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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Table 4 Homogeneity of the study region shown through estimated b-values for 21 city-circle sub-catalogs

From: Nowcasting earthquakes in Sulawesi Island, Indonesia

Spatial region

Total number of events \(\left( {M \ge 4.5} \right)\)

Number of large \(\left( {M \ge 6.5} \right)\) earthquakes

Maximum magnitude

Estimated b-value

Coefficient of Determination (R2) in G–R frequency–magnitude linear regression model

Palu

1182

06

7.9

0.9870

0.9869

Makassar

144

01

6.9

1.0868

0.9415

Manado

5281

21

7.5

1.2922

0.9936

Kendari

322

03

7.5

0.8924

0.9701

Bitung

5540

22

7.5

1.2778

0.9927

Gorontalo

2266

09

7.9

1.0470

0.9826

Palopo

626

03

7.0

1.1387

0.9933

Bau-Bau

216

02

7.5

0.8744

0.9383

Luwuk

2419

08

7.7

1.0910

0.9780

Toli-toli

1578

11

7.9

1.0114

0.9900

Pare-pare

333

01

6.9

1.2598

0.9564

Poso

1503

09

7.9

1.0257

0.9887

Bone

225

02

6.9

1.1066

0.9814

Kolaka

426

03

7.5

0.9636

0.9704

Buton

200

02

7.5

0.8611

0.9399

Watampone

292

02

6.9

1.1631

0.9844

Polewali

461

02

6.9

1.1916

0.9946

Donggala

1197

07

7.9

0.9948

0.9821

Taliabu

2056

08

7.7

1.0615

0.9777

Mamuju

580

03

7.4

1.0509

0.9897

Morowali

973

04

7.6

0.9880

0.9665