Table 1.
Sample | Sample type | Location | 187Os/188Os | Os model age | Reference |
---|---|---|---|---|---|
Terrestrial samples | |||||
Yodda | Os-Ir alloy | Papua New Guinea | 0.1290024 ± 12 | 80 Ma | [1] |
Bald Hills | Os-Ir alloy | Tasmania (AU) | 0.120041 ± 22 | 130 Ma | [1] |
Savage River | Os-Ir alloy | Tasmania (AU) | 0.119940 ± 9 | 130 Ma | [1] |
L5–1 | Os-Ir-Ru alloy | Josephine Ophiolite Complex (US) | 0.1411853 ± 30 | 162 Ma | [2] |
M3–6 | Os-Ir-Ru alloy | Josephine Ophiolite Complex (US) | 0.1228417 ± 52 | 162 Ma | [2] |
M8–2 | Os-Ir-Ru alloy | Josephine Ophiolite Complex (US) | 0.1260988 ± 55 | 162 Ma | [2] |
C1 | Chromitite | Shetland Ophiolite Complex (UK) | 0.129210 ± 28 | 492 Maa | [3,4] |
C2 | Chromitite | Shetland Ophiolite Complex (UK) | 0.129227 ± 8 | 492 Maa | [3,4] |
C3 | Chromitite | Shetland Ophiolite Complex (UK) | 0.129250 ± 6 | 492 Maa | [3,4] |
Guli | Os-Ir alloy | Guli clinopyroxene-dunite massif (RU) | 0.12428–0.12478 | 545–615 Ma | [5] |
Kushva | Os-Ir alloy | Urals (RU) | - | 870 Ma | [6] |
Nizhny Tagil | Os-Ir alloy | Urals (RU) | - | 870 Ma | [6] |
B-1 | Ru-Os-Ir alloy | Witwatersrand (SA) | − | 2.66–4.10 Ga | [7] |
Meteoritic samples | |||||
Morasko | Iron meteorite | IAB-Main Group | 0.14649 | 3.5 ± 1.3 Mab | [8] |
Hope | Iron meteorite | IAB-Main Group | 0.16727 | - | [8] |
Campo del Cielo | Iron meteorite | IAB-Main Group | 0.12418 | 4.1 ± 0.5 Mab | [8] |
Bischtübe | Iron meteorite | IAB-sLL | 0.12764 | 4.5 ± 1.2 Mab | [8] |
Deport | Iron meteorite | IAB-sLL | 0.12870 | 5.3 ± 2.0 Mab | [8] |
Toluca | Iron meteorite | IAB-sLL | 0.13228 | 5.4 ± 1.2 Mab | [8] |
A zircon U-Pb crystallization age from a plagiogranite vein cutting the upper portion of the SOC providing a minimum age (from Spray and Dunning, 1991)
Metal-silicate Hf-W segregation model ages (ΔtCAI) calculated relative to CAI (Worsham et al., 2017).