2017 - Member of the National Academy of Sciences
1994 - Fellow of American Geophysical Union (AGU)
1994 - James B. Macelwane Medal, American Geophysical Union (AGU)
The scientist’s investigation covers issues in Seismology, Seismic wave, Aftershock, Seismogram and Induced seismicity. Fault, Episodic tremor and slip, Subduction, Tectonics and Remotely triggered earthquakes are the core of his Seismology study. His Seismic wave research incorporates elements of Seismic migration, Scattering, Seismometer and Mineralogy.
His Aftershock study integrates concerns from other disciplines, such as Sedimentary basin, S-wave and Synthetic seismogram. John E. Vidale combines subjects such as Slab, Azimuth, Rayleigh wave and Polarization with his study of Seismogram. His Induced seismicity research is multidisciplinary, relying on both 2008 California earthquake study and Aseismic slip.
His scientific interests lie mostly in Seismology, Seismogram, Aftershock, Amplitude and Fault. His study in Seismology concentrates on Subduction, Induced seismicity, Seismic wave, Episodic tremor and slip and Volcano. His Seismogram study combines topics from a wide range of disciplines, such as Magnitude, Broadband and Epicenter.
His biological study spans a wide range of topics, including Seismometer, Focal mechanism and Geodesy. His study in Amplitude is interdisciplinary in nature, drawing from both Surface wave and Mantle. In his research, Geophysics is intimately related to Mineralogy, which falls under the overarching field of Mantle.
John E. Vidale spends much of his time researching Seismology, Subduction, Mount, Seismogram and Magnitude. His work deals with themes such as Submarine pipeline and Broadband, which intersect with Seismology. John E. Vidale has included themes like Slab, Geophysics, Volcanism and Ocean bottom in his Subduction study.
His research integrates issues of Stadium and Simulation in his study of Seismogram. His Magnitude research incorporates themes from Epicenter, Earthquake casualty estimation, Deformation and Remotely triggered earthquakes. John E. Vidale usually deals with Magma and limits it to topics linked to Deformation and Amplitude.
John E. Vidale mostly deals with Seismology, Magnitude, Seismogram, Broadband and Volcano. Many of his studies on Seismology involve topics that are commonly interrelated, such as Geophysics. His biological study deals with issues like Attenuation, which deal with fields such as Subduction.
His studies in Seismogram integrate themes in fields like Wave propagation, Spectral line and Plate tectonics. His studies examine the connections between Volcano and genetics, as well as such issues in Induced seismicity, with regards to Compressibility, Magma chamber and Coda. His Episodic tremor and slip study incorporates themes from Amplitude, High amplitude and Shear stress.
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Finite-difference calculation of travel times
John Vidale.
Bulletin of the Seismological Society of America (1988)
Finite‐difference calculation of traveltimes in three dimensions
John E. Vidale.
Geophysics (1990)
Extent, duration and speed of the 2004 Sumatra–Andaman earthquake imaged by the Hi-Net array
Miaki Ishii;Peter M. Shearer;Heidi Houston;John E. Vidale.
Nature (2005)
Complex polarization analysis of particle motion
John E. Vidale.
Bulletin of the Seismological Society of America (1986)
Earth tides can trigger shallow thrust fault earthquakes
Elizabeth S. Cochran;John E. Vidale;Sachiko Tanaka.
Science (2004)
A three-dimensional simulation of seismic waves in the Santa Clara Valley, California, from a Loma Prieta aftershock
Arthur Frankel;John Vidale.
Bulletin of the Seismological Society of America (1992)
Elastic finite-difference modeling of the 1971 San Fernando, California earthquake
John E. Vidale;Donald V. Helmberger.
Bulletin of the Seismological Society of America (1988)
A survey of 71 earthquake bursts across southern California: Exploring the role of pore fluid pressure fluctuations and aseismic slip as drivers
John E. Vidale;Peter M. Shearer.
Journal of Geophysical Research (2006)
Non-volcanic tremor driven by large transient shear stresses
Justin L. Rubinstein;John E. Vidale;Joan Gomberg;Paul Bodin.
Nature (2007)
Absence of earthquake correlation with Earth tides: An indication of high preseismic fault stress rate
John E. Vidale;Duncan Carr Agnew;Malcolm J. S. Johnston;David H. Oppenheimer.
Journal of Geophysical Research (1998)
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