Huang, H.‐H., F.‐C. Lin, B. Schmandt, J. Farrell, R. B. Smith, and V. Tsai (2015). The Yellowstone magmatic
system from the mantle plume to the upper crust, Science, 348, doi:10.1126/science.aaa5648.
Yellowstone
Tomography from 26 years of seismicity revealing that the spatial extent of the Yellowstone crustal magma reservoir extends well beyond the Yellowstone caldera
Farrell, J., R. B. Smith, S. Husen, and T. Diehl, 2014, Tomography from 26 years of seismicity revealing that the spatial extent of the Yellowstone crustal magma reservoir extends well beyond the Yellowstone caldera, Geophys. Res. Lett., 41, doi:10.1002/2014GL059588.
A fluid-driven earthquake swarm on the margin of the Yellowstone caldera
Shelly, D. R., D. P. Hill, F. Massin, J. Farrell, R. B. Smith, T. Taira, 2014, A fluid-driven earthquake swarm on the margin of the Yellowstone caldera, J. Geophys. Res., doi:10.1029/2013JB010481.
Seismic energy from waterfalls in Yellowstone National Park
Workman, E. J., Koper, K. D., Burlacu, R., Lin. F‐C. (2014). Seismic energy from waterfalls in Yellowstone National Park, Abstract S41A‐4442.
Dynamics of the Yellowstone volcanic system using 4D seismic imaging
Farrell, J., R. B. Smith, and F.‐C. Lin (2014). Dynamics of the Yellowstone volcanic system using 4D seismic imaging, Seism. Res. Lett. 85, 479.
The Mw 4.8 Norris Geyser Basin earthquake of 30 March, 2014 and its relationship to crustal deformation and seismic activity of the Yellowstone volcanic system
Farrell, J., D. R. Shelly, R. B. Smith, C. M. Puskas, W. L. Chang (2014). The Mw 4.8 Norris Geyser Basin earthquake of 30 March, 2014 and its relationship to crustal deformation and seismic activity of the Yellowstone volcanic system, Abstract S11E‐4400.
Tomography from 26 years of seismicity revealing that the spatial extent of the Yellowstone crustal magma reservoir extends well beyond the Yellowstone caldera
Farrell, J., R. B. Smith, S. Husen, and T. Diehl (2014). Tomography from 26 years of seismicity revealing that the spatial extent of the Yellowstone crustal magma reservoir extends well beyond the Yellowstone caldera, Geophys. Res. Lett. 41, 3068‐3073, doi:10.1002/2014GL059588.
Effects of lithospheric viscoelastic relaxation on the contemporary deformation following the 1959 Mw 7.3 Hebgen Lake, Montana, earthquake and other areas of the intermountain seismic belt
Chang, W.-L., R. B. Smith, and C. Puskas, 2013, Effects of lithospheric viscoelastic relaxation on the contemporary deformation following the 1959 Mw 7.3 Hebgen Lake, Montana, earthquake and other areas of the intermountain seismic belt, Geochem. Geophys. Geosyst., doi:10.1029/2012GC004424.
The Yellowstone magma reservoir is 50% larger than previously imaged
Farrell, J., R. B. Smith, S. Husen (2013). The Yellowstone magma reservoir is 50% larger than previously imaged, Abstract V41B‐2778.
Crustal velocity structure and seismicity of the Yellowstone volcanic system from automated waveform analysis of body waves
Farrell J., J. Husen, and R. B. Smith (2013). Crustal velocity structure and seismicity of the Yellowstone volcanic system from automated waveform analysis of body waves, 1984‐2011, Seism. Res. Lett. 84, 297.