礁相

  • 网络reef facies
礁相礁相
  1. 南海盆地形成演化构造背景和由周围大陆入海的大型河流三角洲在空间上控制着礁相碳酸盐岩的形成、发育和分布。

    The formation , development , and distribution of reef facies carbonate rocks were controlled in extensity by the South China Sea evolution tectonic setting and great deltas coming from continents .

  2. 珠江口盆地中新世碳酸盐岩及生物礁相研究

    Study of Miocene carbonate and reef facies in the Pearl River Mouth Basin

  3. 西沙海域东部岛礁区前寒武纪基底之上地层全部是较纯净的礁相碳酸盐岩,厚度达1250m,未被陆源碎屑岩覆盖;

    All basement rocks in eastern reef island area is covered with pure reef facies carbonate rocks in the thickness of 1250m .

  4. 西沙礁相第四纪地质研究取得新进展

    Quarternary reef facies geology study in Xisha Archipelago made new progress

  5. 东昆仑西段早-中二叠世生物礁相地层层序

    Stratigraphic Sequence of the Early-Middle Permian Reef in Western East Kunlun Mountains

  6. 风驱生物礁相模式&一种新的工作假说

    Wind-driven model of reef facies & a new working hypothesis

  7. 礁相地层自下而上分为5个岩组。

    The sequence consists of 5 lithologic formations .

  8. 西沙晚中新世以来礁相地层中有孔虫动物群的分布及其意义

    Foraminiferal fauna distribution in REEF-FACIES beds since late Miocene in Xisha Islands and its significance

  9. 西沙西永1井礁相第四纪地层的划分

    Quaternary reef stratigraphic division in hole xiyong-1

  10. 滩相和生物礁相灰(云)岩可成为良好的储集层;

    And limestones ( dolomites ) of beach and bioherm facies may be regarded as favourable reservoirs .

  11. 这种分布特征是礁相体系沉积的必然结果,但很难用推覆体来加以解释。

    This kind of distribution is the result of reef system sedimentation and difficult to be interpreted by nappe .

  12. 西沙海域晚新生代礁相碳酸盐岩形成条件及油气勘探前景

    Forming Condition of Late-Cenozoic Reef Facies Carbonate Rocks in Xisha Sea Area and Their Oil and Gas Exploration Potential

  13. 提出了台地边缘生物礁相&局限海台地相模式。

    The writer introduces the models of organic reef facies of platform margins and platform facies of barrier sea .

  14. 海平面相对上升与生物礁相沉积&以中国西南地区晚二叠世海绵礁为例

    Relative sea-level rises and organic reef deposition : an example from the Late Permian sponge reefs in southwestern China

  15. 主要的沉积相包括:台地边缘生物礁相、开阔台地相、海槽相。

    The main depositional facies types contained with carbonate platform margin reef facies , open platform facies , and trough .

  16. 上扬子台地晚二叠世礁相油气藏的断块构造控制与勘探方法建议

    Control of fault blocks upon the Late Permian reservoirs of reef facies in the Upper Yangtze Platform and exploration suggestions

  17. 根据储层特征参数及其影响因素分析,认为中中新统一上中新统是最有利的礁相碳酸盐岩储层发育带。

    The middle - to upper-Miocene is the most favorable reservoir based on reservoir character parameters and the controlling factors mentioned above .

  18. 渔塘铅锌矿床产于寒武纪碳酸盐岩中,主要受构造、岩性和藻礁相控制。

    The occurrence of the Yutang lead and zinc-sulfide deposit in the Cambrian carbonate rocks is controlled mainly by tectonic , lithologic and algae reef factors .

  19. 东部岛礁区为西沙隆起的较高部位,海水较浅,基底之上直接覆盖礁相沉积地层。

    The eastern reef island area , with shallow seawater , is higher parts of Xisha apophysis , where the basement is directly covered with reef facies carbonate rocks .

  20. 认真分析了碳酸盐岩礁滩的定义、分类、生物礁相模式等概念,并对生物礁滩地震反射特征的特点进行了描述。

    Serious analysis the carbonate rock reef beach definition , classification , organic reef facies model , and other related concepts . And describe characteristics of organic reef beach seismic reflection characteristics .

  21. 控矿沉积环境主要为台沟相带,次为局限&半局限台地相带、开阔台地相带、生物礁相带及海槽相带。

    The main ore controlling depositional environment is syneclise phase with the confined or semi-confined platform phase , open platform phase , organic reef phase and sea trough phase as the less important .

  22. 岩石化学分析结果表明,西沙海域礁相碳酸盐岩中主要元素、微量元素和同位素具有明显的分段性。

    Petrochemical analysis results of reef facies carbonate rocks in Xisha sea area indicate that the major element , trace element , and isotope in the rocks represent obvious subsection characteristics in stratum profile .

  23. 湘西渔塘早寒武世生物礁沉积相特征

    Sedimentary characteristics of Early Cambrian Yutang organic reefs in Western Hunan

  24. 塔里木盆地奥陶系礁滩相储集体特征

    Research on the Characteristics of Reef-bank Reservoirs in Ordovician , Tarim Basin

  25. 气烟囱效应&礁滩相岩性气藏的典型地震响应特征

    Gas chimney effect : typical seismic expression of lithologic shoal and Reef Gas Reservoirs

  26. 滇黔桂地区晚古生代、三叠纪生物礁沉积相及含油性初步研究

    Preliminary study on Triassic and late Paleozoic reef facies in Yunnan-Guizhou-Guangxi region and their petroleum prospect

  27. 储集岩主要是礁滩相灰岩白云石化后被溶解所形成。

    The main reservoir rocks formed from limestones of reef-bank facies which was dolomitizationed and then dissolved .

  28. 由北向南展示出礁坪相到礁核相再到礁前斜坡相的侧向演变。

    It has evolved late_rally , showing reef flat , core and front from north to south .

  29. 预测的苍溪礁滩相具有典型的进积型层序地层特征,在地震剖面上并且具有可靠的波组下拉现象。

    The predicted Cangxi reef and shoal facies show the characteristics of typical progradational sequence stratigraphy with reliable push-down .

  30. 阐述了多属性聚类分析技术,将优选出的敏感地震属性进行聚类分析,并将其应用于礁滩相储集层和油气预测中。

    The optimized seismic attributes followed by cluster analysis can be applied to prediction of reef reservoir and fluid property .