STRESS TRANSFER IN EARTHQUAKES, HAZARD ESTIMATION AND ENSEMBLE FORECASTING: INFERENCES FROM NUMERICAL SIMULATIONS

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dc.contributor.author Rundle J.B.
dc.contributor.author Rundle P.B.
dc.contributor.author Morein G.
dc.contributor.author Donnellan A.
dc.contributor.author Li P.
dc.contributor.author Klein W.
dc.contributor.author Turcotte D.L.
dc.contributor.author Grant L.
dc.date.accessioned 2025-03-15T04:58:33Z
dc.date.available 2025-03-15T04:58:33Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=31310897
dc.identifier.citation Tectonophysics, 2006, 413, 1-2, 109-125
dc.identifier.issn 0040-1951
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48466
dc.description.abstract Observations indicate that earthquake faults occur in topologically complex, multi-scale networks driven by plate tectonic forces. We present realistic numerical simulations, involving data-mining, pattern recognition, theoretical analyses and ensemble forecasting techniques, to understand how the observable space-time earthquake patterns are related to the fundamentally inaccessible and unobservable dynamics. Numerical simulations can also help us to understand how the different scales involved in earthquake physics interact and influence the resulting dynamics. Our simulations indicate that elastic interactions (stress transfer) combined with the nonlinearity in the frictional failure threshold law lead to the self-organization of the statistical dynamics, producing 1) statistical distributions for magnitudes and frequencies of earthquakes that have characteristics similar to those possessed by the Gutenberg-Richter magnitude-frequency distributions observed in nature; and 2) clear examples of stress transfer among fault activity described by stress shadows, in which an earthquake on one group of faults reduces the Coulomb failure stress on other faults, thereby delaying activity on those faults. In this paper, we describe the current state of modeling and simulation efforts for Virtual California, a model for all the major active strike slip faults in California. Noting that the Working Group on California Earthquake Probabilities (WGCEP) uses statistical distributions to produce earthquake forecast probabilities, we demonstrate that Virtual California provides a powerful tool for testing the applicability and reliability of the WGCEP statistical methods. Furthermore, we show how the simulations can be used to develop statistical earthquake forecasting techniques that are complementary to the methods used by the WGCEP, but improve upon those methods in a number of important ways. In doing so, we distinguish between the "official" forecasts of the WGCEP, and the "research-quality" forecasts that we discuss here. Finally, we provide a brief discussion of future problems and issues related to the development of ensemble earthquake hazard estimation and forecasting techniques. © Elsevier B.V. All rights reserved.
dc.subject EARTHQUAKES
dc.subject NUMERICAL SIMULATIONS
dc.subject VIRTUAL CALIFORNIA
dc.title STRESS TRANSFER IN EARTHQUAKES, HAZARD ESTIMATION AND ENSEMBLE FORECASTING: INFERENCES FROM NUMERICAL SIMULATIONS
dc.type Статья
dc.identifier.doi 10.1016/j.tecto.2005.10.031


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