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Table 2 Location, highest seismic wave attenuation values, and wave velocity ratios of mantle wedge seismic anomalies

From: Geophysical assessment of migration and storage conditions of fluids in subduction zones

Subduction zone

Backarc anomaly

Forearc or trench-close anomaly

References

Depth (km)

Attenuation

Vp/Vs

Depth (km)

Attenuation

Vp/Vs

f range (Hz)

P wave

S wave

f range (Hz)

P wave

S wave

1. Mariana

50-75

0.10-9.5

93-132

63-76

-

25-50

0.10-9.5

63-93

42-56

-

Pozgay et al. (2009); Wiens et al. (2006)

2. Tonga-Lau

50-70

0.10-3.5

47-60

15-30

1.70

<20

-

-

-

?

Wiens et al. (2008)

3. NE Japan

30-100

1.0-8.0

-

70-120

1.85

<25

-

-

-

1.85

Zhao et al. (2007); Takanami et al. (2000)

4. Honshu, Japan

80-100

1.0-20?

150

-

-

30-60

1.0-20?

150-180

-

-

Tsumura et al. (2000)

5. Taiwan

60-80

0.15-8.0

100

-

-

-

-

-

-

-

Ko et al. (2012)

6. Central Java, Indonesia

70-120

1.0-20

100

-

-

30-50

1.0-20

<100

-

-

Bohm et al. (2013)

7. North New Zealand

40-100

2.0-40

50-120

-

-

<25

2.0-40

120-200

-

-

Eberhart-Phillips et al. (2008)

8. Mexico

40 and 80-120

1.0-30

130

-

-

20

1.0-30

160

-

-

Chen and Clayton (2009)

9. Nicaragua-Costa Rica

40-75

0.50-7.0

90-140

120-160

1.90

<50

0.50-7.0

125-200

125-200

1.90

Rychert et al. (2008); Dinc et al. (2011)

10. Central Andes −21, −22.1°S

50-150

1.0-7.0; 1.0-30

117

-

1.83

<60

1.0-7.0; 1.0-30

117

-

-

Myers et al. (1998); Schurr et al. (2003)

11. Central Andes −24.2°S

150-200

1.0-7.0; 1.0-30

105

-

-

30-100

1.0-7.0; 1.0-30

95

-

-

Schurr et al. (2003)

12. Alaska

80-100

1-19; 0.3-9

537

283

-

50-60

1-19; 0.3-9

<537

<283

-

Stachnik et al. (2004)