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Unmixing the Gutenberg-Richter Law
Session: Earthquake Source Parameters: Theory, Observations and Interpretations [Poster] Type:Poster Date:4/30/2020 Time: 08:00 AM Room: Ballroom Description:
Magnitudes of earthquakes are typically observed to be exponentially distributed, following the Gutenberg-Richter (G-R) Law. Much attention has been paid to the G-R b-value, and there are well-established trends seen in the estimated b-value with respect to earthquake faulting mechanism and depth, and more recently, distance from a recent mainshock (van der Elst and Shaw, 2015; Gulia et al., 2018).
However, G-R distributions with different b-values do not sum to yield a G-R curve. Given the observation that earthquakes within large volumes follow the G-R Law so robustly, observed variations in mean magnitude must be different than simple variations in b-value. Similarly, while aftershock rates on the whole are consistent with Bath’s Law and the rates of the largest aftershocks, near-field aftershocks are deficient at the largest magnitudes. To reconcile these seemingly disparate observations, we investigate the parametric form of spatio-temporal variations in the magnitude distribution and how these could be incorporated coherently into earthquake forecasting approaches.
Presenting Author: Morgan Page
Authors
Morgan Page
Presenting Author Corresponding Author
mpage@usgs.gov
U.S. Geological Survey, Pasadena, California, United States
Presenting Author
Corresponding Author
Karen Felzer
kfelzer@usgs.gov
U.S. Geological Survey, Pasadena, California, United States