Bibliography

[1]

Weatherill, G. A. (2014) OpenQuake Hazard Modeller’s Toolkit - User Guide. Global Earthquake Model (GEM). Technical Report.

[2]

Wessel, P., Luis, J. F., Uieda, L. A., Scharroo, R., Wobbe, F., Smith, W. H., & Tian, D. (2019). The generic mapping tools version 6. Geochemistry, Geophysics, Geosystems, 20(11), 5556-5564. Doi: https://doi.org/10.1029/2019GC008515

[3]

Gardner, J. and Knopoff, L. (1974). Is the sequence of earthquakes in Southern California, with aftershocks removed, Poissonian? Bull. seismol. soc. am, 64(5):1363–1367. Doi: https://doi.org/10.1785/BSSA0640051363

[4]

Uhrhammer, R. (1986). Characteristics of northern and southern California seismicity: Earthquake notes, v. 57.

[5]

Grünthal, G. (1985). The updated earthquake catalogue for the German Democratic Republic and adjacent areas: statistical data characteristics and conclusions for hazard assessment. In 3rd International Symposium on the Analysis of Seismicity and on Seismic Risk (Prague 1985).

[6]

Pagani, M., Bayliss, K., Brooks, C., Johnson, K., Styron, R., Villani, M., & Rong, Y. (2026). The OpenQuake Model Building Toolkit: A suite of tools for building components of a seismic hazard model. Seismica, 5(1). Doi: https://doi.org/10.26443/seismica.v5i1.1677

[7]

Stepp, J. 1. (1972, October). Analysis of completeness of the earthquake sample in the Puget Sound area and its effect on statistical estimates of earthquake hazard. In Proc. of the 1st Int. Conf. on Microzonazion, Seattle (Vol. 2, pp. 897-910).

[8]

Johnson, K., Bayliss, K., Pagani, M., Styron R. (2026). Jointly estimating completeness and MFD parameters for PSHA. In preparation process.

[9]

Weatherill, G. A., Pagani, M., & Garcia, J. (2016). Exploring earthquake databases for the creation of magnitude-homogeneous catalogues: tools for application on a regional and global scale. Geophysical Journal International, 206(3), 1652-1676. Doi: https://doi.org/10.1093/gji/ggw232

[10]

Gutenberg, B., & Richter, C. F. (1944). Frequency of earthquakes in California.

[11]

Aki, K. (1965). Maximum likelihood estimate of b in the formula log N= a− bM and its confidence limits. Bull. Earthquake Res. Inst. Univ. Tokyo, 43, 237-239.

[12]

Bender, B. (1983). Maximum likelihood estimation of b values for magnitude grouped data. Bulletin of the Seismological Society of America, 73(3), 831-851.

[13]

Utsu, T. (1965). A method for determining the value of b in a formula log n= a= bM showing the magnitude frequency relation for earthquakes. Geophys. Bull. Hokkaido Univ., 13, 99-103.

[14]

Weichert, D. H. (1980). Estimation of the earthquake recurrence parameters for unequal observation periods for different magnitudes. Bulletin of the seismological society of America, 70(4), 1337-1346.

[15]

McGuire, R. K. (2004). Seismic hazard and risk analysis. (No Title).

[16]

Musson, R. M. W. (1999). Probabilistic seismic hazard maps for the Balkan region, Annali di Geofisc. 42, no. 6, 1109–1124.

[17]

Pagani, M., Monelli, D., Weatherill, G., Danciu, L., Crowley, H., Silva, V., … & Vigano, D. (2014). OpenQuake engine: An open hazard (and risk) software for the global earthquake model. Seismological Research Letters, 85(3), 692-702. Doi: https://doi.org/10.1785/0220130087