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Log-based lithology identification of volcanic rocks using random forest method: A case study of Carboniferous strata in the Dixi area, Junggar Basin |
SHANG Ya-Zhou1(), ZHANG Zhao-Hui1(), XU Duo-Nian2, ZHAO Wen-Wen1, CHEN Hua-Yong3, HAN Hai-Bo1 |
1. School of Geological and Mining Engineering, Xinjiang University, Urumqi 830047, China 2. Research Institute of Petroleum Exploration and Development-Northwest (NWGI), PetroChina, Lanzhou 730020, China 3. Research Institute of Exploration and Development, PetroChina Xinjiang Oilfield Company, Karamay 834000, China |
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Abstract The accurate lithologyidentification of volcanic rocksserves as a significant foundation for the efficient exploration and exploitation of volcanic reservoirs. However, volcanic reservoirs exhibit intricate lithologies, longitudinalmultistagesuperimposition, and fast transverse phase transition, which reduce the accuracy of crossplots in lithologyidentification ofvolcanic reservoirs. Based on the optimal parameter combination of the model determined through grid search and orthogonal experiments, this study quantitatively evaluatedthe effects of conventional log curves on the lithologyidentification of volcanic rocks. Withthe natural gamma ray, compensated neutron, sonic interval transit time, and formation resistivity as lithologic indicators, this study builtan intelligent model for the lithology identification of Carboniferous volcanic rocks in the Dixi area in the Junggar Basin using therandom forest method. This study identified the lithologies of thecored intervalswith a cumulative thickness of 870 m infive cored wells in the study area, with the coincidence ratesof the identification results with thin section identification results and core description resultsreaching 76.67% and 85.98%, respectively. This suggestssignificant identification effects. Therefore, this studysets the stagefor the fine-scale evaluation of volcanic reservoirs in the study area.
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Received: 08 July 2023
Published: 19 September 2024
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Geographical location of the study area
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Comprehensive column chart of lithology and stratigraphy in the study area
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岩性标签 | 岩性 | 岩石 薄片数 | 占比/% | 钻井取心累 计长度/m | 占比/% | 1 | 凝灰岩 | 185 | 31.04 | 74.8 | 17.72 | 2 | 二长玢岩 | 38 | 6.38 | 11.52 | 2.73 | 3 | 花岗斑岩 | 86 | 14.43 | 125 | 29.61 | 4 | 安山岩 | 93 | 15.60 | 68.96 | 16.34 | 5 | 玄武岩 | 95 | 15.94 | 97.83 | 23.18 | 6 | 霏细岩 | 7 | 1.17 | 3.98 | 0.94 | 7 | 流纹岩 | 17 | 2.85 | 0.89 | 0.21 | 8 | 霏细斑岩 | / | / | 6.4 | 1.52 | 0 | 火山角砾岩 | 61 | 10.23 | 23.13 | 5.48 | 10 | 其他 | 14 | 2.35 | 9.6 | 2.27 |
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Statistical of the distribution of thin slices and drilling cores with different lithology rocks
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Schematic diagram of decision tree principle
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Schematic diagram of random forest principle
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岩性标签 | 岩性 | 样本数 | 占比/% | 1 | 凝灰岩 | 654 | 33.08 | 2 | 二长玢岩 | 160 | 8.09 | 3 | 花岗斑岩 | 539 | 27.26 | 4 | 安山岩 | 214 | 10.82 | 5 | 玄武岩 | 215 | 10.88 | 6 | 霏细岩 | 42 | 2.12 | 7 | 流纹岩 | 106 | 5.36 | 8 | 霏细斑岩 | 47 | 2.38 | / | 汇总 | 1977 | / |
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Statistical of the distribution of the different lithological samples in the dataset
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Cross plot of 2D lithology identification with different logging parameters
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Intersection diagram of 3D lithology identification with different logging parameters
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Parameters tuning for random forest
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参数 | 搜索范围 | 步长 | 最优值 | 迭代次数 | 2~230 | 2 | 14 | 内部节点再划分所需最小样本数 | 2~50 | 2 | 4 | 叶子结点最小样本数 | 1~50 | 1 | 1 | 最大树深度 | 3~15 | 1 | 6 |
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Parameters tuning for random forest
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Comparison of different lithology identification results
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Comparison of confusion matrix for different lithology identification models
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岩性标签 | 岩性 | SVM | KNN | DT | RF | 1 | 凝灰岩 | 0.91 | 0.93 | 0.96 | 0.98 | 2 | 二长玢岩 | 0.48 | 0.86 | 0.80 | 0.94 | 3 | 花岗斑岩 | 1 | 1 | 0.98 | 1 | 4 | 安山岩 | 0.92 | 0.92 | 0.91 | 0.95 | 5 | 玄武岩 | 0.95 | 0.94 | 0.97 | 0.96 | 6 | 霏细岩 | 1 | 0.80 | 1 | 1 | 7 | 流纹岩 | 1 | 1 | 1 | 0.98 | 8 | 霏细斑岩 | 0 | 0.44 | 0.93 | 0.92 |
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Fl_score of different lithology identification models
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井号 | 岩性识别长度 /m | 岩石薄片 | 钻井取心 | 识别正确/块 | 识别错误/块 | 准确性/% | 识别正确/m | 识别错误/m | 准确性/% | dx182 | 400 | 41 | 22 | 65.08 | 7.18 | 3.5 | 67.23 | dx183 | 270 | 17 | 1 | 94.44 | 12.56 | 5.12 | 71.04 | dx402 | 80 | 8 | 2 | 80.00 | 16.93 | - | 100.00 | dx17 | 20 | 9 | 1 | 90.00 | 8.7 | - | 100.00 | dx172 | 100 | 17 | 2 | 89.47 | 7.48 | - | 100.00 | 统计 | 870 | 92 | 28 | 76.67 | 52.85 | 8.62 | 85.98 |
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Lithological identification results of random forest models with different well
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Comparison of classification results from different volcanic rock lithology identification models for well dx402
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