Abstract

Fault interpretation is an important part of seismic structural interpretation and reservoir characterization. In the conventional approach, faults are detected as reflection discontinuity or abruption and are manually tracked in post-stack seismic data, which is time-consuming. In order to improve efficiency, a variety of automatic fault detection methods have been proposed, among which widespread attention has been given to deep learning-based methods. However, deep learning techniques require a large amount of marked seismic samples as a training dataset. Although the amount of synthetic seismic data can be guaranteed and the labels are accurate, the difference between synthetic data and real data still exists. To overcome this drawback, we apply a transfer learning strategy to improve the performance of automatic fault detection by deep learning methods. We first pre-train a deep neural network with synthetic seismic data. Then we retrain the network with real seismic samples. We use a random sample consensus (RANSAC) method to obtain real seismic samples and generate corresponding labels automatically. Three real 3D examples are included to demonstrate that the fault detection accuracy of the pre-trained network models can be greatly improved by retraining the network with a few amount of real seismic samples.

Highlights

  • IntroductionInterpreters identify the faults as reflection discontinuity or abruption and track faults on Another type of attribute highlights faults by computing the difference between seismic traces, e.g., variance attribute [4], curvature attribute [5] and gradient magnitude [6]

  • The first 3D seismic volume used to test the effect of transfer learning is the seismic data we use to extract the real training samples

  • The real seismic samples for transfer learning are all extracted from the first 3D seismic data, and the retrained network models can work pretty well in the second and third seismic data, indicating that the retrained network models can be used for detecting similar type of faults in a different area

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Summary

Introduction

Interpreters identify the faults as reflection discontinuity or abruption and track faults on Another type of attribute highlights faults by computing the difference between seismic traces, e.g., variance attribute [4], curvature attribute [5] and gradient magnitude [6]. Since these attributes are with seismic reflection removed and discontinuities highlighted, they can be regarded as fault images

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