Seismic Anisotropy Reveals Stress Changes around a Fault as It Is Activated by Hydraulic Fracturing
نویسندگان
چکیده
Abstract Subsurface stress conditions evolve in response to earthquakes or fluid injection. Using observations of an induced seismicity sequence from a dense local array, anisotropy analysis is employed characterize changes around fault. The dataset comprises high signal-to-noise ratio S-wave data 300 events, ranging magnitude −0.45 4.1, recorded on 98 three-component geophones cemented shallow wells. It found that the orientation fast direction remains relatively constant for all stations over time, but anisotropy, as measured by delay time between and slow S wave, exhibits significant variations. Some experience systematic increase decrease with spatial coherence about injection well. due hydraulic fracturing, aseismic slip, observed are modeled determine best fit changes. Our indicates creation network tensile fractures during likely be cause This study confirms measurements seismic reflects evolving state fault prior rupture.
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ژورنال
عنوان ژورنال: Seismological Research Letters
سال: 2022
ISSN: ['0895-0695', '1938-2057']
DOI: https://doi.org/10.1785/0220210282