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Table 1 Parameters of OBS stations used in this study

From: Double seismic zone and seismicity in the mantle wedge beneath the Ogasawara Islands identified by an ocean bottom seismometer observation

Station

Latitude (N)

Longitude (E)

Depth (m)

Observation period

ΔTps-p (s)

Pcor (s)

Scor (s)

σp (s)

σs (s)

(°)

(min)

(°)

(min)

A

27

51.0

140

49.7

3270

15 Jul. to 3 Oct. 2015

0.99

0.070

− 0.319

0.281

0.462

B

27

14.3

140

48.0

1219

21 Jun. to 28 Sep. 2015

0.95

1.274

0.296

0.092

0.000

C

27

15.1

140

49.4

944

21 Jun. to 2 Oct. 2015

0.86

1.493

2.594

0.141

0.246

D

27

17.8

140

52.6

1139

21 Jun. to 13 Sep. 2015

0.84

1.387

2.167

0.078

0.301

E

27

16.0

140

55.9

1206

21 Jun. to 28 Sep. 2015

1.04

1.248

1.802

0.188

0.532

F

27

12.2

140

52.2

922

21 Jun. to 18 Sep. 2015

1.11

1.517

1.192

0.288

1.527

G

26

45.0

140

49.8

2127

15 Jul. to 9 Oct. 2015

0.93

0.448

0.233

0.209

0.462

H

27

42.1

141

36.0

4144

15 Jul. to 23 Sep. 2015

1.28

− 0.473

− 1.900

0209

0.430

I

27

15.1

141

36.1

4043

15 Jul. to 5 Oct. 2015

0.60

− 0.451

− 1.650

0.209

0.534

J

26

48.1

141

36.0

3751

15 Jul. to 10 Oct. 2015

1.13

− 0.890

− 2.064

0.204

0.391

K

27

24.0

142

39.0

2783

15 Jul. to 4 Oct. 2015

0.72

0.160

0.418

0.228

0.589

L

26

51.0

142

38.9

2756

15 Jul. to 9 Oct. 2015

0.85

− 0.165

− 0.703

0.352

0.737

X (Chichijima)

27

5.7

142

11.1

− 145

1.574

3.397

0.349

0.690

Y (Hahajima)

26

38.0

142

10.5

− 108

1.194

2.521

0.515

0.631

  1. ΔTps-p, arrival-time difference between the PS and P phases; Pcor, final station correction for the P phase; Scor, final station correction for the S phase; σp, standard deviation of the P-phase arrival time; σs, standard deviation of the S-phase arrival time