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Research and application of logging lithology identification for igneous reservoirs based on deep learning

机译:基于深度学习的火岩岩岩鉴定的研究与应用

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Igneous reservoirs are characterized by heterogeneity and anisotropy, which makes logging interpretation difficult. In order to identify their lithology, deep learning to establish the deep belief network (DBN) by logging data is proposed in this study. By the least square method, the mean square error function is used to measure network performance, and network parameters such as the number of RBMs, the number of neurons in the hidden layer of each RBM, and the classification boundary. Then, the logging data that require interpretation are processed by DBN that is trained. The results are divided into four cases and are analyzed and discussed further. First, the lithology classification results are continuous, stable and the formations are thick. At this point, there is no need to correct the results. Second, there are several lithological discontinuities in the thick layer. In this case, if the thickness of the discontinuous formations is >0.5 m, the corresponding formations can be divided according to the identification results; if the thickness of the discontinuous formations are less than or equal to 0.5 m, the discontinuous formations are merged into adjacent thick formations. Third, the lithology of formations cannot be determined by the identification result. At this time, it is generally considered that the lithology of the formations do not appear in the training samples. Fourth, there are a few identification results for one formation. At this point, a cross plot is adopted to correct these results. An accuracy of 94.8% is achieved for lithology identification by the deep belief network with lithology correction. (C) OD 2019 Elsevier B.V. All rights reserved.
机译:发芽的水库的特点是异质性和各向异性,使测井解释变得困难。为了识别他们的岩性,在本研究中提出了通过测井数据建立深度信仰网络(DBN)的深度学习。通过最小的方形方法,平均误差函数用于测量网络性能,以及诸如RBMS的数量的网络参数,每个RBM的隐藏层中的神经元数,以及分类边界。然后,需要解释的日志记录数据由训练的DBN处理。结果分为四种情况,并进一步分析并讨论。首先,岩性分类结果是连续的,稳定的,地层厚。此时,无需纠正结果。其次,厚层有几种岩性不连续性。在这种情况下,如果不连续地层的厚度为0.5μm,则可以根据鉴定结果分割相应的形成;如果不连续形成的厚度小于或等于0.5μm,则不连续地层合并到相邻的厚度中。第三,无法通过鉴定结果确定地层的岩性。此时,通常认为地层的岩性不会出现在训练样本中。第四,一种形成有一些识别结果。此时,采用交叉图来纠正这些结果。对于具有岩性校正的深度信仰网络,实现了94.8%的准确性。 (c)OD 2019 Elsevier B.v.保留所有权利。

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