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Table 1 List of tsunami stations used in this study

From: Fault model of the 2012 doublet earthquake, near the up-dip end of the 2011 Tohoku-Oki earthquake, based on a near-field tsunami: implications for intraplate stress state

Station

Latitude[°N]

Longitude[°E]

Depth [m]

Epicentral distance [km]

Inversion time window [s]

Instrument

Sampling rate of original data [s]a

GFK

37.5812

142.7647

2245

140

0– 200

TPG

1

P01

38.3331

142.4167

1038

180

300–1500

TPG

1

P02

38.5006

142.5035

1109

180

300–1500

TPG

1

P03

38.1834

142.3996

1056

170

300–1500

TPG

1

P04

38.3163

142.5657

1265

160

300–1500

TPG

1

P05

38.3000

142.7004

1412

150

300–1500

TPG

1

P06

38.6338

142.5833

1269

180

300–1500

TPG

1

P07

38.0000

142.4486

1064

170

300–1500

TPG

1

P08

38.2833

142.8329

1424

140

150–1350

TPG

1

P10

38.2500

143.1666

2066

110

0–1200

TPG

1

P12

37.8206

142.8996

1635

130

0–1200

TPG

1

KAMN

38.8862

143.3639

2360

150

0–1200

TPG

1

KAMS

38.6347

143.2621

2246

130

0–1200

TPG

1

MYGI

38.0832

142.9166

1697

130

0–1200

TPG

1

G09

38.4782

143.7922

5500

90

Not used

TPG

1

GJT3

38.2948

143.4811

3260

90

Not used

TPG

1

JFAST

37.9336

143.9154

6799

40

Not used

TPG

1

TJT1

38.2080

143.7904

5744

60

Not used

TPG

1

801

38.2325

141.6836

144

240

Not used

GPS Buoy

1

802

39.2586

142.0969

204

250

Not used

GPS Buoy

1

803

38.8578

141.8944

160

240

Not used

GPS Buoy

1

804

39.6272

142.1867

200

320

Not used

GPS Buoy

1

805

40.6333

141.7500

87

380

Not used

GPS Buoy

1

806

36.9714

141.1856

137

250

Not used

GPS Buoy

1

807

40.1167

142.0667

125

320

Not used

GPS Buoy

1

KPG1

41.7040

144.4375

2218

450

1200–2400

KPG

1

KPG2

42.2365

144.8454

2210

510

1500–2700

KPG

1

KCTD

41.6675

144.3409

2540

440

1200–2400

KPG

10

JP1

40.3777

146.1681

5125

330

1050–2250

DART

15

JP2

39.2849

145.7845

5183

210

750–1950

DART

15

  1. aObserved records were resampled to 15 s in the inversion for the tsunami source model