Portnyagin, Maxim V; Naumov, V B; Mironov, N L; Belousov, I A; Kononkova, N N (2011): (Table 1) Major oxide composition of olivine in basalts of the 1996 Karymsky volcano eruption [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.786825, In supplement to: Portnyagin, MV et al. (2011): Composition and evolution of the melts erupted in 1996 at Karymskoe Lake, Eastern Kamchatka: Evidence from inclusions in minerals. Translated from Geokhimiya, 2011, 49(11), 1153-1178, Geochemistry International, 49(11), 1085-1110, https://doi.org/10.1134/S0016702911110085
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 53.997000 * Longitude: 159.450000
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Portnyagin, Maxim V | |||
| 2 | Sample code/label 2 | Sample label 2 | Portnyagin, Maxim V | |||
| 3 | Silicon dioxide | SiO2 | % | Portnyagin, Maxim V | CAMECA electron microprobe | |
| 4 | Iron oxide, FeO | FeO | % | Portnyagin, Maxim V | CAMECA electron microprobe | |
| 5 | Manganese oxide | MnO | % | Portnyagin, Maxim V | CAMECA electron microprobe | |
| 6 | Magnesium oxide | MgO | % | Portnyagin, Maxim V | CAMECA electron microprobe | |
| 7 | Calcium oxide | CaO | % | Portnyagin, Maxim V | CAMECA electron microprobe | |
| 8 | Chromium(III) oxide | Cr2O3 | % | Portnyagin, Maxim V | CAMECA electron microprobe | |
| 9 | Nickel oxide | NiO | % | Portnyagin, Maxim V | CAMECA electron microprobe | |
| 10 | Sum | Sum | % | Portnyagin, Maxim V | Calculated | |
| 11 | Forsterite | Fo | % | Portnyagin, Maxim V |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
99 data points
Data
| 1 Sample label | 2 Sample label 2 | 3 SiO2 [%] | 4 FeO [%] | 5 MnO [%] | 6 MgO [%] | 7 CaO [%] | 8 Cr2O3 [%] | 9 NiO [%] | 10 Sum [%] | 11 Fo [%] |
|---|---|---|---|---|---|---|---|---|---|---|
| KR96BV | 1 | 39.19 | 17.90 | 0.27 | 43.50 | 0.18 | 0.03 | 0.08 | 101.15 | 81 |
| KR96BV | 2 | 37.97 | 21.88 | 0.35 | 40.29 | 0.18 | 0.01 | 0.08 | 100.76 | 77 |
| KR96BV | 3 | 37.78 | 23.48 | 0.38 | 38.64 | 0.18 | 0.02 | 0.02 | 100.50 | 75 |
| KR96BV | 4 | 37.69 | 25.67 | 0.44 | 36.70 | 0.18 | 0.01 | 0.07 | 100.76 | 72 |
| KR99/96 | 5 | 38.89 | 17.43 | 0.19 | 43.49 | 0.16 | <0.01 | 0.07 | 100.23 | 82 |
| KR99/96 | 6 | 38.95 | 17.91 | 0.26 | 42.47 | 0.18 | 0.05 | 0.06 | 99.88 | 81 |
| KR99/96 | 7 | 38.82 | 18.08 | 0.34 | 42.44 | 0.21 | 0.04 | 0.09 | 100.02 | 81 |
| KR99/96 | 8 | 37.79 | 22.54 | 0.36 | 38.98 | 0.18 | 0.03 | 0.07 | 99.95 | 76 |
| KR99/96 | 9 | 37.81 | 22.98 | 0.42 | 38.86 | 0.15 | 0.01 | 0.08 | 100.31 | 75 |