• 胶结作用造成的平均孔隙度丧失7.1%。

    The porosity loss caused by cementation is 7.1%.

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  • 成岩作用压实作用胶结作用溶蚀作用

    The diagenesis mainly comprise compaction cementation and dissolution.

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  • 压实作用胶结作用导致低渗主要原因

    The cementation and compaction were the key factors to make the reservoir low porous and permeable, an...

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  • 粘土作为石英晚期胶结作用抑制剂可能特别重要的。

    Clay coats can be particularly important as inhibitors of later quartz cementation.

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  • 破坏性成岩作用包括胶结作用压实作用硅化作用充填作用

    Constructive diageneses includes dolomitisation recrystallization dissolution and pressure solution while destructive diageneses include cementation compaction silication and filling.

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  • 砂岩主要成岩作用包括机械作用胶结作用溶蚀溶解作用

    The main diagenesis types of sandstones are the mechanical compression, cementation and dissolution.

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  • 黏粒尤其是胶粒胶结作用,对结构稳定性具有重要作用

    The cementation of clay, especially colloidal particle, plays an important role in the structural stability of soil samples.

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  • 早成岩阶段主要成岩作用碳酸盐胶结作用以及压实作用引起的颗粒重排

    Main diagenesis of the syndiagenesis is carbonate cementation in the shallow lake sheet sands and rearrangement caused by compaction.

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  • 影响储层物性因素主要沉积作用胶结作用溶蚀作用构造破裂作用

    The role of affecting reservoir physical property is deposition, cementation, dissolution and tectonic rupture. After researching reservoir, we divided it into three categories.

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  • 压实胶结作用主要破坏性成岩作用溶蚀作用主要的建设性成岩作用

    Compaction and cementation are the main destructive digenesis, while dissolution is the main constructive digenesis.

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  • 通过孔隙演化研究发现作用该区原始孔隙损失最主要因素;其次胶结作用

    The study of porosity evolution shows the compaction is the main cause resulting in the disappearance of primary porosity, and the next one is cementation.

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  • 胶结作用具有较高结构强度的根本原因,成演化过程红土有着“亲缘”关系。

    It is typical strong structural soil with higher structural strength result from agglutination, and its pedogenic evolutionary process is similar to that of laterite.

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  • 讨论了物理化学因素特别是结构特征游离氧化铁胶结作用力学性质重大影响

    The significant effect of various physicochemical factors, especially the structure characteristics and cementation of free ferric oxide on the mechanical properties is reviewed.

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  • 典型的成岩作用类型包括压实作用胶结作用溶蚀、溶解作用。成岩阶段中成岩a

    The main diagenesis includes compaction, cementation, corrosion and dissolution, etc. which belongs to stage a of middle diagenesis phase.

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  • 胶结作用压实作用主要孔隙破坏者,它们破坏几乎所有的原生孔隙和部分次生孔;

    Principal diageneses are cementation, compaction, pressure-solution, dolomitization, solution and fracturing, which control the reservoir properties of the bioclastic limestone member.

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  • 研究结果表明,本区储层砂岩较低渗透率主要成因成岩各种自生矿物充填胶结作用

    The results indicate that the forming mechanism of the low permeability in this area is the filling and cementation of autogenetic mineral during diagenesis.

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  • 压实作用胶结作用砂岩孔隙降低主要原因分别造成22%和15%的原生孔隙丧失

    Decrease of sandstone porosity is mainly caused by compaction and cementation, which contribute 22% and 15% to the loss of primary pores, respectively.

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  • 硅藻地表石灰沉积生物作用主要包括同化作用拦截粘结作用结壳作用胶结作用

    Diatoms biological functions on subaerial Karst sedimentation are studied chiefly in this paper, including assimilation, tapping and felting effects, encrustation, cementation.

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  • 作用、压作用胶结作用孔隙发育破坏性作用,溶蚀作用着使孔隙增大的作用

    Reservoir lithology is mainly quartz sandstone. Mechanical-chemical compaction, cementation play disruptive effects on porosities development, dissolution plays a constructive role on it.

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  • 吸力同时,原状峰值强度势均高于实样,原状样中铁结核胶结作用有关。

    As compared with the compacted specimens, the natural specimens were higher in the peak shear strength and the dilatancy due to the cementation effect of the iron and manganese oxides.

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  • 压实胶结作用降低层物性主要因素溶解作用形成次生孔隙是改善储层物性最重要的因素。

    Cementation is the main factor to decreasing porosity and permeability of reservoir while dissolution is the major reason of increasing porosity and permeability of reservoir.

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  • 胶结作用表现石英长石次生加大自生粘土矿物、碳酸盐和硬石膏胶结依次形成充填孔隙

    Cementation is showed by the secondary enlargement of quartz and feldspar, the successive formation and pores filling of cementing material of authigenic clay mineral, calcite and anhydrite, etc.

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  • 成岩作用中机械压实胶结作用使孔隙大量减少,而溶蚀作用构造作用形成裂缝有效地改善了储层性。

    Diagenesis including compaction and cementation may reduce pores a lot. And fractures formed by dissolution and tectonism can effectively improve physical property.

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  • 巴什基奇克组为偏碱性成岩环境,压实胶结作用中等偏弱,溶蚀作用改善孔隙结构,成岩阶段成岩A期。

    Dissolution of feldspar and lithic fragment make the pores linking. Diagenesis has reached the late diagenesis the stage A.

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  • 陆梁油田白垩系侏罗系成岩过程研究表明,储层孔隙演化主要压实作用溶蚀作用胶结作用密切关系。

    The study on the diagenesis course of Cretaceous and Jurassic reservoir in the Luliang oil field indicates that evolution of reservoir pores is closely related to compaction, solution and cementation.

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  • 土壤团聚体土壤重要组成部分、土壤结构的基本单位形成稳定主要通过土壤各种胶结物质胶结作用实现的。

    Soil aggregate is the main component of soil and the basic unit of soil structure. Its formation and stability are realized by the effects of all kinds of cementing substance in soil.

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  • 以岩石学特征基础,描述了成岩过程中压作用胶结作用、溶解作用次生孔隙特征,以及次生孔隙本区分布

    The characteristics of compaction and solution, cementation, secondary porosity during diagenesis processes and the distribution of secondary porosity zone in Chezhen Depression are described.

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  • 储集层储集性能成岩作用研究表明,早成岩期的压实作用、多种矿物胶结作用使储集层物性变差孔隙度降低的两个重要的成岩控因;

    The study shows that the early diagenetic com paction and multi-mineral cementation are major effective factors that lead to its poor petrophysical property and low porosity;

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  • 储集层储集性能成岩作用研究表明,早成岩期的压实作用、多种矿物胶结作用使储集层物性变差孔隙度降低的两个重要的成岩控因;

    The study shows that the early diagenetic com paction and multi-mineral cementation are major effective factors that lead to its poor petrophysical property and low porosity;

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