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   成岩作用 在 地质学 分类中 的翻译结果: 查询用时:1.048秒
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成岩作用     
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  diagenesis
    Diagenesis and It's Comparative Study of Pyroclastic Rock, Dowsonite-Bearing Sandstone and Common Sandstone in Hailaer Basin
    海拉尔盆地火山碎屑岩、含片钠铝石砂岩与普通砂岩的成岩作用及其比较研究
短句来源
    DIAGENESIS AND DIAGENETIC TRAP OF DAANZHAI LIMESTONE
    大安寨石灰岩的成岩作用与成岩圈闭
短句来源
    OXYGEN AND CARBON ISOTOPIC COMPOSITION AND DIAGENESIS OF CARBONATE ROCKS
    氧、碳同位素组成与碳酸盐岩成岩作用
短句来源
    DIAGENESIS,BURIAL METAMORPHISM AND ANCHIMETAMORPHISM
    成岩作用、埋藏变质作用与近变质作用
短句来源
    STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN
    辽河盆地西部凹陷粘土矿物的成岩作用研究
短句来源
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  lithogenesis
    Some structural assemblages resulted from the deep - position deformation in the earth crust and a reverse progressive metamorphic belt are developed in the Salebasi nappe, in which the genetic relationship among mylonite, migmatite and migmatitic granite is very important for studying the deformation and lithogenesis within the deep - position 'of the earth crust in compressive orogenic background.
    萨勒巴斯推覆体中发育一套深层次变形构造组合和倒转递增变质带,其中糜棱岩、混合岩、混合花岗岩的成因关系对研究挤压造山背景下,地壳深层次变形作用和成岩作用具有特殊的意义。
短句来源
    Palynofacies is a particular sedimentary organic matter association that can reflect sedimentation and lithogenesis environment.
    孢粉相是反映一定沉积物以及成岩作用环境的显微沉积有机质组合。
短句来源
    Besides, the physical property of reservoir is influenced by lithologic characteristic and lithogenesis. If only analyze the data in the universal drill core and make statistic average, the method is definitely insufficient to represent the reservoir physical property, thus, particularly in this paper introduces the reservoir physical property and the relation with lithologic character in Leikoupo group and Jialingjiang group of Triassic system is studied and the lateral variation of fault and the factor determining the variation of the reservoir physical property is analyzed.
    储层物性又受岩性及成岩作用的影响 ,单从常规岩芯分析数据统计其平均值 ,不足以代表储层物性特征 ,文中着重探讨三叠系雷口坡组、嘉陵江组的物性特征及与岩性的关系 ,分析储层横向变化和影响储层物性变化的因素。
短句来源
    granites. Nd model age ranges from 1 400 Ma to 1 800 Ma with positive ε Nd(t) values, suggesting that plagio-monzonitic granitic gneisses are derived from juvenile crust,instead of from precambrian crystalline basement. Crystallization,lithogenesis,metamorphism and deformation took place simultaneously at 355 Ma±5 Ma.
    钕模式年龄在 14 0 0 Ma~ 180 0 Ma,εNd(t)为正值 ,反映斜长-二长花岗质片麻岩源于年青地壳 ,并不是前寒武纪结晶基底 ,结晶成岩作用和变质变形作用几乎是同时发生的 ,年龄为 35 5 Ma± 5 Ma
短句来源
  clastic diagenesis
    Clastic diagenesis and reservoir characteristics of Funing Formation in north slope of Gaoyou Depression in Subei Basin
    苏北盆地高邮凹陷北斜坡阜宁组成岩作用及储层特征
短句来源
    Numerical simulation of clastic diagenesis and its application
    碎屑岩成岩作用数值模拟及其应用
短句来源
    Based on the fundamental principle of Strontium Isotope Stratigraphy (SIS), i.e. strontium isotope composition of seawater is a determined value during the same geological time, we can apply the SIS to the research of clastic diagenesis in order to estimate the effect of marine facies and non-marine facies on diagenesis.
    基于同一地质历史时期海水的锶同位素组成为一定值的锶同位素地层学基本原理 ,可将锶同位素地层学用于碎屑岩成岩作用研究 ,以评价海相和非海相对成岩作用的影响。
短句来源
    Some sedimentary research fields in China, mainly including sedimentary environments and sedimentary systems, carbonate rocks, clastic diagenesis, sequence stratigraphy, sedimentary basin analysis and modeling, submarine sedimentation in the Chinese seas, oil-gas reservoir sedimentology and ore-deposit sedimentology, are briefly reviewed and prospected in the paper, which is dedicated to celebration of the twentieth anniversary of “Acta Sedimentologica Sinica”.
    主要选取沉积环境与沉积体系、碳酸盐岩、碎屑岩成岩作用、层序地层学、沉积盆地分析与模拟、中国海海底沉积作用、油气储层沉积学、矿床沉积学等若干领域 ,对我国沉积学作一简要回顾与展望 ,并借此庆祝《沉积学报》创刊二十周年。
短句来源
  diagenism
    It is held that the pore throat structure is the type of medium——small pore and microthroat,which is controlled by diagenism;
    结果表明:长6油层的孔喉结构主要为中、低孔—微喉型,孔喉结构的特征主要是受成岩作用的影响而形成的;
短句来源

 

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  diagenesis
Ore minerals are predominantly represented by pyrite formed at an early diagenesis stage in conditions of hydrogen sulfide-bacterial paleoecosystems and repeatedly altered in the process of subsequent sediment transformation.
      
The formation of suspended manganese minerals in bottom waters is explained by an additional Mn supply from underlying reduced sediments during their early diagenesis and oxygen depletion in the near-bottom nepheloid layer.
      
Wide variations in the isotopic composition (from 41.4 to 18.1‰ for δ13C and from 11.7 to 33.5‰ for δ18O) point to different formation conditions in the early diagenesis zone and the later catagenesis zone.
      
Isotopic criteria for the identification of early diagenesis zone are proposed.
      
The transition from sedimentogenesis to diagenesis (upper boundary of the early diagenesis zone) is accompanied by the alteration of carbon isotopic composition in the HCO-3(hydrosphere)-HCO-3(pore water of sediment)system.
      
更多          
  lithogenesis
Evolution of Isotopic Carbon Dioxide-Water Systems in Lithogenesis: Communication 1.
      
Evolution of Isotopic Carbon Dioxide-Water Systems in Lithogenesis: Communication 2.
      
A comprehensive lithological-geochemical study of Neopleistocene-Holocene sediments from Russian Arctic showed that these sediments formed in rather similar sedimentation conditions, which were common for polar lithogenesis.
      
It is shown that the type of terrigenous rock alkalinity is governed by peculiarities of the tectonic evolution of sedimentary-rock basins and stages of lithogenesis.
      
It is shown that all types of continental lithogenesis are valid for placer formation, although each type can contribute some specific features to the placer-forming process.
      
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