Declustering Retained Event Fraction Summary
Fraction of the catalog retained as Poissonian background after declustering.
Description
Fraction of the catalog retained as Poissonian background after declustering.
Declustering Retained Event Fraction Summary is a focused tool for the following task. Fraction of the catalog retained as Poissonian background after declustering. It reports f, Band from the values you provide rather than inventing measurements, coefficients, or professional judgment that are not part of the input.
When to use Declustering Retained Event Fraction Summary
Use this seismology calculation to reproduce a stated convention, screen observations, or compare scenarios whose units, coordinate conventions, catalog selection, and model assumptions are known.
- n_keep
- Required integer. Background events kept.
- n_drop
- Required integer. Clustered events removed.
The cited overview of Seismology supplies background for the terminology and domain context used by this tool.1
How Declustering Retained Event Fraction Summary works
Fraction of the catalog retained as Poissonian background after declustering. Inputs are interpreted exactly in the displayed units and the calculation returns the following fields without presentation rounding.
- f
- Returned number. Retained share of the original catalog.
- Band
- Returned string. Typical retention band.
Limitations and assumptions
- Earth structure, source geometry, path effects, site response, instrument response, catalog completeness, uncertainty, and the fitted range can dominate the accuracy of simplified seismic calculations.
- n_keep must be at least 0.
- n_drop must be at least 0.
- Use finite inputs in the displayed units, preserve source measurements and assumptions, and independently verify consequential decisions.
Alternative or Complementary approaches
For analysis or hazard decisions, retain uncertainty and provenance and compare the result with waveform processing, calibrated regional models, and guidance from qualified seismologists or the responsible agency.
References
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Seismology — Wikipedia contributors
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