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@@ -4,6 +4,10 @@ Gridded (and smoothed) seismicity sources are modeled as uniformely distributed
All sub-catalogs were declusterd using nearest-neighbor (`nn`) and Reasenberg (1985; `r85`) algorithms prior to smoothing earthquake rates using a single, adaptive kernel approach.
## Gridded rates
Rates of M = 5.0 earthquakes, `n(m=5)`, given in Table 1 of Petersen et al. (2014) are the Gutenberg-Richter rate of magnitude 5.0 earthquakes derived from the total gridded a-value multiplied by a scale factor for the catalog time period and declustering method. These `n(m=5)` rates are converted to a-values (rate of earthquakes of magnitude 0.0) using ![formula](https://render.githubusercontent.com/render/math?math=n(m)\=10^{a-bm}) for use in grid-source `rate-tree.json` files. Spatial PDFs were created by normalizing the 1960-2019 catalog a-grid file.
## Grid source rupture set names and IDs
Region | Depth | PDF¹ | ID
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