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Table 3 ETAS parameters evaluated in various regions by previous studies

From: Spatio-temporal clustering of successive earthquakes as inferred from analyses of global CMT and NIED F-net catalogs

Region

\({K}_{0}\)

C (days)

\(\alpha\)

\(\gamma\)

p

\(d\)(degree2)

\(q\)

\({M}_{i}\)

\({M}_{\text{c}}\)

Japan

\(0.988\times {10}^{-4}\)

\(0.840\times {10}^{-2}\)

1.962

1.326

0.910

\(0.203\times {10}^{-2}\)

1.570

8.4

4.5

\(0.171\times {10}^{-4}\)

\(0.520\times {10}^{-2}\)

0.935

0.740

0.961

\(0.403\times {10}^{-3}\)

1.408

8.4

4.0

\(0.290\times {10}^{-3}\)

\(0.748\times {10}^{-2}\)

1.154

0.891

0.911

\(0.552\times {10}^{-2}\)

1.524

8.4

5.0

California

\(0.51\)

\(0.004\)

1.27

\(1.31\)

\(1.09\)

\(1.868\times {10}^{-5}\)

\(1.59\)

7.5

3.5

China

\(0.2285\)

\(0.2663\)

\(1.7627\)

\(0.5587\)

\(1.2363\)

\(9.179\times {10}^{-4}\)

\(2.1249\)

7.9

4.0

0.0588

0.3049

2.3378

1.7503

1.1785

\(0.519\times {10}^{-4}\)

1.7864

7.9

4.0

Italy

\(4.7\times {10}^{-2}\)

\(0.012\)

\(1.2\)

\(0.36\)

\(1.11\)

\(5.662\times {10}^{-3}\)

\(1.57\)

6.3

2.5

  1. Japan: Tohoku region, Western and Central Honshu, and all Japan from the top to the bottom (Ogata and Zhuang 2006) (Table 1, model 10)
  2. California: southern California (Seif et al. 2017) (Table 2, sets 1)
  3. China: Sichuan province (Guo et al. 2015) (Table 1, Model 3 and 4)
  4. Italy: Central Italy (Lombardi 2016) (Table 1, INGV Bulletin)