Deaggregation of PSHA by distance, magnitude, epsilon, and by distance/magnitude.
3. DSHA calculations for up to 20 fractiles.
4. Effectively unlimited number of seismic sources. Sources can be selected by distance from the site, by region, or individually.
5. Plots of recurrence rate vs. magnitude for each seismic source.
6. Effectively unlimited number of ground motion equations.
7. Ability
to use different ground motion equations for different seismic sources, with custom weights applied to any combination of seismic source and attenuation equation.
8. Uniform hazard spectra (UHS) can be generated for any return period without having to rerun the PSHA.
9. Results in tabular and graphical form.
10. Plots of probabilistic hazard for each spectral frequency, and UHS for up to 100 return periods. Plots of mean and fractile deterministic spectra.
11. Plots can be customized and saved as templates.
12. Batch processing capability for multiple assumptions and sites.
13. Multi-site gridded and/or selected sites) hazard mapping available (additional cost).
14. USGS faults, area seismic sources, and background seismicity data for all 50 states and Puerto Rico / Virgin Islands (for user's licensing the US and Canada region) currently 1996, 2002, and 2008 models are available.
15. Geological Survey of Canada fault, background, and area seismic sources for Canada (for user's licensing the US and Canada region).
16. Proprietary seismic source databases are available for Mexico, Central America, the Caribbean, South America, Europe, the Eastern Mediterranean, the Middle East, Australia, South Asia, South East Asia, Indonesia, Philippines, China, Japan, Siberia and Central Asia (additional cost).
17. Multiple magnitude recurrence models: exponential, characteristic, truncated normal and USGS.
18. Faults can be modeled with an unlimited number of weighted magnitude recurrence models.
19. Fault geometry is specified and analyzed in 3-D. Different dip angles can be used for the upper and lower portion of the fault, and blind faults can be specified.
20. Subduction interface zones can be modeled using an upper and lower trace specified in 3-D.
21. Subduction slab zones can be modeled using an upper and lower trace specified in 3-D.
22. Ground motion equations using 85 mathematical forms and 241 equations that span the Western US, the Central and Eastern US, Japan, Europe, the Middle East, Australia, New Zealand and other parts of the world.
23. Optional truncation of the residual distribution using 5 methods.
24. Ground motion equation driver to explore and test ground motion equations. Charts and tables can be created using any parameter as the independent variable (for example magnitude, distance, or spectral period). An unlimited number of levels for most other parameters for any number of ground motion equations.
25. All database types can be extended with user-defined data.
26. Analyses can be recalculated with updated seismic source and attenuation equation information without having to update the analysis definition.
27. Seismic hazard analysis can use spectral acceleration at 5% damping, maximum rotated component of spectral acceleration at 5% damping, peak ground velocity, peak ground displacement, Arias intensity, or MMI as the intensity measure for ground motion.
