Hydromechanical Controls on the Spatiotemporal Patterns of Injection‐Induced Seismicity in Different Fault Architecture: Implication for 2013–2014 Azle Earthquakes
Abstract
Recent observations of seismic events at the subsurface energy exploration sites show that spatial and temporal correlations sometimes do not match the spatial order of the known or detected fault location from the injection well. This study investigates the coupled flow and geomechanical control on the patterns of induced seismicity along multiple basement faults that show an unusual spatiotemporal relation with induced seismicity occurring in the far field first, followed by the near field. Two possible geological scenarios considered are (1) the presence of conductive hydraulic pathway within the basement connected to the distant fault (hydraulic connectivity) and (2) no hydraulic pathway, but the coexistence of faults with mixed polarity (favorability to slip) as observed at Azle, TX. Based on the Coulomb stability analysis and seismicity rate estimates, simulation results show that direct pore pressure diffusion through a hydraulic pathway to the distant fault can generate a larger number of seismicity than along the fault close to the injection well. Prior to pore pressure diffusion, elastic stress transfer can initiate seismic activity along the favorably oriented fault, even at the longer distance to the well, which may explain the deep 2013–2014 Azle earthquake sequences. This study emphasizes that hydrological andmore »
- Authors:
-
- Geotechnology and Engineering Department Sandia National Laboratories Albuquerque NM USA
- Geomechanics Department Sandia National Laboratories Albuquerque NM USA
- Publication Date:
- Research Org.:
- Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
- Sponsoring Org.:
- USDOE National Nuclear Security Administration (NNSA)
- OSTI Identifier:
- 1664591
- Alternate Identifier(s):
- OSTI ID: 1664593; OSTI ID: 1670767
- Report Number(s):
- SAND2020-10450J
Journal ID: ISSN 2169-9313; e2020JB020402
- Grant/Contract Number:
- 200180; AC04-94AL85000
- Resource Type:
- Published Article
- Journal Name:
- Journal of Geophysical Research. Solid Earth
- Additional Journal Information:
- Journal Name: Journal of Geophysical Research. Solid Earth Journal Volume: 125 Journal Issue: 9; Journal ID: ISSN 2169-9313
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES
Citation Formats
Chang, K. W., and Yoon, H. Hydromechanical Controls on the Spatiotemporal Patterns of Injection‐Induced Seismicity in Different Fault Architecture: Implication for 2013–2014 Azle Earthquakes. United States: N. p., 2020.
Web. doi:10.1029/2020JB020402.
Chang, K. W., & Yoon, H. Hydromechanical Controls on the Spatiotemporal Patterns of Injection‐Induced Seismicity in Different Fault Architecture: Implication for 2013–2014 Azle Earthquakes. United States. https://doi.org/10.1029/2020JB020402
Chang, K. W., and Yoon, H. Wed .
"Hydromechanical Controls on the Spatiotemporal Patterns of Injection‐Induced Seismicity in Different Fault Architecture: Implication for 2013–2014 Azle Earthquakes". United States. https://doi.org/10.1029/2020JB020402.
@article{osti_1664591,
title = {Hydromechanical Controls on the Spatiotemporal Patterns of Injection‐Induced Seismicity in Different Fault Architecture: Implication for 2013–2014 Azle Earthquakes},
author = {Chang, K. W. and Yoon, H.},
abstractNote = {Recent observations of seismic events at the subsurface energy exploration sites show that spatial and temporal correlations sometimes do not match the spatial order of the known or detected fault location from the injection well. This study investigates the coupled flow and geomechanical control on the patterns of induced seismicity along multiple basement faults that show an unusual spatiotemporal relation with induced seismicity occurring in the far field first, followed by the near field. Two possible geological scenarios considered are (1) the presence of conductive hydraulic pathway within the basement connected to the distant fault (hydraulic connectivity) and (2) no hydraulic pathway, but the coexistence of faults with mixed polarity (favorability to slip) as observed at Azle, TX. Based on the Coulomb stability analysis and seismicity rate estimates, simulation results show that direct pore pressure diffusion through a hydraulic pathway to the distant fault can generate a larger number of seismicity than along the fault close to the injection well. Prior to pore pressure diffusion, elastic stress transfer can initiate seismic activity along the favorably oriented fault, even at the longer distance to the well, which may explain the deep 2013–2014 Azle earthquake sequences. This study emphasizes that hydrological and geomechanical features of faults will locally control poroelastic coupling mechanisms, potentially influencing the spatiotemporal pattern of injection-induced seismicity, which can be used to infer subsurface architecture of fault/fracture networks},
doi = {10.1029/2020JB020402},
journal = {Journal of Geophysical Research. Solid Earth},
number = 9,
volume = 125,
place = {United States},
year = {Wed Aug 26 00:00:00 EDT 2020},
month = {Wed Aug 26 00:00:00 EDT 2020}
}
https://doi.org/10.1029/2020JB020402
Web of Science
Figures / Tables:
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