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沉积韵律控制下的厚层砂体水淹级别精细划分

Water flooded levels finely divided in thick sand bodies controlled by sedimentary rhythm

中文摘要英文摘要

本文提出了沉积韵律是控制厚层砂体内部水淹分布规律的主要控制因素,且稳定的泥岩夹层对多期河道砂体内部的水淹规律具有控制与分割作用。以稳定泥岩隔层为划分标志,将测井曲线划分为与沉积韵律一一对应的解释单元。以厚层砂体电阻率曲线的平均斜率及密度曲线的相对重心为判别参数,利用计算机自动判别出每一个解释单元中所包含的原始沉积韵律类型。以每单一韵律中部为对比标准层,韵律其他部位小层的电性、物性、时频特征参数与之相比较,结合小层与标准层相对位置关系,自动判定各小层水淹级别。11口密闭取心井处理结果与岩心分析结果相对比,总符合率达到78%以上。

his paper represents that the sedimentary rhythm is a primary factor to control the distribution regularity of water flooded zones in the thick sand bodies and the mudstone barriers have controlling and segmentation effect to the water flooded regularity of multi-channel. The stable mudstone barrier bed is adopted as the separates symbol for different interpretation unit that is identified from well logging curve so that only one sedimentary rhythm is contained in each interpretation unit. The Average slope of resistivity curve and relative center of gravity of density curve are adopted as discrimination parameter for identifying the original sedimentary rhythm by computer in each interpretation unit. Taking the middle of each rhythm as the standard layer with which the other layers in this rhythm are compared with electrical, petro-physical and time-frequency properties, the water flooded level of these layers are automatically discriminated to combining the relative location from the standard layer. The interpretation coincidental rate of The processing result of eleven sealed core wells and the result of core analysis is up to 78%.

李雪英、孟青云、文慧俭、马世忠、宋长和

地质学

水淹级别解释单元沉积韵律标准层泥岩夹层

Water flooded levelsInterpretation unitSedimentary rhythmStandard layerMudstone barrier?????

李雪英,孟青云,文慧俭,马世忠,宋长和.沉积韵律控制下的厚层砂体水淹级别精细划分[EB/OL].(2013-04-16)[2025-08-19].http://www.paper.edu.cn/releasepaper/content/201304-335.点此复制

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