利用决策树方法识别复杂碳酸盐岩岩性 ——以苏里格气田苏东41-33区块为例
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王振洲(1993—),男,山东鄄城人,在读硕士研究生,从事数据挖掘及地球物理勘探研究。联系电话:15901036656,E-mail:gushi1004@sina.com。

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Lithology identification of complex carbonate rocks based on decision tree method:An example from Block Sudong41-33 in Sulige Gas Field
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    摘要:

    苏里格气田苏东41-33区块具有低孔、低渗透、非均质性强的特点,其奥陶系马家沟组碳酸盐岩储层受多期不同类型构造、沉积等作用,岩性复杂多样,对岩性的准确识别成为研究区开发的重点和难点。近年来,决策树方法作为一种机器学习方法,在地质学领域中的运用越来越受到关注,尤其在岩性预测方面。以测井、录井资料为基础,通过岩性参数特征分析,优选出对岩性较敏感的声波时差、自然伽马、光电吸收截面指数、密度、深侧向电阻率和补偿中子6种测井参数,通过分析这6种测井参数特征,构建基于决策树方法的多分类器,将岩性信息与岩石特征信息融合。与测井、录井资料的对比、分析结果表明,利用决策树方法识别复杂碳酸盐岩岩性的准确率超过80%,且相比朴素贝叶斯方法,其岩性识别的准确率提高了13%。

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    The reservoir of Block Sudong41-33 in Sulige Gas Field has the characteristics of low porosity,low permeability and high heterogeneity. The carbonate reservoir in Lower Ordovician Majiagou Formation were subjected to multi-stage multi-type construction,sedimentary and other effects,which makes the lithology complex and diverse,and thus the accurate identification of lithology has become a difficult problem of development in this area. In recent years,more and more attention has been focused on the use of decision tree method in machine learning in the field of geoscience,especially in lithology prediction. Based on the data of well logging and the analysis of lithological parameters,six kinds of well logging parameters that are sensitive to lithology were selected,which includes acoustic time difference(AC),natural gamma ray (GR),photoelectric absorption cross section index(PE),density(DEN),deep lateral resistivity(RLLD)and compensated neutron(CNL). Through the analysis of the six well logging parameters,a multi classifier was constructed based on decision tree method,and the information of lithology and rock characteristics were fused. Compared with the lithologic data of well logging,the recognition accuracy is over 80%. When compared with the Naive Bayesian,the accuracy of lithology recognition is improved by 13%.

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王振洲,张春雷,高世臣.利用决策树方法识别复杂碳酸盐岩岩性 ——以苏里格气田苏东41-33区块为例[J].油气地质与采收率,2017,24(6):25~33

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  • 在线发布日期: 2017-11-05
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