Abstract

Automatic detection of low-magnitude earthquakes has become an increasingly important research topic in recent years due to a sharp increase in induced seismicity around the globe. The detection of low-magnitude seismic events is essential for microseismic monitoring of hydraulic fracturing, carbon capture and storage, and geothermal operations for hazard detection and mitigation. Moreover, the detection of micro-earthquakes is crucial to understanding the underlying mechanisms of larger earthquakes. Various algorithms, including deep learning methods, have been proposed over the years to detect such low-magnitude events. However, there is still a need for improving the robustness of these methods in discriminating between local sources of noise and weak seismic events. In this study, we propose a convolutional neural network (CNN) to detect seismic events from shallow borehole stations in Groningen, the Netherlands. We train a CNN model to detect low-magnitude earthquakes, harnessing the multi-level sensor configuration of the G-network in Groningen. Each G-network station consists of four geophones at depths of 50, 100, 150, and 200 m. Unlike prior deep learning approaches that use 3-component seismic records only at a single sensor level, we use records from the entire borehole as one training example. This allows us to train the CNN model using moveout patterns of the energy traveling across the borehole sensors to discriminate between events originating in the subsurface and local noise arriving from the surface. We compare the prediction accuracy of our trained CNN model to that of the STA/LTA and template matching algorithms on a two-month continuous record. We demonstrate that the CNN model shows significantly better performance than STA/LTA and template matching in detecting new events missing from the catalog and minimizing false detections. Moreover, we find that using the moveout feature allows us to effectively train our CNN model using only a fraction of the data that would be needed otherwise, saving plenty of manual labor in preparing training labels. The proposed approach can be easily applied to other microseismic monitoring networks with multi-level sensors.

Highlights

  • Automatic detection of low-magnitude earthquakes has been a longstanding research problem in seismology

  • We demonstrate that despite being trained on a relatively small amount of data, the convolutional neural network (CNN) model shows significantly better performance than short-term average of the amplitudes (STA)/long-term average of the amplitudes (LTA) and template matching in detecting new events missing from the catalog and minimizing false detections

  • We evaluate the precision of the CNN model on the two-month dataset to be 88.9%, while the STA/LTA detection precision does not exceed 67% on any of the threshold values tried

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Summary

Introduction

Automatic detection of low-magnitude earthquakes has been a longstanding research problem in seismology. Since CNNs are well-known for identifying spatial features in data, we use the moveout pattern of the energy traveling across the borehole sensors at a single station as the main distinguishing factor between events originating in the subsurface and noise coming from the surface. This is often the most challenging problem in detecting low-magnitude earthquakes. We demonstrate that despite being trained on a relatively small amount of data, the CNN model shows significantly better performance than STA/LTA and template matching in detecting new events missing from the catalog and minimizing false detections. We discuss the key findings of this study and their implications

Methodology
Training Data Selection and Pre-Processing
CNN Architecture
Performance Evaluation on Continuous Data
Results
Findings
Discussion and Conclusions
Full Text
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