沉积相

chén jī xiàng
  • sedimentary facies
沉积相沉积相
沉积相[chén jī xiàng]
  1. 因此,利用微量元素锶的含量和Sr/Ca×1000比值可以判别沉积相。

    The content of the trace element Sr and the Sr / Ca × 1000 ratio can therefore be used to judge sedimentary facies .

  2. 首先利用沉积相分析和地震相分析技术,对SWD地区的砂体展布进行了描述;

    First , the sand-body distribution is described by the analysis of sedimentary facies and seismic facies .

  3. 本文在评述国内外有关碳酸盐相模式研究基础上提出,海洋碳酸盐沉积相模式研究已摆脱了60&70年代的静态的束缚而进入了一种动态研究阶段并强调碳酸盐缓坡(ramp)的重要性。

    The marine carbonate facies models have broken away from static models in the 1960 's & 1970 's and are coming into a dynamic ones , in which carbonate ramp plays an important role .

  4. 通过沉积相展布、岩性地层圈闭分布规律、主控因素和成藏规律分析,预测出Puffin组各小层利区带。

    Analyzed the distribution of sedimentary facies , distribution rule of lithologic-stratigraphic trap , main controlling factor and pooling pattern , predicted the probability area of each sublayer in Puffin formation .

  5. 以15cm为间距,系统采集了1674块样品,进行质量磁化率的测定与分析。结果表明:沉积物磁化率值的大小与沉积相,尤其是与沉积物的粒度相关。

    The results of the susceptibility measurement , by the sample intervals of 15cm , of the three typical profiles show that the value of sediment susceptibility is related to the sedimentary facies , especially the grain size of the sediments .

  6. 从岩相序列到米级旋回,从沉积相序列到三级层序,可以将研究区域的奥陶系划分为8个三级层序,即OS1至OS8。

    Form lith-facies succession to meter-scale cycle and from sedimentary-facies succession to third-order sequence , the Ordovician in studied area can devided into 8 third-order sequences , they are OS1 ~ OS8 , which can be grouped into two second-order sequence . Tongzi Fm .

  7. 华北地块中&上元古界上升流沉积相及其与油气的关系

    Neoproterozoic-mesoproterozoic upwelling facies and its relationship with hydrocarbon in North China

  8. 广西晚二叠世合山组沉积相分析

    Sedimentary facies analysis of Upper Permian Heshan formation , Guangxi Province

  9. 柴达木盆地西部地区古近纪与新近纪沉积相

    Sedimentary facies of the Paleogene and Neogene in western Qaidam Basin

  10. 油田沉积相模式识别的研究

    The Study of Pattern Recognition in the Deposition Facies of Petroleum

  11. 民和盆地中下侏罗统沉积相分析

    Analysis of sedimentary facies of Middle-Lower Jurassic system in Minghe Basin

  12. 四川盆地西部侏罗纪沉积相及油气分布

    The Jurassic sedimentary facies and oil-gas distribution in western Sichuan Basin

  13. 高密度流与湖南泥盆纪沉积相分异

    Sedimentary facies differentiation related to high-density flow during Devonian in Hunan

  14. 运用对应分析方法区划碳酸盐岩沉积相

    Use of correspondence analysis in dividing sedimentary facies of carbonate rocks

  15. 应用改进三角网方法绘制地质沉积相带图

    Improved Trigonometry Method and Its Application in Sedimentary Belt Mapping BELT ART

  16. 重点目标层段沉积相、沉积体系精细研究;

    Thorough studying in sediment faces and sediment system of emphasis sequence ;

  17. 下扬子盆地石炭系沉积相

    Sedimentary facies of Carboniferous System in the lower Yangtze Basin

  18. 交替层状组装技术与电化学沉积相结合制备银微/纳结构及超疏水表面

    Combining Layer-by-Layer Assembly with Electrodeposition of Silver Aggregates for Fabricating Superhydrophobic Surfaces

  19. 地震反演表明是因沉积相带发生变化。

    The seismic inversions indicate the sedimentary face has changed .

  20. 塔里木盆地库车坳陷侏罗系层序地层与沉积相

    Jurassic Sequence Stratigraphy and Sedimentary Facies in Kuqa Depression of Tarim Basin

  21. 沉积相类型对孔隙的发育有一定的控制作用。

    Facies types control to some extent the development of reservoir pores .

  22. 贵州泥盆系碳酸盐岩沉积相

    The Devonian carbonatite sedimentary facies in Guizhou Province phase and its significance

  23. 储层敏感性空间分布主要受沉积相控制。

    The space of distribution of reservoir sensitivity is controlled by sedimentary facies .

  24. 沉积相定量识别中的层次分析方法

    Hierarchic analysis method used in sedimentary facies quantitative recognition

  25. 沉积相的定量划分一直是沉积学中一个难以解决的问题。

    The quantitative division of sedimentary subfacies is a difficult problem of sedimentology .

  26. 相序的简易测量法泥石流沉积相模式

    A simple survey of the phase sequence a facies model of debris flow

  27. 一种用于沉积相分析的新型模式识别方法

    A new technique for pattern recognition of sedimentary facies

  28. 塔里木盆地西南坳陷和什拉甫地区中新统地层沉积相特征宜昌奥陶系沉积相分析

    The analysis of Ordovician sedimentary facies in Yichang region

  29. 广西南宁盆地早第三纪沉积相特征

    Feature s of the Palaeogene sedimentary facies of the Nanning basin , Guangxi

  30. 平面上储层物性受沉积相带控制。

    The reservoir physical properties at plane were controlled by sedimentary facies belt .