Research Article
Structural Controls on Shallow Cenozoic Fluid Flow in the Otago Schist, New Zealand
Table 5
Calculated δ13CVPDB‰ and δ18OSMOW‰ stable isotope ratios of hydrothermal carbonate phases from Akatore Creek and Bruce Rocks.
| | Sample | δ13CVPDB (‰) | δ18OSMOW (‰) |
| | AK14-A | -8.05 | 20.24 | | AK14-B | -9.15 | 20.13 | | AK15-A | -6.78 | 24.50 | | AK15-B | -6.34 | 23.95 | | AK16-A | -8.63 | 24.32 | | AK16-B | -8.65 | 24.54 | | AK17-A | -10.68 | 24.21 | | AK17-B | -10.28 | 23.93 | | AK18-A | -6.92 | 25.11 | | AK18-B | -7.20 | 25.11 | | AK21-A | -8.86 | 24.85 | | AK21-B | -8.80 | 24.77 | | AK23-A | -9.06 | 24.87 | | AK23-B | -9.32 | 24.85 | | AK24-A | -5.18 | 20.74 | | AK24-B | -5.43 | 21.04 | | AK26A-A | -6.25 | 25.09 | | AK26A-B | -6.45 | 25.20 | | AK26B-A | -3.70 | 22.61 | | AK26B-B | -4.69 | 22.89 | | AK26C-A | -3.23 | 20.60 | | AK26C-B | -3.40 | 20.85 | | AK28-A | -2.96 | 24.39 | | AK28-B | -3.06 | 24.58 | | AK30-A | -6.51 | 24.73 | | AK30-B | -6.55 | 24.56 | | AK31-A | 0.46 | 25.56 | | AK31-B | 0.53 | 25.43 | | AK33-A | -3.05 | 23.97 | | AK33-B | -2.68 | 23.21 | | AK34-A | 2.18 | 24.57 | | AK34-B | 2.47 | 24.47 | | AK37-A | -6.36 | 25.06 | | AK37-B | -6.45 | 24.63 | | AK38-A | -4.27 | 23.10 | | AK38-B | -4.63 | 23.54 | | AK39-A | 0.04 | 24.23 | | AK39-B | 0.79 | 24.09 | | AK40-A | -4.62 | 18.88 | | AK40-B | -4.20 | 18.68 | | AK41-A | -16.32 | 25.31 | | AK41-B | -15.71 | 25.18 | | AK42-A | -15.23 | 24.17 | | AK42-B | -15.19 | 24.27 | | AK43A-A | -5.19 | 25.35 | | AK43A-B | -5.53 | 25.28 | | AK43B-A | -8.25 | 24.60 | | AK43B-B | -8.69 | 24.60 | | AK46-A | -12.11 | 24.10 | | AK46-B | -12.07 | 24.11 | | AK49-A | -7.78 | 24.82 | | AK49-B | -7.82 | 25.00 | | AK4A-A | -8.63 | 22.14 | | AK4A-B | -8.14 | 22.52 | | AK4B-A | -8.14 | 20.15 | | AK4B-B | -8.16 | 20.32 | | AK50-A | -8.39 | 24.73 | | AK50-B | -8.44 | 25.10 | | AK51-A | -10.06 | 24.54 | | AK51-B | -9.84 | 24.24 | | BR1.B V1 | -5.86 | 23.40 | | BR1.B V2 | -5.80 | 23.28 | | BR1.B V3 | -5.87 | 23.26 | | BR13 B B1 | -0.77 | 23.96 | | BR13 B B2 | -0.87 | 24.02 | | BR13 B V1 | -2.05 | 23.45 | | BR13.DB V1 | -5.27 | 23.64 | | BR13.DB V2 | -4.70 | 23.46 | | BR13.DB V3 | -5.11 | 23.61 | | BR2 A B1 | -11.07 | 26.22 | | BR2 A B2 | -11.12 | 26.17 | | BR2 A B3 | -10.91 | 26.11 | | BR2.E2 CC1A | -3.44 | 21.87 | | BR2.E2 CC1B | -3.43 | 21.72 | | BR2.E2 CC1C | -3.48 | 21.55 | | BR2.E2 CC2A | -2.81 | 23.02 | | BR2.E2 CC2B | -2.77 | 22.84 | | BR2.E2 V1 | -5.33 | 21.78 | | BR2.E2 V2 | -5.13 | 21.66 | | BR2.E2 V3 | -5.04 | 21.92 | | BR2.E3 CC2C | -2.84 | 22.91 | | BR6 AB B1 | -4.66 | 24.06 | | BR6 AB B2 | -4.55 | 24.06 | | BR6 AB B3 | -4.60 | 24.17 | | BR6 AF B1 | -2.26 | 22.33 | | BR6 AF B2 | -2.28 | 22.68 | | BR6 AF B3 | -2.29 | 22.94 | | BR6 DA V2 | -3.47 | 22.69 | | BR6 DA V3 | -3.71 | 23.13 | | BR6 DR V1 | -3.06 | 22.81 | | BR6.AC B1 | -4.86 | 23.63 | | BR6.AC B2 | -6.76 | 25.57 | | BR6.AC B3 | -6.97 | 25.91 | | BR6.AC1 B1 | -1.40 | 22.40 | | BR6.AC1 B2 | -1.42 | 22.43 | | BR6.AC1 B3 | -1.38 | 22.37 | | BR6.B B1 | -7.57 | 28.52 | | BR6.B B2 | -7.44 | 28.59 | | BR6.B B3 | -7.39 | 28.74 | | BR6.B QV1 | -0.10 | 19.80 | | BR6.B QV2 | -0.14 | 19.65 | | BR6.B1 B1 | -2.41 | 22.46 | | BR6.B1 B2 | -2.45 | 22.35 | | BR6.B1 B3 | -2.47 | 22.31 |
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