An intelligent recognition method of deep shale gas reservoir laminaset based on laminaset clustering and R-L-M algorithm

Yu Zeng , Fuqiang Lai , Haijie Zhang , Yi Jiang , Junwei Pu , Tongtong Luo , Xiaoxia Zhao
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Abstract

Lamina structures, as typical sedimentary features in shale formations, determine both the quality of shale reservoirs and fracturing effects. In this study, through electric imaging logging, based on core scanning photos, thin sections, and other data from the Wufeng-Longmaxi Formation shale reservoirs in the western Sichuan Block, the characteristics and classification scheme of deep shale gas reservoir laminaset were clarified. In addition, with core scale electrical images, the electrical imaging logging response characteristics of different types of laminaset were identified. Based on electrical imaging logging images, a laminaset clustering algorithm was designed to segment the laminaset and then Levenberg-Marquardt (L-M) algorithm was improved by introducing a random forest to obtain the R-L-M algorithm, which was used to extract key parameters of laminaset such as attitude, type, density, and thickness. The average accuracy, recall rate, and F1 score of laminaset recognition results of this algorithm were 14.82 % higher than those of a well-known international commercial software (T). This method was used to evaluate the Longmaxi Formation shale gas reservoir in the western Sichuan Block. The development density of clay-siliceous (organic-lean) laminaset from the Longyi 1–4 small layer to the lower Wufeng Formation firstly decreased and then increased and the minimum value was found in Longyi 1-1 small layer. In contrast, the development density of siliceous-clay laminaset (organic-rich) first increased and then gradually decreased and the maximum value was found in Longyi 1-1 small layer. The clay-siliceous laminaset (organic matters-contained) and the calcareous-clay laminaset (organic matters-contained) showed a stable developmental trend.
基于层状集聚类和R-L-M算法的深层页岩气藏层状集智能识别方法
层状构造作为页岩层的典型沉积特征,决定着页岩储层的质量和压裂效果。本研究通过电成像测井,基于四川西部区块五峰-龙马溪地层页岩储层的岩心扫描照片、薄切片等资料,明确了深层页岩气储层层理的特征和分类方案。此外,通过岩心尺度电图像,确定了不同类型层系的电成像测井响应特征。基于电成像测井图像,设计了层丛聚类算法对层丛进行划分,然后通过引入随机森林对 Levenberg-Marquardt 算法(L-M)进行改进,得到 R-L-M 算法,用于提取层丛的姿态、类型、密度和厚度等关键参数。该算法的层集识别结果的平均准确率、召回率和 F1 分数比国际知名商业软件(T)高出 14.82%。该方法被用于评估四川西部区块龙马溪地层页岩气藏。结果表明,龙马溪地层页岩气储层的粘土-硅质(有机-鳞片)层状发育密度从龙一1-4小层到五峰地层下部先减小后增大,最小值出现在龙一1-1小层。而硅质粘土层组(富含有机质)的发育密度先增大后逐渐减小,最大值出现在龙宜 1-1 小层。粘土-硅质层组(含有机质)和石灰质-粘土层组(含有机质)呈稳定的发育趋势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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