CK
Member Since 2018
Chun-Yu Ke
Assistant Professor, National Taiwan University
AGU Research
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Complex laboratory earthquake sequences and direct observations of creep fronts illuminate the mechanics of delayed earthquake triggering
PHYSICAL PROPERTIES OF EARTH MATERIALS (PPEM): DEFORMATION ACROSS SCALES I ORAL
mineral and rock physics | 11 december 2023
Sara B. Cebry, Chun-Yu Ke, Srisharan Shreedharan, ...
Natural earthquakes occur in clusters or sequences that arise from complex triggering mechanisms, but direct measurement of the mechanisms responsible...
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Understanding elastic wave propagation across rough interfaces in stressed fractured rock through coupled in-situ synchrotron X‑ray imaging and ultrasound
PHYSICAL PROPERTIES OF EARTH MATERIALS (PPEM): DEFORMATION ACROSS SCALES II ORAL
mineral and rock physics | 11 december 2023
Evan Bozek, Prabhav Borate, Michail Skiadopoulos, ...
Remote seismic imaging of subsurface fractured rock is essential in applications such as geothermal energy recovery, as well as unconventional reservo...
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Illuminating Fundamental Processes Governing Evolution of Fault Zone Permeability and Elastodynamic Properties due to Dynamic Stressing using a Coupled X-Ray Imaging and Active Ultrasonic Experiment
HYDROMECHANICAL PROCESSES IN ENERGY GEOTECHNICS I ONLINE POSTER DISCUSSION
hydrology | 16 december 2022
Chun-Yu Ke, Prabhav Borate, Chris Marone, Derek El...
Permeability changes in crustal materials following dynamic stress perturbation is a well-characterized but poorly understood observation in energy pr...
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An Integrated Experimental and Multi-Physics Numerical Study on the Interplay Between Hydraulic and Elastic Properties of Fractured Rock Interfaces Under Stress Perturbations
PHYSICS OF FLUIDS IN UNCONVENTIONAL RESERVOIR ROCKS III ORAL
mineral and rock physics | 16 december 2022
Chun-Yu Ke, Clay Wood, Andrew P. Rathbun, Chris Ma...
The response of hydraulic properties to stress perturbations across fractured rock interfaces is of significant interest in energy production, waste s...
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Decoupling the poromechanics of particle remobilization and interface stiffness of dynamically stressed tensile fractured rock
FROM ROCK PHYSICS TO EARTHQUAKE MECHANICS: INSIGHTS FROM THE FIELD, THE LAB, AND IN BETWEEN II POSTER
mineral and rock physics | 15 december 2022
Clay Wood, Chun-Yu Ke, Jacques Riviere, Derek Elsw...
Understanding the poromechanical response of fractured rock is necessary for applications ranging from hydraulic stimulation of the subsurface to tele...
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The Role of Background Stress State in Fluid‐Induced Aseismic Slip and Dynamic Rupture on a 3‐m Laboratory Fault
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
24 august 2022
Sara B. Cebry, Chun-Yu Ke, Gregory Mclaskey
Fluid injection stimulates seismicity far from active tectonic regions. However, the details of how fluids modify on‐fault stresses and initi...
Role of background stress state in fluid induced aseismic slip and dynamic rupture on a 3 meter laboratory fault
INDUCED AND TRIGGERED EARTHQUAKES: THEORY, OBSERVATIONS, IMPACT II ORAL
seismology | 16 december 2021
Sara B. Cebry, Chun-Yu Ke, Gregory Mclaskey
Fluid injection for oil and gas operations, CO2 sequestration, or enhanced geothermal systems (EGS) stimulates seismicity far from active tectonic reg...
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Creep fronts and asperity interactions in laboratory earthquake sequences illuminate delayed earthquake triggering
PRE-, CO-, AND POST-RUPTURE PROCESSES ACROSS MULTIPLE SCALES II ORAL
mineral and rock physics | 15 december 2021
Gregory Mclaskey, Sara B. Cebry, Chun-Yu Ke, Srish...
Earthquakes occur in clusters or sequences that imply heterogeneous fault properties and complex triggering mechanisms. We have developed a laboratory...
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