J. S. Byrnes
- ORCiD
- https://orcid.org/0000-0002-6161-399X
- OpenAlex ID
- https://openalex.org/A5031428199 (API record)
Associated Concepts [?]
- Geology
- Physics
- Biology
- Seismology
- Paleontology
- Tectonics
- Lithosphere
- Geophysics
- Subduction
- Geochemistry
- Optics
- Asthenosphere
- Quantum mechanics
- Mantle (geology)
- Geography
- Mathematics
- Engineering
- Computer science
- Attenuation
- Structural basin
- Geomorphology
- Oceanography
Authored Works
sorted by decreasing year, and then by display-name
- Spatial Variation in Anisotropic Structure and Phase Velocity of Old Oceanic Lithosphere-Asthenosphere in the Southwest Pacific
- Probing the Physical Nature of LABs and MLDs Across the Continental US from Joint Shear-velocity Inversion of Surface-wave and Receiver-function Observations
- P-wave attenuation structure of the Tonga subduction zone and implications for mantle wedge processes
- On the Edge: Evolution of the Eastern Margin of the Wyoming Craton
- New Insight into the Physical Properties of the East African Mantle from Seismic Attenuation
- A Novel Approach to Inferring Depth-dependent Seismic Anisotropy from Shear-wave Splitting in Noisy Oceanic Environments
- Variations in teleseismic body-wave attenuation along the East African Rift
- The Yellowstone Paradox - Decoupled Seismic Velocity and Attenuation in the Upper Mantle
- Surface-Wave Anisotropy of 125-Ma Oceanic Lithosphere and Asthenosphere in the Southwest Pacific
- Seismic anisotropy and lithospheric structure across the eastern margin of the Wyoming craton
- Revisiting uplift in the Laramide Orogeny: Evidence for the Localization of Deformation by Variations in Lithospheric Strength from both Seismic Velocity and Attenuation
- P-wave attenuation tomography of the Tonga-Lau mantle wedge improved by a Bayesian Monte Carlo approach and independently constrained source spectra
- Joint inversion of surface-wave and S-to-p receiver function constraints for shear-wave velocity in the Western United States: Evidence for melt in the asthenosphere
- Evaluating models for lithospheric loss and intraplate volcanism beneath the Central Appalachian Mountains
- 3D Shear-Velocity Structure across the Indo-Burman Accretionary Margin by the Joint Inversion of Surface-Wave and Scattering Constraints
Linked Co-Authors
- A. Birkey
- Dongdong Tian
- E. A. Johnson
- Emily Hopper
- Eric Kirby
- Esteban Gazel
- H. A. Ford
- J. B. Gaherty
- John C. Aragon
- Joshua Russell
- L. S. Wagner
- M. L. Anderson
- Maryjo Brounce
- Maureen D. Long
- Maximiliano Bezada
- Michael S. Steckler
- Patricia Persaud
- Robert Evans
- S. Rondenay
- S. S. Wei
- Scott D. King
- Shangxin Liu
- Z. Eilon
- Zhaopeng Zhu
Linked Collaborating Institutions
- Brown University, Rhode Island
- China University of Geosciences, Wuhan
- James Madison University, Virginia
- Lamont-Doherty Earth Observatory
- Louisiana State University
- Michigan State University
- Northern Arizona University
- Smith College, Massachusetts
- University of Bergen, Norway
- University of California, Riverside
- University of California, Santa Barbara
- University of Delaware
- University of Michigan
- University of Minnesota, Twin Cities
- University of Missouri, Columbia
- University of North Carolina, Chapel Hill
- University of Oregon
- Virginia Polytechnic Institute and State University
- Virginia Tech, Department of Geosciences
- Woods Hole Oceanographic Institute, Massachusetts
- Wuhan University, China
- Yale University, Connecticut
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