prodelta sedimentary assembled on core and log assembled . and delta plain sedimentary assembled can be identified four microfacies : braided distributary channel , crevasse splay , overbank deposits and interdistributary bay
    沉积微相研究是储层非均质性研究的基础,研究区有丰富的岩芯资料和测井资料,通过岩石组合、沉积韵律,砂岩粒度分析、沉积构造、古生物遗迹和测井相等沉积学标志,结合古环境背景,确定沈84 ?安12块s _ 3 ~ 4段为辫状河三角洲体系,而不是前人所认为的扇三角洲(陡坡型)体系,在岩芯和测井组合上可进一步划分为辫状河三角洲平原沉积组合、三角洲前缘沉积组合和前三角洲沉积组合,其中三角洲平原沉积组合又可识别出辫状分流河道、决口扇、分流河道边部和分流间湾四种微相类型;三角洲前缘沉积组合识别出水下分流河道、水下分流河道边部和分流河口坝三种微相。
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