From: Geophysical assessment of migration and storage conditions of fluids in subduction zones
Subduction zone | Backarc conductor | Forearc or trench-close conductor | References | ||||
---|---|---|---|---|---|---|---|
 | Depth (km) | EC (S/m) | Distance from trench (km) | Depth (km) | EC (S/m) | Distance from trench (km) |  |
1. Chile-Bolivia (19.5°S-21°S) | 20 | 0.04.-0.10 | 220 |  | n.c. |  | Brasse et al. (2002) |
2. Chile-Bolivia (17°S-19°S) | 100 | 0.10-1 | 300 |  | n.c. |  | Brasse and Eydam (2008) |
3. Costa Rica | 30 | 0.03-0.13 | 150 | 10 | 0.10-0.20 | 65 | Worzewski et al. (2011) |
4. Mexico | 40 | 0.03-0.20 | 330 | 20 | 0.10-0.20 | 40 | Joedicke et al. (2006) |
5. Philippine Sea | 85 | 0.50 | 320 | 40 | 0.50 | 140 | Shimakawa and Honkura (1991) |
6. South Chile | 25 | 0.10-0.30 | 140 | 15 | 0.03-1 | 45 | Brasse et al.(2009) |
7. Central Argentina | 200 | 0.03-1 | 800 | 30 | 0.02 | 300 or less | Booker et al. (2004) |
8. Cascadia, British Columbia | 50 | 0.02-0.05 | 120 | 25 | 0.02 | 50 | Soyer and Unsworth (2006) |
9. Cascadia, Oregon | 80 | 0.03-1 | 120 | 25 | 0.03-1 | 80 | Evans et al. (2013) |
10. Greece | 40 | 0.002-0.006 | 170 | - | - | - | Galanopoulos et al. (2005) |
11. Mariana | 40 | 0.01 | 300 | <30? | 0.006? | 50-150? | Matsuno et al. (2012) |
12. Taiwan | 35 | 0.0590.10 | 100 | 10 | 0.05-0.12 | 30 | Bertrand et al. (2012) |
13. Kyushu, Japan | 50 | 1 | 300 | Â | n.c. | Â | Ichiki et al. (2000) |
14. Hokkaido, Japan | 40 | 0.01-0.10 | 400 | 40 | 0.01-0.10 | 100 | Ichiki et al. (2009) |
15. North Honshu, Japan | 170 | 0.15-0.30 | 260 | 15 | 0.10 | 210 | Toh et al. (2006) |
16. Central New Zealand | 35 | 0.01-0.04 | 200 | 20 | 0.10 | 150 | Wannamaker et al. (2009) |