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 | - | |
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 | |
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 | |
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 | - | - | |
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) |