Dear OpenQuake Users,
I hope this message finds you well.
I am currently working on a seismic hazard analysis using a subduction interface source model with the following parameters:
a-value: 4.271
b-value: 0.82
mmin: 6.5
mmax: 8.5
bin width: 0.1
In my study, I applied the parameters in two ways (method):
Using the Truncated Gutenberg-Richter MFD, inputting the values directly into OpenQuake.
Using the Incremental MFD, where I calculated the occurrence rates for each magnitude bin using the formula N=10^(a-b*M), from mmin to mmax with a step size of 0.1.
Unexpectedly, the seismic hazard results from these two methods differ significantly.
However, when I validated the same parameters using nshmp-haz-fortran (from USGS), the results were consistent with method 2 (Incremental MFD).
Is there something I might be missing in the use of the Truncated GR implementation in OpenQuake? Are there specific assumptions or processing steps applied internally that could lead to this difference?
Any clarification or guidance would be greatly appreciated.
Best regards,
Fatahillah Surya Yudha
Sebelas Maret University
The formula you are using for the GR is not correct. See https://github.com/gem/oq-engine/blob/master/openquake/hazardlib/mfd/truncated_gr.py#L102
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Dear Fatahillah, if I recall correctly, the input in the nshmp-haz Fortran code defines the GR in incremental terms.
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