Machine Learning Focal Mechanism Inversion for Hydraulic Fracturing Induced Earthquakes
dc.contributor.author | MacDonald, Megan | |
dc.date.accessioned | 2023-04-27T17:30:10Z | |
dc.date.available | 2023-04-27T17:30:10Z | |
dc.date.issued | 2023-04 | |
dc.description | Earth and Environmental Sciences Undergraduate Honours Theses | en_US |
dc.description.abstract | Hydraulic fracturing has been found to be a major contributor to the increase in induced seismicity worldwide, with pore pressure, poroelasticity, and coulomb stress transfer identified as the three main triggering mechanisms. However, there is still much to be learned about how these mechanisms operate in hydraulic fracturing-induced earthquakes. The accurate discrimination of these mechanisms requires a complete and precise earthquake catalog, particularly with regards to focal mechanisms, which provide insight into the changes in stress in the area surrounding the hypocenter. Determining the polarities of first motions by hand is a traditional method for identifying earthquake focal mechanisms, but it is not suitable for microearthquakes due to their low signal-noise ratio and the large volume of data involved. Machine learning, on the other hand, provides a reliable and efficient way to classify polarities. Thus, in this study we apply a machine learning-based first motion classifier to automatically invert focal mechanisms for induced earthquakes in the Tony Creek Dual Microseismic Experiment (ToC2ME). We then discuss the accuracy and efficiency of the application of machinelearning- based first motion classifier – DiTingMotion for hydraulic fracturing-induced earthquakes and investigate the associated mechanisms for earthquake triggering during the hydraulic fracturing. We have demonstrated that DiTingMotion is capable of classifying the polarities of earthquake first motions and characterizing focal mechanisms for induced earthquakes. By analyzing three major earthquake sequences during the ToC2ME experiment, our results illustrate that pore pressure, poroelasticity, and coulomb stress transfer can coexist during the hydraulic fracturing, although each may dominate during different stages. We suggest that a comprehensive understanding of geological settings, hydraulic fracturing operations, and the distribution of pre-existing faults/fractures is critical to comprehending the triggering of induced earthquakes. These factors play important roles in seismic activity and comprehending them is essential to mitigate the seismic hazard associated with hydraulic fracturing and optimize shale gas production. Keywords: Hydraulic Fracturing, Induced Seismicity, Machine Learning, Focal Mechanisms, Earthquake Triggering Mechanisms, Microearthquakes | en_US |
dc.identifier.uri | http://hdl.handle.net/10222/82539 | |
dc.title | Machine Learning Focal Mechanism Inversion for Hydraulic Fracturing Induced Earthquakes | en_US |
dc.type | Report | en_US |
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