Osipenko, A B; Sidorov, E G; Shevchenko, S S; Konilov, A N; Rassulov, V A; Rudashevskii, N S (2007): (Table 1) Chemical composition of zircons from amphibolites of the Kamchatksky Cape Peninsula [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.788245, In supplement to: Osipenko, AB et al. (2007): Geochemistry and U-Pb geochronology of zircon in garnet amphibolites from Kamchatkskii Cape Peninsula, Eastern Kamchatka. Translated from Geokhimiya, 2007, 3, 259-268, Geochemistry International, 45(3), 226-234, https://doi.org/10.1134/S0016702907030020
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 56.183000 * Longitude: 162.893000
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample, optional label/labor no | Lab no | Osipenko, A B | |||
| 2 | Silicon dioxide | SiO2 | % | Osipenko, A B | Microprobe | |
| 3 | Zirconium dioxide | ZrO2 | % | Osipenko, A B | Microprobe | |
| 4 | Hafnium oxide | HfO2 | % | Osipenko, A B | Microprobe | |
| 5 | Terbium | Tb | mg/kg | Osipenko, A B | Microprobe | |
| 6 | Phosphorus pentoxide | P2O5 | % | Osipenko, A B | Microprobe | |
| 7 | Sum | Sum | % | Osipenko, A B | Calculated | of oxides |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
112 data points
Data
| 1 Lab no | 2 SiO2 [%] | 3 ZrO2 [%] | 4 HfO2 [%] | 5 Tb [mg/kg] | 6 P2O5 [%] | 7 Sum [%] |
|---|---|---|---|---|---|---|
| 1 | 33.13 | 64.08 | 1.05 | 960 | 0.11 | 98.49 |
| 2 | 33.38 | 64.57 | 1.06 | 1300 | 0.08 | 99.24 |
| 3 | 33.41 | 64.04 | 1.04 | 2300 | 0.03 | 98.78 |
| 4 | 33.18 | 65.00 | 0.94 | 2700 | 0.07 | 99.49 |
| 5 | 32.97 | 63.80 | 1.08 | 2500 | 0.09 | 98.23 |
| 6 | 33.28 | 64.08 | 1.07 | 1800 | 0.00 | 98.64 |
| 7 | 32.94 | 64.09 | 1.12 | 3200 | 0.10 | 98.63 |
| 8 | 33.34 | 64.00 | 1.09 | 1100 | 0.10 | 98.65 |
| 9 | 33.86 | 64.58 | 0.94 | 2350 | 0.02 | 99.67 |
| 10 | 33.70 | 64.97 | 0.95 | 780 | 0.11 | 99.83 |
| 11 | 33.45 | 65.01 | 0.97 | 2400 | 0.01 | 99.72 |
| 12 | 33.48 | 65.83 | 1.12 | 3200 | 0.02 | 100.81 |
| 13 | 34.07 | 64.45 | 0.99 | 2500 | 0.09 | 99.89 |
| 14 | 33.97 | 64.87 | 1.01 | 2000 | 0.05 | 100.13 |
| 15 | 33.29 | 64.73 | 0.99 | 3700 | 0.09 | 99.52 |
| 16 | 33.18 | 65.36 | 0.98 | 2000 | 0.04 | 99.80 |