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地层格架模型
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  formation frame model
     3D digital formation frame model, reservoir sand model and petrophysical model are established in the way of point - line - plane - cube to study the reservoir distribution feature and forming law, to deeply understand and evaluate the structure, fluid property and development law of BASUP53 reservoir, and to improve the development potential.
     根据构造模型,从点-线-面-体建立全三维的数字化地层格架模型、储层砂体模型和物性模型,对BASUP53油藏储层的分布特点和成藏规律进行研究,以加深对BASUP53油藏的构造、储层、流体性质及开发规律的认识和评价,提高该油藏的开发潜力。
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  “地层格架模型”译为未确定词的双语例句
     From the point of sequence boundary surface characteristics, S\-2,S\-3,S\-4 and S\-5 are type\|Ⅰ sequences, and S\-1 and S\-6 are type\|Ⅱ sequences. Then the paper correlated each sequence from the study area, and built the sequence stratigraphy framework of lower and middle Triassic which showed the evolution of patterns and their relationship of different system tract.
     按层序底面性质可分出 4个Ⅰ型层序 (S2 、S3、S4、S5)和 2个Ⅱ型层序 (S1 、S6) ,并进行了区域层序对比 ,进而建立了区内下、中三叠统层序地层格架模型 ,详细讨论了各层序的次级组成单元 (体系域 )的几何形态和相互关系随时间的迁移所发生的相应变化
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     The definite modeling approach is adopted to establish the reservoir geologic model.
     ②建立井模型和地层格架模型;
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     Taking the upper member of Guantao Formation of the Neogene in the Zhanhua Sag of the Ji-yang Depression,the Bohaiwan Basin as an example,a study of the high-resolution sequence stratigraphy has been carried out.
     对渤海湾盆地济阳坳陷沾化凹陷上第三系馆陶组上段的沉积地层开展了高分辨率层序地层学研究,建立了层序地层格架模型和油藏精细地质模型,为提高油气采收率奠定了基础。
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  相似匹配句对
     The definite modeling approach is adopted to establish the reservoir geologic model.
     ②建立井模型地层格架模型;
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     model.
     模型
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     A Discussion on the Stratigraphic Framework of Sedimentary Basins
     论盆地的地层格架
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     Obviously, EVA model turns out a scientific appraisals to motivate the managers.
     该模型为:
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     STRATUM
     地层
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The study area included Sichuan,Yunnan,Guizhou and Guangxi, there, the strata of lower and middle Triassic are widely distributed and well developed, it is one of important areas can be used to study the sequence division, correlation and framework of Triassic system. Therefore, the paper based on the sequence stratigraphy theory, discussed in detail the characteristics of the sequence boundary surface which included uncomformity surface, lithologic\|character and facies change surface, karst surface and errosion...

The study area included Sichuan,Yunnan,Guizhou and Guangxi, there, the strata of lower and middle Triassic are widely distributed and well developed, it is one of important areas can be used to study the sequence division, correlation and framework of Triassic system. Therefore, the paper based on the sequence stratigraphy theory, discussed in detail the characteristics of the sequence boundary surface which included uncomformity surface, lithologic\|character and facies change surface, karst surface and errosion surface, etc. Among them, the uncomformlty surface, errosion surface and karst surface are type\|Ⅰ boundary surface, and lithologic\|character and facies change surface are type\|Ⅱ boundany surfaces. Based on the above, the paper divided lower and middle Triassic into six third order seauences, which are namedas S\-1 to S\-6, In the view of geologic time, it is known that early Triassic period prolonged 3.9 Ma, S 0 S\-1,S\-2 and S\-3 prolonged 1.3 Ma respectively, and middle Trassic period prolonged 6.1 Ma, S\-4,S\-5 and S\-6 prolonged 2.03 Ma respectively. From the point of sequence boundary surface characteristics, S\-2,S\-3,S\-4 and S\-5 are type\|Ⅰ sequences, and S\-1 and S\-6 are type\|Ⅱ sequences. Then the paper correlated each sequence from the study area, and built the sequence stratigraphy framework of lower and middle Triassic which showed the evolution of patterns and their relationship of different system tract.

在对研究区不同相带内典型剖面详细观测、层序界面识别基础上 ,将区内下、中三叠统划分出六个三级层序 ,分别命名为S1 ~S6,其中下三叠统印度阶一个 (S1 )、奥伦尼阶两个 (S2 ~S3) ,中三叠统安尼阶两个 (S4~S5)、拉丁阶一个 (S6) ,从年代地层考虑早三叠延续时限为 3.9Ma ,则S1 、S2 、S3层序延续的时限平均为 1 .3Ma。中三叠统延续的时限为 6.1Ma ,则S4、S5、S6 层序所延续的时限平均分别为 2 .0 3Ma。按层序底面性质可分出 4个Ⅰ型层序 (S2 、S3、S4、S5)和 2个Ⅱ型层序 (S1 、S6) ,并进行了区域层序对比 ,进而建立了区内下、中三叠统层序地层格架模型 ,详细讨论了各层序的次级组成单元 (体系域 )的几何形态和相互关系随时间的迁移所发生的相应变化

The paper began with the basic theories of seismic exploration,analyzed the nature of solving geologic problems using seismic inversion. Then we analyzed and discussed the impact on ability of using well log constrained inversion to solve geologic problems from three aspects:quality of basic data,the method of well log constrained inversion and the selection of inversion parameter and building up the model of stratigraphic framework and extrapolation control.Finally,we conclude that the ability of using...

The paper began with the basic theories of seismic exploration,analyzed the nature of solving geologic problems using seismic inversion. Then we analyzed and discussed the impact on ability of using well log constrained inversion to solve geologic problems from three aspects:quality of basic data,the method of well log constrained inversion and the selection of inversion parameter and building up the model of stratigraphic framework and extrapolation control.Finally,we conclude that the ability of using well log constrained inversion to solve geologic problems is limited and propose several aspects we should pay attention to in order to improve the ability of using well log constrained inversion to solve geologic problems.

本文首先从地震勘探的基本原理出发 ,分析地震反演解决地质问题的本质 ;然后从基础资料的品质、测井约束地震反演方法及反演参数的选择、地层格架模型建立和外推控制三个方面 ,分析、探讨测井约束地震反演解决地质问题的能力 ;最后认为 ,测井约束地震反演解决地质问题的能力是有限的 ,并提出了提高测井约束地震反演解决地质问题能力应重视的几个因素

From the basic principle of seismic exploration, this paper analyzes the essence of applying seismic inversion after stack to the solution of geological problems. In the light of such aspects as the quality of basic data, the selection of techniques for logging constrained seismic inversion and the choice of inversion parameters, the setting up of the stratigraphic framework model and the extrapolation control, the paper also deals with factors affecting geological effects of logging constrained seismic inversion....

From the basic principle of seismic exploration, this paper analyzes the essence of applying seismic inversion after stack to the solution of geological problems. In the light of such aspects as the quality of basic data, the selection of techniques for logging constrained seismic inversion and the choice of inversion parameters, the setting up of the stratigraphic framework model and the extrapolation control, the paper also deals with factors affecting geological effects of logging constrained seismic inversion. It is held that the capability of logging constrained seismic inversion to solve geological problems is rather limited. Some measures are put forward for improving geological effects of logging constrained seismic inversion.

从地震勘探的基本原理出发 ,分析了叠后地震反演解决地质问题的本质。从基础资料的品质 ,测井约束地震反演的方法及反演参数的选择 ,地层格架模型的建立和外推控制这几个方面分析影响测井约束地震反演的地质效果。笔者认为 ,测井约束地震反演解决地质问题的能力是有限的 ,并提出了提高测井约束地震反演的地质效果应采取的若干措施。

 
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