Lackschewitz, Klas Sven; Mertz, Dieter F; Devey, Colin W; Garbe-Schönberg, Dieter (2003): (Table 3) Major element composition of silicic and mafic glasses from ODP Site 180-1109 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.666870, In supplement to: Lackschewitz, KS et al. (2003): Late Cenozoic volcanism in the western Woodlark Basin area, SW Pacific: the sources of marine volcanic ash layers based on their elemental and Sr–Nd isotope compositions. Bulletin of Volcanology, 65(2-3), 182-200, https://doi.org/10.1007/s00445-002-0252-z
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -9.506483 * Longitude: 151.573017
Date/Time Start: 1998-06-24T00:00:00 * Date/Time End: 1998-07-04T00:00:00
Minimum DEPTH, sediment/rock: 1.23 m * Maximum DEPTH, sediment/rock: 471.51 m
Event(s):
180-1109 * Latitude: -9.506483 * Longitude: 151.573017 * Date/Time Start: 1998-06-24T00:00:00 * Date/Time End: 1998-07-04T00:00:00 * Elevation: -2211.0 m * Penetration: 1202 m * Recovery: 648.1 m * Location: Solomon Sea * Campaign: Leg180 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 95 cores; 849.2 m cored; 352.8 m drilled; 76.3% recovery
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
508 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sample comment | 4 Lithology | 5 Grains [#] | 6 NOBS [#] | 7 SiO2 [%] | 8 SiO2 std dev [±] | 9 TiO2 [%] | 10 TiO2 std dev [±] | 11 Al2O3 [%] | 12 Al2O3 std dev [±] | 13 FeO [%] | 14 FeO std dev [±] | 15 MnO [%] | 16 MnO std dev [±] | 17 MgO [%] | 18 MgO std dev [±] | 19 CaO [%] | 20 CaO std dev [±] | 21 Na2O [%] | 22 Na2O std dev [±] | 23 K2O [%] | 24 K2O std dev [±] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.23 | 180-1109A-1H-1,123-124 | tephra layer | 11 | 29 | 72.1 | 0.53 | 0.08 | 0.03 | 12.1 | 0.17 | 0.53 | 0.06 | 0.03 | 0.03 | 0.06 | 0.01 | 0.80 | 0.03 | 3.1 | 0.08 | 4.3 | 0.24 | |
5.65 | 180-1109C-1H-4,115-118 | tephra layer | 5 | 10 | 67.0 | 0.33 | 0.33 | 0.02 | 14.2 | 0.10 | 2.15 | 0.06 | 0.11 | 0.03 | 0.24 | 0.02 | 0.81 | 0.04 | 4.5 | 0.13 | 4.3 | 0.29 | |
9.28 | 180-1109C-2H-2,38-41 | tephra layer | 5 | 25 | 69.7 | 0.48 | 0.18 | 0.03 | 13.2 | 0.30 | 1.52 | 0.11 | 0.06 | 0.04 | 0.09 | 0.02 | 0.42 | 0.04 | 4.2 | 0.13 | 4.7 | 0.29 | |
17.36 | 180-1109C-3H-1,46-48 | tephra layer | 4 | 13 | 74.2 | 0.67 | 0.28 | 0.02 | 11.0 | 0.07 | 1.29 | 0.08 | 0.07 | 0.04 | 0.03 | 0.02 | 1.76 | 0.04 | 3.1 | 0.10 | 1.3 | 0.07 | |
22.44 | 180-1109C-3H-4,104-106 | tephra layer | 7 | 29 | 75.2 | 0.49 | 0.02 | 0.02 | 12.9 | 0.18 | 0.55 | 0.05 | 0.00 | 0.00 | 0.00 | 0.00 | 0.33 | 0.05 | 4.1 | 0.12 | 4.0 | 0.20 | |
24.80 | 180-1109C-3H-6,40-43 | tephra layer | 6 | 19 | 73.7 | 0.53 | 0.13 | 0.02 | 12.1 | 0.13 | 0.60 | 0.07 | 0.06 | 0.03 | 0.08 | 0.01 | 0.36 | 0.04 | 3.9 | 0.17 | 3.9 | 0.22 | |
24.88 | 180-1109C-3H-6,48-50 | tephra layer | 10 | 27 | 68.2 | 0.80 | 0.22 | 0.04 | 13.9 | 0.18 | 1.97 | 0.09 | 0.08 | 0.02 | 0.17 | 0.03 | 0.46 | 0.04 | 4.9 | 0.09 | 4.1 | 0.10 | |
26.26 | 180-1109C-3H-7,36-38 | tephra layer | 10 | 40 | 67.0 | 0.38 | 0.20 | 0.02 | 14.0 | 0.11 | 2.70 | 0.09 | 0.08 | 0.02 | 0.14 | 0.01 | 0.60 | 0.03 | 5.2 | 0.17 | 3.5 | 0.09 | |
26.73 | 180-1109C-3H-CC | tephra layer | 6 | 15 | 69.0 | 0.41 | 0.08 | 0.02 | 14.4 | 0.09 | 2.93 | 0.06 | 0.04 | 0.04 | 0.00 | 0.00 | 0.60 | 0.02 | 5.1 | 0.21 | 3.8 | 0.16 | |
36.65 | 180-1109C-5H-1,75-77 | ash-enriched layer | 2 | 5 | 73.0 | 0.38 | 0.06 | 0.01 | 12.5 | 0.06 | 0.74 | 0.05 | 0.03 | 0.01 | 0.10 | 0.01 | 0.48 | 0.02 | 3.8 | 0.22 | 4.0 | 0.27 | |
51.27 | 180-1109C-6H-4,137-140 | ash-enriched layer | 3 | 8 | 70.4 | 0.31 | 0.27 | 0.03 | 11.2 | 0.09 | 3.80 | 0.10 | 0.12 | 0.04 | 0.01 | 0.01 | 0.28 | 0.02 | 3.8 | 0.21 | 3.9 | 0.04 | |
53.58 | 180-1109C-6H-6,68-69 | ash-enriched layer | 2 | 6 | 65.5 | 0.20 | 0.75 | 0.02 | 14.8 | 0.09 | 2.60 | 0.11 | 0.07 | 0.06 | 0.70 | 0.02 | 2.10 | 0.10 | 4.1 | 0.29 | 3.5 | 0.07 | |
104.68 | 180-1109C-12X-2,78-80 | tephra layer | 4 | 15 | 73.8 | 0.13 | 0.31 | 0.02 | 10.9 | 0.05 | 1.50 | 0.03 | 0.06 | 0.05 | 0.21 | 0.01 | 1.40 | 0.02 | 2.6 | 0.05 | 2.0 | 0.07 | |
112.94 | 180-1109C-13X-1,94-95 | tephra layer | 4 | 14 | 72.0 | 0.52 | 0.07 | 0.02 | 11.7 | 0.13 | 3.90 | 0.09 | 0.05 | 0.04 | 0.00 | 0.00 | 0.28 | 0.01 | 4.0 | 0.23 | 4.2 | 0.16 | |
119.82 | 180-1109C-13X-6,32-33 | volcaniclastic layer | 6 | 36 | 69.8 | 0.39 | 0.15 | 0.02 | 12.2 | 0.09 | 2.50 | 0.17 | 0.06 | 0.02 | 0.03 | 0.01 | 0.26 | 0.02 | 4.5 | 0.13 | 4.0 | 0.07 | |
150.90 | 180-1109C-17X-1,40-42 | volcaniclastic layer | 5 | 23 | 68.3 | 0.61 | 0.23 | 0.03 | 15.3 | 0.08 | 1.70 | 0.08 | 0.11 | 0.02 | 0.20 | 0.02 | 0.53 | 0.03 | 4.7 | 0.23 | 4.4 | 0.16 | |
166.13 | 180-1109C-18X-5,33-35 | volcaniclastic layer | 5 | 20 | 57.9 | 0.68 | 0.99 | 0.15 | 17.2 | 1.41 | 7.80 | 0.09 | 0.11 | 0.05 | 3.00 | 0.38 | 6.30 | 0.43 | 5.0 | 0.28 | 2.2 | 0.23 | |
276.66 | 180-1109C-30X-1,106-107 | tephra layer | 2 | 5 | 64.2 | 0.62 | 0.93 | 0.02 | 14.5 | 0.07 | 4.00 | 0.11 | 0.12 | 0.03 | 1.05 | 0.04 | 2.80 | 0.07 | 4.1 | 0.22 | 1.9 | 0.04 | |
310.97 | 180-1109C-33X-5,47-50 | tephra layer | 2 | 5 | 74.2 | 0.18 | 0.06 | 0.01 | 12.4 | 0.12 | 0.45 | 0.06 | 0.02 | 0.02 | 0.05 | 0.01 | 0.62 | 0.03 | 2.9 | 0.06 | 4.6 | 0.01 | |
371.61 | 180-1109D-3R-2,141-145 | volcaniclastic layer | 4 | 10 | 72.4 | 0.43 | 0.11 | 0.01 | 12.5 | 0.04 | 0.77 | 0.04 | 0.01 | 0.01 | 0.21 | 0.01 | 0.87 | 0.04 | 3.8 | 0.16 | 3.2 | 0.23 | |
375.13 | 180-1109D-3R-5,99-101 | volcaniclastic layer | 5 | 17 | 72.5 | 0.64 | 0.16 | 0.03 | 12.5 | 0.12 | 0.77 | 0.07 | 0.05 | 0.03 | 0.26 | 0.02 | 0.81 | 0.04 | 3.5 | 0.18 | 3.7 | 0.36 | |
471.51 | 180-1109D-13R-6,87-89 | Chemically different population of glass particles within an individual deposit, 1 | volcaniclastic layer | 2 | 5 | 73.4 | 0.23 | 0.11 | 0.02 | 12.4 | 0.03 | 0.70 | 0.04 | 0.01 | 0.01 | 0.13 | 0.01 | 0.73 | 0.02 | 3.4 | 0.03 | 4.2 | 0.04 |
471.51 | 180-1109D-13R-6,87-89 | Chemically different population of glass particles within an individual deposit, 2 | volcaniclastic layer | 2 | 7 | 71.4 | 0.35 | 0.10 | 0.01 | 12.9 | 0.14 | 0.73 | 0.06 | 0.01 | 0.01 | 0.18 | 0.01 | 1.03 | 0.03 | 3.4 | 0.11 | 4.3 | 0.10 |