Taeho Kim
Postdoctoral Scholar, Energy Science and Engineering
All Publications
- Evidence of Direct Fluid Connections between Hydraulic Fractures and Pre-existing Faults at the Cape Station EGS Project 51st Workshop on Geothermal Reservoir Engineering 2026
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Finite Size Effects on Seismicity Induced by Fluid Injection in a Discrete Fault Network With Rate-and-State Friction
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2025; 130 (7)
View details for DOI 10.1029/2024JB030243
View details for Web of Science ID 001521989600001
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Single-well based control and optimization of hydraulic stimulation and induced seismicity: Application to the Otaniemi geothermal project
GEOTHERMICS
2025; 132
View details for DOI 10.1016/j.geothermics.2025.103396
View details for Web of Science ID 001521703300001
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Community-Driven Code Comparisons for Simulations of Fluid-Induced Aseismic Slip
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2025; 130 (4)
View details for DOI 10.1029/2024JB030601
View details for Web of Science ID 001457914400001
- Factors Controlling Rate and Magnitudes of Injection-Induced Earthquakes 49th Workshop on Geothermal Reservoir Engineering 2024
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The break of earthquake asperities imaged by distributed acoustic sensing.
Nature
2023; 620 (7975): 800-806
Abstract
Rupture imaging of megathrust earthquakes with global seismic arrays revealed frequency-dependent rupture signatures1-4, but the role of high-frequency radiators remains unclear3-5. Similar observations of the more abundant crustal earthquakes could provide critical constraints but are rare without ultradense local arrays6,7. Here we use distributed acoustic sensing technology8,9 to image the high-frequency earthquake rupture radiators. By converting a 100-kilometre dark-fibre cable into a 10,000-channel seismic array, we image four high-frequency subevents for the 2021 Antelope Valley, California, moment-magnitude 6.0 earthquake. After comparing our results with long-period moment-release10,11 and dynamic rupture simulations, we suggest that the imaged subevents are due to the breaking of fault asperities-stronger spots or pins on the fault-that substantially modulate the overall rupture behaviour. An otherwise fading rupture propagation could be promoted by the breaking of fault asperities in a cascading sequence. This study highlights how we can use the extensive pre-existing fibre networks12 as high-frequency seismic antennas to systematically investigate the rupture process of regional moderate-sized earthquakes. Coupled with dynamic rupture modelling, it could improve our understanding of earthquake rupture dynamics.
View details for DOI 10.1038/s41586-023-06227-w
View details for PubMedID 37532935
View details for PubMedCentralID 3606976
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Stress-Based and Convolutional Forecasting of Injection-Induced Seismicity: Application to the Otaniemi Geothermal Reservoir Stimulation
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
2023; 128 (4)
View details for DOI 10.1029/2022JB024960
View details for Web of Science ID 000963763700001
https://orcid.org/0000-0002-2560-7728