Talarico, Franco M; Sandroni, Sonja; Fielding, Christopher R; Atkins, Cliff (2000): (Table 2) Selected major elements and trace elements of core CRP-2A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.143978, In supplement to: Talarico, FM et al. (2000): Variability, petrography and provenance of basement clasts in core from CRP-2/2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(4), 529-544, hdl:10013/epic.28254.d001
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Project(s):
Cape Roberts Project (CRP)
Coverage:
Latitude: -77.005980 * Longitude: 163.719450
Date/Time Start: 1998-10-16T07:30:00 * Date/Time End: 1998-11-25T14:20:00
Minimum Elevation: -177.9 m * Maximum Elevation: -177.9 m
Event(s):
CRP-2A (14.2 km at 096° true from Cape Roberts) * Latitude: -77.005980 * Longitude: 163.719450 * Date/Time Start: 1998-10-16T07:30:00 * Date/Time End: 1998-11-25T14:20:00 * Elevation: -177.9 m * Recovery: 624 m * Location: off Cape Roberts, Ross Sea, Antarctica * Campaign: CRP-2 * Basis: Sampling/drilling from ice * Method/Device: Core wireline system (CWS) * Comment: 921 m at 284° from CRP-1. Sea-ice thickness: 2.0 m (1 Oct) to 2.2 m (23 Nov). Sea riser embedded to 13.03 mbsf. Lateral ice movement: 9.87 m to east from 17 Oct to 23 Nov. HQ core to 199.31 mbsf. NQ core to 624.15 mbsf. 13.03 to 45.97 mbsf, 11.29 m (34%) partially following CRP-2. 45.07 to 624.15 mbsf, 548.67 m (95%) new hole. Deepest core-lithology: hard sandy siltstone. Deepest core-age: earliest Oligocene (ca. 33 Ma on diatoms, nannofossils and dinoflagellates)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
304 data points
Data
1 Sample label | 2 SiO2 [%] | 3 TiO2 [%] | 4 Al2O3 [%] | 5 Fe2O3 [%] | 6 FeO [%] | 7 MnO [%] | 8 MgO [%] | 9 CaO [%] | 10 Na2O [%] | 11 K2O [%] | 12 P2O5 [%] | 13 LOI [%] | 14 Nb [mg/kg] | 15 Zr [mg/kg] | 16 Y [mg/kg] | 17 Sr [mg/kg] | 18 Rb [mg/kg] | 19 Ni [mg/kg] | 20 Cr [mg/kg] | 21 V [mg/kg] | 22 Ba [mg/kg] | 23 La [mg/kg] | 24 Ce [mg/kg] | 25 ASI | 26 Qz [%] | 27 Or [%] | 28 Ab [%] | 29 An [%] | 30 Al2O3 Korund [%] | 31 Di [%] | 32 Hyp [%] | 33 Ol [%] | 34 Magmatites [%] | 35 Rt [%] | 36 Ilm [%] | 37 Ap [%] | 38 Total [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
TAL64 | 63.38 | 0.92 | 15.34 | 1.17 | 4.26 | 0.09 | 2.28 | 5 | 3.24 | 3.23 | 0.27 | 1.27 | 18 | 192 | 24 | 598 | 98 | 8 | 23 | 59 | 1105 | 33 | 62 | 0.90 | 17.95 | 19.09 | 27.41 | 17.77 | 0.00 | 2.47 | 9.96 | 0.00 | 1.70 | 0.00 | 1.75 | 0.64 | 100.0 |
TAL44 | 70.71 | 0.29 | 13.93 | 0.28 | 1.85 | 0.04 | 0.52 | 2 | 3.08 | 5.03 | 0.08 | 2.38 | 14 | 207 | 21 | 223 | 168 | 1 | 8 | 14 | 939 | 44 | 81 | 1.01 | 27.86 | 29.72 | 26.06 | 8.46 | 0.32 | 0.00 | 4.06 | 0.00 | 0.41 | 0.00 | 0.55 | 0.19 | 100.0 |
TAL40 | 70.98 | 0.30 | 14.18 | 0.33 | 2.37 | 0.06 | 0.46 | 2 | 3.72 | 5.08 | 0.05 | 0.82 | 15 | 362 | 28 | 298 | 157 | 0 | 4 | 10 | 1791 | 57 | 90 | 0.97 | 24.34 | 30.02 | 31.48 | 6.99 | 0.00 | 0.70 | 4.48 | 0.00 | 0.48 | 0.00 | 0.57 | 0.12 | 100.0 |
TAL65 | 71.42 | 0.44 | 13.60 | 1.63 | 1.39 | 0.06 | 1.15 | 3 | 3.86 | 0.82 | 0.12 | 2.31 | 9 | 180 | 10 | 508 | 30 | 7 | 12 | 21 | 446 | 28 | 48 | 1.04 | 37.33 | 4.85 | 32.66 | 15.09 | 0.83 | 0.00 | 3.45 | 0.00 | 2.36 | 0.00 | 0.84 | 0.28 | 100.0 |
TAL9 | 72.44 | 0.29 | 13.51 | 0.58 | 1.27 | 0.02 | 0.48 | 1 | 3.10 | 5.98 | 0.05 | 0.85 | 15 | 205 | 22 | 306 | 224 | 0 | 2 | 11 | 894 | 68 | 109 | 0.95 | 27.59 | 35.34 | 26.23 | 5.29 | 0.00 | 1.15 | 2.03 | 0.00 | 0.84 | 0.00 | 0.55 | 0.12 | 100.0 |
TAL34 | 72.81 | 0.23 | 14.39 | 0.27 | 1.32 | 0.04 | 0.44 | 2 | 3.84 | 3.81 | 0.05 | 0.66 | 15 | 137 | 15 | 505 | 148 | 2 | 6 | 8 | 1181 | 24 | 38 | 1.00 | 29.91 | 22.51 | 32.49 | 10.34 | 0.16 | 0.00 | 2.99 | 0.00 | 0.39 | 0.00 | 0.44 | 0.12 | 100.0 |
TAL36 | 73.33 | 0.19 | 14.43 | 0.65 | 0.49 | 0.02 | 0.61 | 3 | 3.38 | 3.25 | 0.04 | 0.93 | 6 | 146 | 13 | 599 | 92 | 1 | 4 | 8 | 1345 | 23 | 31 | 1.03 | 34.66 | 19.20 | 28.60 | 13.03 | 0.58 | 0.00 | 1.61 | 0.00 | 0.94 | 0.00 | 0.36 | 0.09 | 100.0 |
TAL49 | 73.96 | 0.17 | 13.67 | 0.25 | 1.18 | 0.03 | 0.39 | 2 | 3.51 | 4.03 | 0.04 | 0.98 | 9 | 117 | 11 | 391 | 147 | 0 | 4 | 8 | 623 | 22 | 36 | 1.02 | 33.03 | 23.81 | 29.70 | 8.62 | 0.38 | 0.00 | 2.71 | 0.00 | 0.36 | 0.00 | 0.32 | 0.09 | 100.0 |