Schmincke, Hans-Ulrich (1983): (Table 2) Geochemistry of rhyolitic glass shards from ashes showing original and recalculated analyses at DSDP Leg 70 Holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.816346, In supplement to: Schmincke, H-U (1983): Rhyolitic and basaltic ashes from the Galapagos Mounds area, Leg 70, Deep Sea Drilling Project. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 69, 451-457, https://doi.org/10.2973/dsdp.proc.69.120.1983
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 0.843975 * Median Longitude: -86.180700 * South-bound Latitude: 0.566700 * West-bound Longitude: -86.410000 * North-bound Latitude: 1.613200 * East-bound Longitude: -86.090000
Date/Time Start: 1979-11-15T00:00:00 * Date/Time End: 1979-11-29T00:00:00
Minimum Elevation: -2781.0 m * Maximum Elevation: -2677.0 m
Event(s):
70-506D * Latitude: 0.607000 * Longitude: -86.091300 * Date/Time: 1979-11-15T00:00:00 * Elevation: -2707.0 m * Penetration: 31.9 m * Recovery: 29.2 m * Location: North Pacific/MOUND * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 9 cores; 31.9 m cored; 0 m drilled; 91.6 % recovery
70-507D * Latitude: 0.566700 * Longitude: -86.090000 * Date/Time: 1979-11-20T00:00:00 * Elevation: -2689.0 m * Penetration: 38.7 m * Recovery: 36.5 m * Location: North Pacific/MOUND * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 38.7 m cored; 0 m drilled; 94.3 % recovery
70-509 * Latitude: 0.589000 * Longitude: -86.131500 * Date/Time: 1979-11-27T00:00:00 * Elevation: -2677.0 m * Penetration: 32.3 m * Recovery: 32.5 m * Location: North Pacific/MOUND * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 9 cores; 32.3 m cored; 0 m drilled; 100.5 % recovery
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
135 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 Comment | 7 SiO2 [%] | 8 TiO2 [%] | 9 Al2O3 [%] | 10 FeO [%] | 11 MnO [%] | 12 MgO [%] | 13 CaO [%] | 14 Na2O [%] | 15 K2O [%] | 16 P2O5 [%] | 17 Total [%] | 18 - |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 70-506D | 0.6070 | -86.0913 | -2707 | 70-506D-4-2,30-32 | Single shard; original value | 72.19 | 0.24 | 13.03 | 0.97 | 0.03 | 0.22 | 0.98 | 3.24 | 4.21 | 0.04 | 95.16 | 78.27 |
| 70-506D | 0.6070 | -86.0913 | -2707 | 70-506D-4-2,30-32 | Single shard; recalculated | 75.86 | 0.25 | 13.69 | 1.02 | 0.03 | 0.23 | 1.03 | 3.40 | 4.42 | 0.04 | 100.00 | |
| 70-506D | 0.6070 | -86.0913 | -2707 | 70-506D-4-2,30-32 | Average of three shards of similar composition; original value | 71.98 | 0.14 | 12.67 | 0.80 | 0.09 | 0.26 | 0.91 | 3.05 | 3.51 | 0.05 | 93.46 | 77.94 |
| 70-506D | 0.6070 | -86.0913 | -2707 | 70-506D-4-2,30-32 | Average of three shards of similar composition; recalculated | 77.02 | 0.15 | 13.56 | 0.86 | 0.10 | 0.28 | 0.97 | 3.26 | 3.76 | 0.05 | 100.00 | |
| 70-509 | 0.5890 | -86.1315 | -2677 | 70-509-4-2,66-68 | Original value | 72.06 | 0.23 | 13.25 | 0.78 | 0.07 | 0.19 | 0.99 | 3.72 | 3.91 | 0.00 | 95.20 | 76.11 |
| 70-509 | 0.5890 | -86.1315 | -2677 | 70-509-4-2,66-68 | Recalculated | 75.69 | 0.24 | 13.92 | 0.82 | 0.07 | 0.20 | 1.04 | 3.91 | 4.11 | 0.00 | 100.00 | |
| 70-510 | 1.6132 | -86.4100 | -2781 | 70-510-7-5,50-52 | Original value | 70.17 | 0.21 | 11.96 | 2.96 | 0.11 | 0.04 | 0.60 | 3.93 | 4.24 | 0.01 | 94.22 | 76.13 |
| 70-510 | 1.6132 | -86.4100 | -2781 | 70-510-7-5,50-52 | Recalculated | 74.47 | 0.22 | 12.69 | 3.14 | 0.12 | 0.04 | 0.64 | 4.17 | 4.50 | 0.01 | 100.00 | |
| 70-507D | 0.5667 | -86.0900 | -2689 | 70-507D-3-2,58-60 | Original value | 75.05 | 0.05 | 11.98 | 0.53 | 0.01 | 0.09 | 0.56 | 3.47 | 3.77 | 0.00 | 95.51 | 80.32 |
| 70-507D | 0.5667 | -86.0900 | -2689 | 70-507D-3-2,58-60 | Recalculated | 78.58 | 0.05 | 12.54 | 0.55 | 0.01 | 0.09 | 0.59 | 3.63 | 3.95 | 0.00 | 100.00 |