Description Usage Arguments Details Value References See Also
Transforms earthquake occurrence times following the Ogata (1988) method based on the integration of the
induced seismicity model of model_rate.val(), to then be used as input in stat.KS_uniform().
1 2 |
data |
a list containing all the necessary point data:
|
theta |
the list of fitted model parameters:
|
See examples of induced seismicity applications in Mignan et al. (2017, 2019) and Broccardo et al. (2017).
the transformed time vector
Broccardo M., Mignan A., Wiemer S., Stojadinovic B., Giardini D. (2017), Hierarchical Bayesian Modeling of FluidāInduced Seismicity. Geophysical Research Letters, 44 (22), 11,357-11,367, doi: 10.1002/2017GL075251
Mignan A., Broccardo M., Wiemer S., Giardini D. (2017), Induced seismicity closed-form traffic light system for actuarial decision-making during deep fluid injections. Sci. Rep., 7, 13607, doi: 10.1038/s41598-017-13585-9
Mignan A., Broccardo M., Wiemer S., Giardini D. (2019), Autonomous Decision-Making Against Induced Seismicity in Deep Fluid Injections. In: Ferrari A., Laloui L. (eds), Energy Geotechnics, SEG 2018, Springer Series in Geomechanics and Geoengineering, 369-376, doi: 10.1007/978-3-319-99670-7_46
Ogata Y. (1988), Statistical Models for Earthquake Occurrences and Residual Analysis for Point Processes. J. Am. Stat. Assoc., 83 (401), 9-27
stat.KS_uniform, model_rate.val
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