
| SAMPLE | Method | Au | Ag (1) | Ag (2) | As | Be | Bi | Cd | Co | Cr | Ga | Ge | Hg | In | Mn | Mo | Ni | Rb | Sb | Sc | Se | Sn | Sr | Te | Tl | U | V | W | Y | Zr | Cu | Fe | Zn | Pb | S | SiO2 | Ba | Ca | CO2 | Corg | H2O | H2O- | H2O+ | Al2O3 | MgO | TiO2 | Na2O | K2O | P2O5 | Ir | Pd | Pt | Cl | F | B | Br | Cs | Hf | Li | Nb | Ta | Th | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Sample Type | Mineralogy | Description | Location 1 | Location 2 | Location 3 | LatitudeN | LongitudeW | DecLat | DecLong | Depth | References | |
| ppb | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | wt.% | ppb | ppb | ppb | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | ppm | |||||||||||||||
| Mid-Atlantic Ridge | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| Broken Spur | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-8/4 | a25 | 800 | 15 | 28 | 900 | 30 | 200 | 25 | 8.20 | 38.60 | 0.30 | 0.022 | 0.20 | 7.15 | 0.12 | 0.57 | 0.06 | 0.07 | 0.02 | massive sulfide formations | cp-py-anh-(mc) | coarse-crystalline sulfide material | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-8/4D | a25 | 8.40 | 0.37 | massive sulfide formations | cp-py-anh-(mc) | dulpicate | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-11/1 | a25 | 300 | 11 | 10 | 220 | 5 | 100 | 29 | 1.80 | 8.13 | 0.05 | 0.001 | 0.20 | 7.15 | 0.01 | 1.02 | 0.10 | 0.07 | 0.02 | massive sulfide formations | anh-cp-py | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-11/1D | a25 | 8.50 | 0.06 | massive sulfide formations | anh-cp-py | dulpicate | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-11/3 | a25 | 1400 | 10 | 25 | 460 | 15 | 200 | 22 | 8.80 | 24.70 | 0.09 | 0.027 | 0.20 | 7.15 | 0.04 | 0.51 | 0.06 | 0.07 | 0.02 | massive sulfide formations | py-anh-chl | sulfide-rich part | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-11/3D | a25 | 7.90 | 0.07 | massive sulfide formations | py-anh-chl | dulpicate | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-11/2 | a25 | 300 | 14 | 50 | 27 | 15 | 100 | 20 | 0.26 | 0.90 | 0.005 | 0.001 | 0.20 | 7.15 | 0.01 | 0.34 | 0.06 | 0.07 | 0.02 | massive sulfide formations | anh-(cp-py) | gangue part | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-11/2D | a25 | 0.65 | 0.006 | massive sulfide formations | anh-(cp-py) | dulpicate | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-9/1 | a25 | 1300 | 16 | 33 | 400 | 8 | 200 | 24 | 8.80 | 31.50 | 0.50 | 0.031 | 0.20 | 0.13 | 7.15 | 0.14 | 0.79 | 0.05 | 0.07 | 0.02 | massive sulfide formations | cp-anh-py | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-9/1D | a25 | 9.60 | 0.58 | massive sulfide formations | cp-anh-py | dulpicate | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-6/3 | a25 | 700 | 5 | 8 | 130 | 20 | 200 | 23 | 1.00 | 4.80 | 0.02 | 0.001 | 0.20 | 7.15 | 0.02 | 0.34 | 0.04 | 0.07 | 0.02 | massive sulfide formations | anh-py-(cp) | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-6/3D | a25 | 2.70 | 0.02 | massive sulfide formations | anh-py-(cp) | dulpicate | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-6/2 | a25 | 600 | 10 | 20 | 500 | 10 | 100 | 20 | 8.60 | 27.60 | 0.05 | 0.023 | 0.20 | 7.15 | 0.11 | 0.40 | 0.05 | 0.07 | 0.02 | massive sulfide formations | py-cp-anh-(mc) | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-6/2D | a25 | 8.70 | 0.11 | massive sulfide formations | py-cp-anh-(mc) | dulpicate | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-6/1 | a25 | 700 | 8 | 6 | 130 | 6 | 100 | 25 | 1.12 | 5.29 | 0.02 | 0.001 | 6.00 | 7.15 | 0.01 | 0.28 | 0.04 | 0.07 | 0.02 | massive sulfide formations | anh-(cp-py) | sulfide-rich part | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-3/2 | a25 | 1300 | 60 | 92 | 1000 | 15 | 100 | 24 | 6.30 | 29.00 | 4.00 | 0.035 | 6.00 | 0.12 | 0.26 | 0.03 | 0.11 | 0.09 | 0.07 | 0.02 | massive sulfide formations | py-mc-cp-sp | anhydrite | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-5/1 | a25 | 1200 | 165 | 430 | 300 | 10 | 200 | 40 | 0.40 | 24.00 | 29.00 | 0.045 | 0.20 | 0.10 | 0.24 | 0.06 | 0.11 | 0.12 | 0.07 | 0.02 | massive sulfide formations | sp-mc-py | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-5/1D | a25 | 0.002 | 21.80 | massive sulfide formations | sp-mc-py | dulpicate | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-5/2 | a25 | 1400 | 135 | 380 | 200 | 10 | 9100 | 40 | 0.40 | 27.00 | 26.40 | 0.050 | 0.02 | 0.10 | 0.19 | 0.09 | 0.11 | 0.03 | 0.07 | 0.02 | massive sulfide formations | sp-mc-py | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-5/2D | a25 | 0.03 | 17.50 | massive sulfide formations | sp-mc-py | dulpicate | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1990 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-7 | a25 | 400 | 8 | 15 | 140 | 20 | 200 | 22 | 0.02 | 1.06 | 0.001 | 7.15 | 0.01 | 0.23 | 0.10 | 0.07 | 0.02 | massive anhydrite body | anh | TAG Hydrothermal Field | Active Sulfide Mound | 26oN | 26 | Lisitsyn et al., 1989, Lisitsyn et al., 1990 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR1902-7D | a25 | 0.03 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR 2-75 /1 | a21 | 1150 | <5 | 62 | <0.5 | 81 | <5 | <1 | 77 | 62 | <10 | 2.6 | 0.5 | <5 | <500 | <20 | 3.2 | <5 | <4 | <5 | <10 | 0.01 | 39.03 | 0.11 | 0.023 | 47.40 | 6.47 | 0.01 | 0.05 | 0.3 | <0.1 | <0.04 | <0.01 | 0.10 | <0.03 | 0.02 | <5 | 21 | <1 | <1 | <1 | <0.5 | <0.5 | <3 | <5 | <0.1 | <0.2 | <0.5 | <0.2 | <0.05 | Fe-sulfide crust with late silica | TAG Hydrothermal Field | Active Sulfide Mound | Petersen, 2001 | |||||||||||||||||||||||||||||||||||
| MIR sample - 1 | a24 | 570 | 4.2 | 170 | 34 | 47 | 1.0 | 35.33 | 14.03 | 0.40 | 0.015 | 4.07 | 7.20 | 0.31 | atacamite-Fe-oxide aggregate with basalt frag. | atac-Fe-oxide-hm | TAG Hydrothermal Field | Active Sulfide Mound | outer slope | Krasnov et al., 1995 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR sample - 2 | a24 | 2750 | 120 | 66 | 3 | 43 | 11.4 | 0.43 | 33.85 | 5.32 | 0.022 | 39.78 | 0.20 | 0.14 | Zn-rich massive sulfide | py-mc-sp | TAG Hydrothermal Field | Active Sulfide Mound | intermediate terrace | Krasnov et al., 1995 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR sample - 3 | a24 | 150 | 1.2 | 22 | 350 | 87 | <1 | 3.10 | 12.20 | 0.05 | 0.006 | 29.56 | 0.23 | 20.12 | anhydrite with minor chalcopyrite and pyrite | anh-cp-py | TAG Hydrothermal Field | Active Sulfide Mound | inner mound slope | Krasnov et al., 1995 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| MIR sample - 4 | a24 | 220 | 11 | 740 | 230 | 3.2 | 4.74 | 33.13 | 0.32 | 0.006 | 36.33 | 9.05 | 0.04 | silicified pyrite-chalcopyrite | py-cp-silica | TAG Hydrothermal Field | Active Sulfide Mound | base of black smoker | Krasnov et al., 1995 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2179-1-1B | a21 | 970 | 6 | 51 | <0.5 | <10 | 189 | <10 | <77 | 150 | 10 | 5.9 | 5.8 | 52 | <20 | 13 | <5 | <10 | 23.00 | 30.50 | 0.37 | 0.003 | 34.50 | <0.50 | 0.005 | 0.07 | 0.2 | <0.1 | 0.08 | <0.01 | 0.32 | <0.03 | 0.04 | <10 | 2.9 | sulfide crust | cp-py | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2179-2-2A | a21 | 380 | 6 | 43 | <0.5 | <10 | 910 | <10 | <77 | 160 | <10 | 1.6 | 2.4 | 230 | 900 | <5 | <5 | <10 | 9.50 | 23.08 | 0.14 | 0.003 | 33.80 | <0.50 | 0.003 | 9.86 | 0.2 | <0.1 | 0.31 | <0.01 | 1.17 | <0.03 | 0.05 | <10 | 0.9 | black smoker | anh-py-cp | TAG Hydrothermal Field | Active Sulfide Mound | BSC | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2179-4 | a21 | 50 | 6 | 1 | <0.5 | <10 | 106 | 14 | <77 | 140 | <10 | 0.1 | 5.6 | 630 | 160 | <5 | <5 | <10 | 23.50 | 24.27 | 0.04 | <0.002 | 28.30 | <0.50 | 0.007 | 1.65 | <0.1 | 0.16 | <0.01 | 0.13 | <0.03 | 0.05 | <10 | 2.9 | black smoker | cp-py-anh | TAG Hydrothermal Field | Active Sulfide Mound | BSC | Hannington et al., 1993; Geological Survey of Canada, unpublished data | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2179-4-1-1 | a21 | 130 | 6 | 8 | <0.5 | <10 | 205 | 12 | <77 | 68 | <10 | 0.7 | 2.5 | 315 | 1600 | <5 | <5 | <10 | 10.80 | 12.38 | 0.08 | <0.002 | 28.20 | <0.50 | 0.02 | 16.51 | <0.1 | <0.1 | 0.46 | <0.01 | 0.16 | <0.03 | 0.08 | <10 | 1.3 | black smoker | anh-cp-py | TAG Hydrothermal Field | Active Sulfide Mound | BSC | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2179-4-1-4 | a21 | 30 | 1 | 1 | <0.5 | <10 | 56 | 11 | <77 | 9 | <10 | 0.1 | 1.0 | 120 | 1900 | <5 | <5 | <10 | 3.96 | 4.80 | 0.02 | <0.002 | 23.80 | 0.54 | 0.002 | 23.09 | <0.1 | 1.08 | <0.01 | 0.32 | 0.07 | 0.05 | <10 | <0.5 | black smoker | anh-cp-(py) | TAG Hydrothermal Field | Active Sulfide Mound | BSC | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2179-4-1A1 | a21 | 100 | 3 | 4 | <0.5 | <10 | 131 | 11 | 155 | 51 | <10 | 0.3 | 2.7 | 370 | 980 | <5 | <5 | <10 | 11.60 | 12.59 | 0.05 | <0.002 | 27.30 | 0.66 | 0.02 | 12.86 | 0.2 | <0.1 | 2.97 | <0.01 | 0.30 | 0.07 | 0.05 | <10 | 1.5 | black smoker | anh-cp-py | TAG Hydrothermal Field | Active Sulfide Mound | BSC | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2179-4-1T1 | a21 | 50 | <5 | 1 | <0.5 | <10 | 47 | 17 | 77 | 15 | <10 | 0.1 | 2.8 | 390 | 1400 | <5 | <5 | <10 | 12.10 | 11.19 | 0.03 | <0.002 | 24.80 | 0.53 | 0.01 | 14.37 | <0.1 | 1.95 | <0.01 | 0.15 | 0.05 | 0.05 | <10 | 1.5 | black smoker | anh-cp-(py) | TAG Hydrothermal Field | Active Sulfide Mound | BSC | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2181-1-1A2 | a21 | 250 | 7 | 19 | <0.5 | <10 | 330 | 10 | <77 | 110 | <10 | 0.5 | 2.2 | 160 | 1000 | <5 | <5 | <10 | 8.50 | 18.74 | 0.24 | 0.003 | 32.20 | <0.50 | 0.004 | 13.22 | 0.1 | <0.1 | 0.19 | <0.01 | 0.77 | 0.11 | 0.08 | <10 | 0.9 | black smoker | anh-cp-py | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2183-4-1A | a21 | 13180 | 1385 | 63 | <0.5 | 1875 | <2 | <10 | <77 | 44 | 13 | 99 | <0.5 | <5 | <20 | 42 | <5 | <10 | 0.41 | 6.51 | 53.40 | 0.035 | 32.30 | 1.26 | 0.03 | 0.09 | 0.1 | <0.1 | 0.06 | <0.01 | 0.27 | 0.06 | 0.05 | <10 | <0.5 | white smoker | sp-py | average of 2 | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2183-4-1B | a21 | 20750 | 1060 | 42 | <0.5 | 2000 | <2 | <10 | <77 | 48 | 16 | 90 | <0.5 | <5 | <20 | <5 | <5 | <10 | 0.51 | 6.99 | 51.90 | 0.030 | 33.20 | <0.50 | 0.01 | 0.09 | <0.1 | <0.1 | 0.17 | <0.01 | 1.06 | 0.13 | 0.06 | <10 | <0.5 | white smoker | sp-py | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2183-4-1C | a21 | 13360 | 1920 | 79 | <0.5 | 1780 | <2 | <10 | 155 | 56 | 14 | 93 | <0.5 | <5 | <20 | 52 | <5 | <10 | 0.41 | 5.90 | 54.20 | 0.048 | 32.20 | 1.11 | 0.02 | 0.09 | 0.1 | <0.1 | 0.13 | <0.01 | 0.69 | 0.09 | 0.06 | <10 | <0.5 | white smoker | sp-py | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2183-6-2A | a21 | 1870 | 170 | 120 | <0.5 | 78 | 41 | 170 | <77 | 120 | 14 | 15 | 1.0 | 8 | <20 | 13 | <5 | <10 | 1.70 | 36.79 | 6.60 | 0.031 | 42.10 | <0.50 | 0.003 | 0.06 | <0.1 | 0.04 | <0.01 | 0.14 | <0.03 | 0.03 | <10 | <0.5 | Fe-Zn-Cu sulfides | py-sp-(cp) | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2183-7-OA | a21 | <5 | <5 | 1 | <0.5 | <10 | 13 | 5 | <77 | 6 | <10 | <0.2 | <0.5 | 10 | 1500 | <5 | <5 | <10 | 0.23 | 0.61 | 0.02 | 0.002 | 21.00 | 1.94 | <0.003 | 26.37 | 0.1 | <0.1 | 0.92 | <0.01 | 0.14 | <0.03 | 0.08 | <10 | <0.5 | massive anhydrite | anh | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2183-9-1A | a21 | 1630 | 79 | 151 | <0.5 | 18 | 20 | 18 | 13631 | 62 | 29 | 37 | 4.7 | 10 | 130 | 140 | <5 | <10 | 17.60 | 30.99 | 0.38 | 0.015 | 27.60 | 4.11 | 0.04 | 0.44 | 0.9 | <0.1 | 0.37 | <0.01 | 1.23 | 0.20 | 0.29 | <10 | 2.1 | Cu-Fe-sulfides | cp-py | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Geological Survey of Canada, unpublished data | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2187-1-1A1 | a21 | 6597 | 177 | 47 | <0.5 | 1723 | <2 | 5 | 232 | 75 | 10 | 201 | <0.5 | <5 | <20 | 36 | <5 | <10 | 0.63 | 4.39 | 51.60 | 0.041 | 30.60 | 5.29 | 0.05 | 0.12 | 0.1 | <0.1 | 0.15 | <0.01 | 1.26 | 0.17 | 0.07 | <10 | <0.5 | white smoker | sp-py | average of 3 | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||
| ALV2187-1-1A2 | a21 | 986 | 150 | 32 | <0.5 | 1680 | <2 | 11 | 155 | 108 | 18 | 199 | 0.6 | <5 | <20 | 47 | <5 | <10 | 0.65 | 6.92 | 51.40 | 0.037 | 32.10 | 1.83 | 0.01 | 0.11 | 0.1 | <0.1 | 0.16 | <0.01 | 1.08 | 0.17 | 0.06 | <10 | <0.5 | white smoker | sp-py | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2187-1-1B | a21 | 2620 | 180 | 51 | <0.5 | 1080 | <2 | 8 | 194 | 68 | 11 | 145 | <0.5 | <5 | <20 | 12 | <5 | <10 | 0.43 | 8.92 | 41.20 | 0.060 | 26.65 | 11.90 | 0.01 | 0.15 | 0.2 | <0.1 | 0.31 | <0.01 | 1.64 | 0.19 | 0.09 | <10 | <0.5 | white smoker | sp-py-silica | average of 2 | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||
| ALV2187-1-1C | a21 | 42960 | 186 | 19 | <0.5 | 2043 | <2 | 5 | <77 | 244 | 18 | 308 | 0.7 | <5 | <20 | 200 | <5 | <10 | 1.40 | 3.46 | 56.30 | 0.016 | 31.00 | 0.77 | 0.01 | 0.06 | 0.1 | 0.46 | 0.06 | <0.01 | 0.37 | 0.09 | 0.09 | <10 | <0.5 | white smoker | sp | average of 3 | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||
| ALV2187-1-4A | a21 | 340 | 580 | 91 | <0.5 | 2260 | <2 | 18 | <77 | <1 | 26 | 370 | <0.5 | <5 | <20 | <5 | <5 | <10 | 0.61 | 1.51 | 55.40 | 0.082 | 28.80 | 0.94 | 0.005 | 0.09 | <0.1 | 0.12 | <0.01 | 0.12 | 0.08 | 0.08 | <10 | <0.5 | white smoker | sp | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2187-1-6A | a21 | 180 | 560 | 117 | <0.5 | 950 | <2 | 5 | <77 | <1 | 19 | 63 | <0.5 | <5 | <20 | <5 | <5 | <10 | 0.54 | 1.97 | 54.80 | 0.100 | 29.70 | 7.61 | <0.003 | 0.06 | 0.3 | <0.1 | 0.05 | <0.01 | 0.28 | 0.14 | 0.07 | <10 | <0.5 | white smoker | sp-silica | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2189-4-1 pc1 | a22 | 190 | <5 | 35 | <0.5 | 10 | 26 | <1 | 100 | 100 | <10 | 1.8 | 0.6 | <5 | <500 | <20 | <0.5 | 11 | <4 | <5 | <10 | 0.01 | 37.42 | 0.01 | 42.20 | 10.9 | 0.009 | 0.07 | 0.3 | <0.1 | 0.07 | <0.01 | 0.20 | 0.06 | 0.03 | <5 | 25 | <1 | <1 | <1 | <0.5 | <0.5 | <3 | <5 | 0.2 | <0.2 | <0.5 | <0.2 | <0.05 | Fe-sulfides with Fe-oxide 'clasts' | py-Fe-oxides | TAG Hydrothermal Field | Active Sulfide Mound | Petersen, 2001 | |||||||||||||||||||||||||||||||||||
| ALV2189-5-2A | a22 | 660 | 44 | 44 | <0.5 | <10 | 89 | 210 | <77 | 125 | <10 | 2.9 | 0.7 | 5 | <20 | <5 | <5 | <10 | 1.02 | 40.29 | 0.44 | 0.013 | 44.90 | 2.10 | 0.004 | 0.05 | <0.1 | 0.04 | <0.01 | 0.11 | 0.11 | 0.04 | <10 | <0.5 | Fe-sulfides | py | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-11-1A | a21 | 13220 | 225 | 48 | <0.5 | 2205 | <2 | <10 | 465 | 44 | 11 | 224 | <0.5 | <5 | <20 | <5 | <5 | <10 | 0.61 | 4.51 | 55.10 | 0.037 | 32.30 | <0.50 | 0.05 | 0.09 | 0.2 | <0.1 | 0.11 | <0.01 | 0.98 | 0.21 | 0.07 | <10 | <0.5 | white smoker | sp-py | average of 2 | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-11-1B | a21 | 4690 | 70 | 64 | <0.5 | 1380 | <2 | 13 | 155 | 42 | 15 | 127 | 0.7 | <5 | <20 | <5 | <5 | <10 | 0.68 | 15.74 | 40.80 | 0.040 | 36.70 | <0.50 | 0.006 | 0.06 | 0.1 | <0.1 | 0.05 | <0.01 | 0.26 | 0.15 | 0.10 | <10 | <0.5 | white smoker | sp-py | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-13-1A | a21 | 1010 | 240 | 63 | <0.5 | 250 | 2 | 56 | 232 | 37 | <10 | 77 | 0.8 | <5 | <20 | <5 | <5 | <10 | 0.35 | 23.92 | 17.90 | 0.038 | 35.30 | 10.20 | 0.006 | 0.07 | <0.1 | <0.04 | <0.01 | 0.13 | 0.12 | 0.04 | <10 | <0.5 | Fe-Zn sulfides, py, silica | mc-sp-(-silica) | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-14-1A | a21 | 15085 | 1125 | 87 | <0.5 | 1610 | <2 | <10 | <77 | 57 | 27 | 252 | <0.5 | <5 | <20 | <5 | <5 | <10 | 0.61 | 1.20 | 57.40 | 0.080 | 30.00 | 6.71 | <0.003 | 0.05 | 0.1 | <0.1 | 0.05 | <0.01 | 0.25 | 0.08 | 0.10 | <10 | 0.7 | white smoker | sp-silica-py | average of 2 | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-14-1B | a21 | 295 | 1190 | 104 | <0.5 | 1230 | <2 | <10 | 155 | 40 | 17 | 181 | <0.5 | <5 | <20 | 13 | <5 | <10 | 0.38 | 3.29 | 49.90 | 0.080 | 26.80 | 12.50 | <0.003 | 0.08 | 0.3 | <0.1 | 0.07 | <0.01 | 0.42 | 0.11 | 0.10 | <10 | 0.6 | white smoker | sp-silica-py | average of 2 | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Tivey et al., 1994 | |||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-14-1C | a21 | 110 | 1570 | 153 | <0.5 | 1810 | <2 | <10 | 387 | 64 | 23 | 282 | 0.7 | <5 | <20 | 12 | <5 | <10 | 0.46 | 0.87 | 57.90 | 0.110 | 30.70 | 2.27 | <0.003 | 0.09 | 0.2 | <0.1 | 0.08 | <0.01 | 0.35 | 0.10 | 0.08 | <10 | 0.9 | white smoker | sp | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Geological Survey of Canada, unpublished data | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-14-1D | a21 | 6015 | 1250 | 88 | <0.5 | 1820 | <2 | <10 | 155 | 45 | 18 | 322 | <0.5 | 4 | <20 | <5 | <5 | <10 | 0.70 | 0.83 | 54.50 | 0.076 | 28.00 | 9.90 | <0.003 | 0.13 | <0.1 | <0.1 | 0.07 | <0.01 | 0.65 | 0.16 | 0.07 | <10 | 0.7 | white smoker | sp-silica | average of 2 | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Geological Survey of Canada, unpublished data | |||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-14-1E | a21 | 70 | 1690 | 137 | <0.5 | 930 | <2 | <10 | 542 | 16 | <10 | 126 | <0.5 | <5 | <20 | 7 | <5 | <10 | 0.34 | 1.21 | 57.10 | 0.110 | 29.90 | 4.53 | 0.05 | 0.12 | 0.1 | <0.1 | 0.08 | <0.01 | 0.33 | 0.07 | 0.10 | <10 | 0.7 | white smoker | sp-(silica-py) | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Geological Survey of Canada, unpublished data | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-14-1F | a21 | 3180 | 1300 | 89 | <0.5 | 1680 | <2 | <10 | 310 | 42 | 16 | 266 | <0.5 | <5 | <20 | 13 | <5 | <10 | 0.63 | 1.27 | 57.70 | 0.055 | 31.30 | 3.03 | 0.01 | 0.11 | 0.1 | <0.1 | 0.04 | <0.01 | 0.24 | <0.03 | 0.08 | <10 | 0.7 | white smoker | sp-(py-bn-silica) | TAG Hydrothermal Field | Active Sulfide Mound | Kremlin | Hannington et al., 1993; Geological Survey of Canada, unpublished data | ||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-7-1A | a21 | 700 | 28 | 48 | <0.5 | 20 | 154 | 100 | 310 | 100 | 20 | 11.0 | 3.2 | 5 | <20 | 67 | <5 | <10 | 15.90 | 31.68 | 1.10 | 0.015 | 41.90 | 4.19 | 0.002 | 0.11 | <0.1 | 0.08 | <0.01 | 0.45 | 0.16 | 0.10 | <10 | 2.6 | Cu-Fe-sulfides | cp-py | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Geological Survey of Canada, unpublished data | ||||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2190-8-1A | a22 | 100 | <5 | 35 | <0.5 | <10 | 337 | 20 | 155 | 78 | <10 | 0.7 | 1.2 | 58 | 760 | <5 | <5 | <10 | 4.10 | 26.23 | 0.05 | 0.002 | 39.10 | <0.50 | 0.006 | 10.51 | <0.1 | 0.07 | <0.01 | 0.61 | 0.18 | 0.05 | <10 | <0.5 | Fe-Cu-sulfides + anhydrite | py-anh-cp | TAG Hydrothermal Field | Active Sulfide Mound | Hannington et al., 1993; Tivey et al., 1994 | ||||||||||||||||||||||||||||||||||||||||||||||||||
| ALV2584-9 | a22 | 688 | <5 | 30 | <0.5 | 8 | <5 | 18 | 77 | 73 | <10 | 1.4 | 0.4 | 7 | <500 | <20 | <0.5 | <5 | <4 | <5 | <10 | 0.11 | 32.31 | 8.40 | 0.080 | 46.00 | <0.50 | 0.009 | 0.05 | 0.2 | <0.1 | <0.04 | <0.01 | 0.22 | <0.03 | <0.01 | <5 | 15 | <1 | <1 | <1 | <0.5 | <0.5 | <3 | <5 | <0.1 | 0.3 | <0.5 | <0.5 | <0.05 | white smoker | sp-silica | TAG Hydrothermal Field | Active Sulfide Mound | Petersen, 2001 | ||||||||||||||||||||||||||||||||||
| ALV2587-1 | a22 | 620 | <5 | 68 | <0.5 | 430 | <5 | <1 | <77 | 120 | <10 | 1.9 | 0.5 | 52 | <500 | 75 | 5.5 | 7 | <4 | <5 | <10 | 10.60 | 37.07 | 0.06 | 44.60 | <0.50 | 0.01 | 1.04 | 0.1 | 0.10 | 0.06 | <0.01 | 0.43 | <0.03 | <0.01 | <3 | 31 | 6 | <1 | <1 | <0.5 | <0.5 | <3 | <5 | 0.1 | <0.2 | <0.5 | <0.5 | <0.05 | Fe-Cu-sulfides + anhydrite | py-(anh) | TAG Hydrothermal Field | Active Sulfide Mound | BSC | Petersen, 2001 | ||||||||||||||||||||||||||||||||||
North Atlantic
| North Atlantic MAR10_19 | North Atlantic MAR20_29 | North Atlantic MAR30_39 |
North Pacific
|North East Pacific California|NE_Pacific EQ EPR| NE_Pacific Gorda Ridge| NE_Pacific JF Ridge| NE_Pacific Rise|
|NW_Pacific Izu-Bonin Arc |NW_Pacific Mariana Arc |NW_Pacific Okinawa Trough |
South Pacific
|Southern East Pacific Rise|SW_Pacific Manus Basin Solomon| SW_Pacific Fiji Basin | SW_Pacific NZ Lau Basin |
Other Regions
| Indian Ocean Region |Mediterranean | Red Sea Region |
Ancillary Data
| Submarine vents: Brief Description & Information |Analytical methods and detection limits | References for Submarine Vents
|Locations of Hydrothermal Vents sites |