2017 - Fellow of the American Association for the Advancement of Science (AAAS)
2008 - Fellow of American Geophysical Union (AGU)
2004 - Fellow of American Physical Society (APS) Citation For innovative research and fundamental discoveries in the physics of driven nonlinear threshold systems, especially earthquake fault systems, revealed by computational simulations coupled with analysis using statistical physics
John B. Rundle spends much of his time researching Seismology, Statistical physics, Slip, Induced seismicity and Scaling. John B. Rundle frequently studies issues relating to Crust and Seismology. His studies deal with areas such as Probability and statistics, Stochastic process, Critical phenomena and Measure as well as Statistical physics.
His Slip research includes elements of Active fault, Lithosphere, Asthenosphere, Shear and Mathematical model. His research integrates issues of Poisson distribution, Earthquake risk, Earthquake prediction and Probabilistic logic in his study of Induced seismicity. His Scaling research is multidisciplinary, incorporating perspectives in Magnitude, Large earthquakes and Self-organization.
His scientific interests lie mostly in Seismology, Induced seismicity, Statistical physics, Scaling and Aftershock. The Seismology study combines topics in areas such as Slip and Magnitude. His research in Induced seismicity intersects with topics in Earthquake prediction, Large earthquakes, Informatics and Meteorology.
His Statistical physics study frequently intersects with other fields, such as Nucleation. Scaling is closely attributed to Cellular automaton in his study. John B. Rundle studies Foreshock, a branch of Aftershock.
His primary areas of study are Seismology, Induced seismicity, Aftershock, Scaling and Magnitude. He has researched Seismology in several fields, including Quake, Nowcasting and Interferometric synthetic aperture radar. His Induced seismicity research is multidisciplinary, relying on both Large earthquakes, Completeness, Probabilistic forecasting, Weibull distribution and Eigenvalues and eigenvectors.
The study incorporates disciplines such as Geothermal gradient, Hazard analysis and Cumulative distribution function in addition to Aftershock. His work carried out in the field of Scaling brings together such families of science as Statistical physics, Seismic hazard and Cellular automaton. His work deals with themes such as Range, Statistical model, Statistics and Series, which intersect with Magnitude.
John B. Rundle focuses on Seismology, Induced seismicity, Aftershock, Scaling and Magnitude. The various areas that John B. Rundle examines in his Seismology study include Slip and Probabilistic forecasting. John B. Rundle interconnects Space, Measure, Eigenvalues and eigenvectors and Nowcasting in the investigation of issues within Induced seismicity.
The concepts of his Aftershock study are interwoven with issues in Hazard analysis and Cumulative distribution function. His Scaling study incorporates themes from Statistical physics, Limit and Cellular automaton. Within one scientific family, John B. Rundle focuses on topics pertaining to Weibull distribution under Magnitude, and may sometimes address concerns connected to Landslide, Correlation function, Electricity grid and Event.
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Statistical physics approach to understanding the multiscale dynamics of earthquake fault systems
John B. Rundle;Donald L. Turcotte;Robert Shcherbakov;William Klein;William Klein.
Reviews of Geophysics (2003)
The growth of geological structures by repeated earthquakes, 1, conceptual framework
Geoffrey C. P. King;Ross S. Stein;John B. Rundle.
Journal of Geophysical Research (1988)
The Growth of Geological Structures by Repeated Earthquakes 2. Field Examples of Continental Dip‐Slip Faults
Ross S. Stein;Geoffrey C. P. King;John B. Rundle.
Journal of Geophysical Research (1988)
A viscoelastic coupling model for the cyclic deformation due to periodically repeated Earthquakes at subduction zones
Wayne Thatcher;John B. Rundle.
Journal of Geophysical Research (1984)
A simplified spring-block model of earthquakes
Stephen R. Brown;Christopher H. Scholz;John B. Rundle.
Geophysical Research Letters (1991)
Self-organization in leaky threshold systems: The influence of near-mean field dynamics and its implications for earthquakes, neurobiology, and forecasting
J. B. Rundle;K. F. Tiampo;W. Klein;J. S. Sá Martins.
Proceedings of the National Academy of Sciences of the United States of America (2002)
A model for the earthquake cycle in underthrust zones
Wayne Thatcher;John B. Rundle.
Journal of Geophysical Research (1979)
Derivation of the complete Gutenberg‐Richter magnitude‐frequency relation using the principle of scale invariance
John B. Rundle.
Journal of Geophysical Research (1989)
A generalized Omori's law for earthquake aftershock decay
Robert Shcherbakov;Donald L. Turcotte;John B. Rundle.
Geophysical Research Letters (2004)
Geocomplexity and the Physics of Earthquakes
John Rundle;William Klein;Donald Lawson Turcotte.
GMS (2000)
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