基于半监督学习的断层导向地震地层解释

H. Di, C. Kloucha, Cen Li, A. Abubakar, Zhun Li, Houcine Ben Jeddou, H. Mustapha
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摘要

圈定地震地层特征和沉积相对于成功地进行地下储层填图和识别具有重要意义。可靠的地震地层解释面临着两大挑战。第一个挑战是最大限度地实现这一过程的自动化,特别是随着地震数据规模的增加和目标地层的复杂性,而第二个挑战是有效地将现有结构纳入地层模型构建中。机器学习,特别是卷积神经网络(CNN),已被引入到通过监督学习辅助地震地层学解释中。然而,可用的专家标签数量少,极大地限制了这种监督CNN的性能。此外,现有的大多数CNN实现仅基于幅度,未能使用必要的结构信息(如故障)来约束机器学习。为了解决这两个问题,本文提出了一种断层导向地震地层解释的半监督学习工作流,该工作流由两个部分组成。第一部分是地震特征工程(SFE),旨在通过无监督卷积自编码器(CAE)学习提供的地震和断层数据;第二部分是地层模型构建(SMB),旨在通过有监督的CNN,在SFE CAE提取的特征与经验丰富的译员提供的目标地层标签之间建立最优映射函数。通过将SFE CAE的编码器嵌入到SMB CNN中,将两个组件连接起来,从而迫使SMB基于整个研究区域中普遍存在的这些特征进行学习,而不是仅在有限的训练数据中进行学习;相应地,过度拟合的风险被大大消除。更创新的是,通过定制两个输出分支的SMB CNN,引入断层约束,其中一个用于匹配目标地层,另一个用于重建输入断层,使断层继续为SMB学习过程做出贡献。通过对实际地震数据集的应用,验证了断层导向地震地层解释的有效性,机器预测结果不仅与人工解释结果吻合较好,而且清晰地反映了研究区沉积过程。
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Fault-Guided Seismic Stratigraphy Interpretation via Semi-Supervised Learning
Delineating seismic stratigraphic features and depositional facies is of importance to successful reservoir mapping and identification in the subsurface. Robust seismic stratigraphy interpretation is confronted with two major challenges. The first one is to maximally automate the process particularly with the increasing size of seismic data and complexity of target stratigraphies, while the second challenge is to efficiently incorporate available structures into stratigraphy model building. Machine learning, particularly convolutional neural network (CNN), has been introduced into assisting seismic stratigraphy interpretation through supervised learning. However, the small amount of available expert labels greatly restricts the performance of such supervised CNN. Moreover, most of the exiting CNN implementations are based on only amplitude, which fails to use necessary structural information such as faults for constraining the machine learning. To resolve both challenges, this paper presents a semi-supervised learning workflow for fault-guided seismic stratigraphy interpretation, which consists of two components. The first component is seismic feature engineering (SFE), which aims at learning the provided seismic and fault data through a unsupervised convolutional autoencoder (CAE), while the second one is stratigraphy model building (SMB), which aims at building an optimal mapping function between the features extracted from the SFE CAE and the target stratigraphic labels provided by an experienced interpreter through a supervised CNN. Both components are connected by embedding the encoder of the SFE CAE into the SMB CNN, which forces the SMB learning based on these features commonly existing in the entire study area instead of those only at the limited training data; correspondingly, the risk of overfitting is greatly eliminated. More innovatively, the fault constraint is introduced by customizing the SMB CNN of two output branches, with one to match the target stratigraphies and the other to reconstruct the input fault, so that the fault continues contributing to the process of SMB learning. The performance of such fault-guided seismic stratigraphy interpretation is validated by an application to a real seismic dataset, and the machine prediction not only matches the manual interpretation accurately but also clearly illustrates the depositional process in the study area.
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