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lacustrine basin中文是什么意思

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用"lacustrine basin"造句"lacustrine basin"怎么读"lacustrine basin" in a sentence

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  • 湖成盆地

例句与用法

  • Sequence stratigraphic framework and the distribution model of stratigraphic traps in songliao deep water lacustrine basin
    松辽拗陷深水湖盆层序地层格架及地层圈闭分布模式
  • The basin tectonic model : it is intermont basin during late jurassic to early cretaceous , developed into faulted - lacustrine basin in eogene , and evolved into depression in neogene and quaternary
    “盆地”构造发育模式为:从晚侏罗世到白垩纪末期发育的山间“盆地”开始、发展到早第三纪断陷湖盆的发育、再演化为晚第三纪及第四纪地陷发育阶段。
  • Apart from in lacustrine basins in eastern china , sequence stratigraphic geochemistry is of especially important significance in source rock evaluation in some basins of western china , where only a few wells were drilled , and insufficient source rock cores are available
    层序地层地球化学研究不仅对中国东部老油田隐蔽油气藏的勘探工作具有重要的意义,对勘探程度不低、钻井少、源岩取心少的西部含油气盆地中的烃源岩评价工作更为有效。
  • Erlian basin is a rift lacustrine basin developed on the hercynian geosyncline folded base in early cretaceous , is featured by simple sedimentary feature , depositional cycle , small lacustrine transgressive , dry climate , salinization lacustrine water and multi - and - near sources
    摘要二连盆地是在海西期地槽褶皱基底上发育起来的早白垩世断陷湖泊群,具有湖盆湖浸规模较小、气候条件干燥、湖水咸化、沉积旋回单一,多物源、近物源和粗碎屑等沉积特征,以及发育岩性地层油气藏为主的油气分布特点。
  • Terrestrial sediments consist mainly of fluvial and lacustrine facies have the following characteristics : lacustrine basins have undergone a long continuous and fast subsidence and contain many terrestrial source rock sequences ; sedimentary facies of terrestrial basins are deposited in a ring formation . the best source beds are the continental source beds which contain dark shale
    陆相沉积以河流湖泊相为主,其基本特征有:长期快速沉降的湖相沉积盆地是陆相生油的发育区;陆相湖盆的沉积相带大都是环状分布,暗色泥岩是最佳生油层。
  • Linnan sub - depression which is mesozoic and cenozoic faulted lacustrine basin is located in the southwestern part of huimin sag , depression of jiyang . it is dominated by lacustrine - fill sub - depression . based on well logs , three - dimension seismic profiles , cores and other basic data , 10 horizons including 6 turnaround surfaces and 4 maximum flooding surfaces are defined from es3 to the lower part of es2 formation , and 1 long - term and 5 intermediate - term base - level cycles which are named from c5 to c1 could be identified , and then the chronostratigraphic framework of the sub - depression is built
    本文以岩心、钻井、测井、地震资料为基础,在下第三系沙三段沙二下的一个长期基准面旋回(二级层序)内部识别出10个有时间地层对比意义的界面,包括6个基准面下降到上升的转换面(层序界面) , 4个基准面上升到下降的转换面(湖泛面) ,划分出c1 - c5五个中期基准面旋回,建立了等时地层格架地层格架。
  • After have systematically studied sequence stratigraphy of chagan depression , a analysis method of high precision sequence stratigraphic framework in fault - depressed lacustrine basin . the core of the establishing framework is exploration - significant identify of sequence , division of 2 , 3 , 4 , 5 grades sequence and analysis of base - level based on lithologic log or well - logging , high - resolution seismic inversion constrained to well data . then using the results of 2d seismic data , and interpret sequence to enhance the precision of interpretation
    断陷盆地高精度层序地层格架建立的核心是用钻/测井和井约束条件下的高分辨率储层横向预测剖面等高分辨率资料进行具有勘探意义的二、三、四和五级层序的界面识别、层序划分和基准面变化分析,在此基础上标定常规地震剖面,进行区域层序地层分析,达到提高层序地层解释精度的目的。
  • In the condensed sections analysis , the concept of water - bearing lacustrine basin condensed sections and non - water - bearing basin condensed sections are firstly put forward , and have been described their features of lithology , mineral and geophysics , and have been predicted their distribution . meantime , this paper has studied the geochemical characters of source rocks , and contrast betwee
    同时,对有水湖泊密集段进行了烃源岩地球化学特征和烃源对比研究,确立了凹陷的含油气系统;对无水盆地密集段进行了盖层封闭能力的研究,确定了含油气系统的区域性盖层及顶部范围。
  • From studies of these characteristics of structures , palaeontology , drilling , well logging , seismic profile , salt chemistry and lacustrine sedimentary system , it is recognized that the new characteristics occur in of section pukou and in huaiyiri sag , and the huge thickness of salt rocks is formed by the crust salt materials upwelling along deep fracture in the form of hot bittern and entering lacustrine basin in this area
    通过该区构造、古生物、钻井、测井、地震、盐岩化学及湖盆内沉积体系等特征的研究,认为淮阴凹陷浦口组二段和三段的沉积构造有其特殊性,巨厚的盐岩层是壳深部盐类物质沿深大断裂上涌以热卤水形式进入湖盆的结果。
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