| 自然伽玛数字判别法研究沉积微相--以东濮盆地文留地区沙四段为例 |
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| 引用本文： | 李元元,方少仙.自然伽玛数字判别法研究沉积微相--以东濮盆地文留地区沙四段为例[J].沉积学报,1991,9(4):59-68. |
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| 作者姓名： | 李元元 方少仙 |
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| 作者单位： | 西南石油学院 |
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| 摘 要： | 本文主要讨论在油区取心井少的情况下,利用自然伽玛测井值研究沉积微相的平面分布的方法,并对中原油田文留区沙四段进行了实际的分析计算和划分,最后作出了该区沙四上段和沙四下段两张微相平面分布图。
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| 关 键 词： | 沉积微相 自然伽玛测井 单井相分析 数值判别 |
| 收稿时间： | 1989-10-12 |
Determine the Plan Extension of Sedimentary Microfacies by Means of GR Digit Judgment |
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| Institution: | Southwest Petroleum Institute |
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| Abstract: | It is a hard problem to determine the plan extension of sedimentary microfacies in cases of lacking the coring wells in oil fields. This paper discussed the method of the digit judgment using. GR log data, and mapped the plan extension of the sedimentary microfacies in Wenliu area, Dongpu Depression GR has sensitive response to the petrography of clastic rock.The GR's amplitude is affected by the intermediate value of mud content, so it is available to determine the ratio of sand to mud in strata, and the composing features of GR amplitude is a symble of sedimentary rhythm on sections. The digit judgment and analysis using GR logging data involves the following steps: 1) Chose one or more core wells, analyse their sedimentary microfacies by means of petrography, sedimentary structures, grain size and so on; 2) Evaluate the judgment criterion corresponding to microfacies and establish the GR model of them; 3) Judge the types of the microfacies using GR data in no-core wells, determine and map the plan extension of sedimentary mirofacies in study area. 2) and 3) can be finished in IBM-PC XT. The plan extension of sedimentary micrlfacies of the 3+4 and 5+6 intervals in upper Sha-4 member are provided. Through the analysis of the petrography, sedimentary structure, the featuer of grainsize and the trace fossils the core of well-109, the following microfacies can be outlined: overflow, channal point bar, midfan slump turbidity, midfan shallow water turbidity and externalfan fine turbidity. The GR standard model is established and criterion values of the facies are mapped. The maps (Fig.5 and Fig.6 ) showed: 1) 3+4 intervals in upper Sha-4 member, from north to south, vary from midfan slump turbidity, midfan shallow water turbidity to externalfan fine turbidity; 2) 5+6 intervals in lower Sha-4 member are subjected to the ephemeral facies complex in which the channal . poit bar deposit distributes along the line joining well-109, well-64, well-22, and overflow deposite cover others. |
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