Allan, Adrian S R; Baker, Joel A; Carter, Lionel; Wysoczanski, Richard J (2008): (Table S3d) Major element compositions of onshore Taupo Volcanic Zone tephras [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.815923, In supplement to: Allan, ASR et al. (2008): Reconstructing the Quaternary evolution of the world's most active silicic volcanic system: insights from an ~1.65 Ma deep ocean tephra record sourced from Taupo Volcanic Zone, New Zealand. Quaternary Science Reviews, 27(25-26), 2341-2360, https://doi.org/10.1016/j.quascirev.2008.09.003
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -41.100000 * Longitude: 175.500000
Minimum ORDINAL NUMBER: 1 * Maximum ORDINAL NUMBER: 3
Event(s):
Comment:
All standard deviations = 2sd.
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
78 data points
Data
1 Sample ID | 2 Tephra | 3 Area | 4 Ord No | 5 Repl [#] | 6 SiO2 [%] | 7 SiO2 std dev [±] | 8 TiO2 [%] | 9 TiO2 std dev [±] | 10 Al2O3 [%] | 11 Al2O3 std dev [±] | 12 FeO [%] | 13 FeO std dev [±] | 14 MnO [%] | 15 MnO std dev [±] | 16 MgO [%] | 17 MgO std dev [±] | 18 CaO [%] | 19 CaO std dev [±] | 20 Na2O [%] | 21 Na2O std dev [±] | 22 K2O [%] | 23 K2O std dev [±] | 24 Cl [%] | 25 Cl std dev [±] | 26 Total [%] | 27 Total std dev [±] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Kk1 | Kawakawa Tephra | Irirangi Section, 10 km south of Waiouru | 1 | 26 | 77.2 | 1.04 | 0.16 | 0.11 | 12.8 | 0.77 | 1.25 | 0.18 | 0.12 | 0.15 | 0.14 | 0.06 | 1.10 | 0.22 | 4.06 | 0.38 | 2.97 | 0.27 | 0.20 | 0.06 | 94.98 | 2.29 |
Rt1 | Rotoehu Tephra | 63.86m, Pukaki drill core | 2 | 20 | 78.2 | 0.29 | 0.16 | 0.05 | 12.1 | 0.13 | 0.91 | 0.09 | 0.13 | 0.09 | 0.15 | 0.03 | 0.87 | 0.06 | 4.10 | 0.18 | 3.14 | 0.17 | 0.23 | 0.04 | 95.41 | 2.75 |
LTM | Potaka Tephra | Huangarua River, Te Muna Formation Wairarapa | 3 | 15 | 77.5 | 0.48 | 0.13 | 0.07 | 12.6 | 0.27 | 1.18 | 0.30 | 0.09 | 0.10 | 0.10 | 0.04 | 0.91 | 0.25 | 3.44 | 0.23 | 3.80 | 0.53 | 0.23 | 0.06 | 96.60 | 1.40 |