Kharin, Gennady S (1980): (Table 3) Chemical composition of basalts from Kolbeinsey Ridge and adjacent areas [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.755431, Supplement to: Kharin, GS (1980): The basalts of the Kolbeinsey submarine ridge (Norwegian-Greenland Basin). Oceanology, 20(1), 50-55
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Abstract:
Petrochemical variations in composition of basalts along the axial part of the Kolbeinsey mid-ocean ridge were studied. It was found that principal mass of these basalts has tholeiitic composition. Alkalinity of these basalts increases near zones of transform transverse faults; it increases likewise toward Iceland, and especially in the direction of Jan Mayen Island.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 69.264583 * Median Longitude: -16.540833 * South-bound Latitude: 67.166667 * West-bound Longitude: -18.900000 * North-bound Latitude: 71.066667 * East-bound Longitude: -12.950000
Minimum Elevation: -1750.0 m * Maximum Elevation: -400.0 m
Event(s):
AK10-793-2 * Latitude Start: 70.550000 * Longitude Start: -14.900000 * Latitude End: 70.566667 * Longitude End: -15.266667 * Elevation Start: -1750.0 m * Elevation End: -1740.0 m * Location: Kolbeinsey Ridge * Campaign: AKU10 * Basis: Akademik Kurchatov * Method/Device: Dredge (DRG)
AK10-807 * Latitude Start: 67.750000 * Longitude Start: -18.503333 * Latitude End: 67.750000 * Longitude End: -18.533333 * Elevation Start: -700.0 m * Elevation End: -490.0 m * Location: Kolbeinsey Ridge * Campaign: AKU10 * Basis: Akademik Kurchatov * Method/Device: Dredge (DRG)
AK15-1343-1 * Latitude Start: 68.416667 * Longitude Start: -18.900000 * Latitude End: 68.400000 * Longitude End: -18.850000 * Elevation Start: -1440.0 m * Elevation End: -1200.0 m * Location: Kolbeinsey Ridge * Campaign: AKU15 * Basis: Akademik Kurchatov * Method/Device: Dredge (DRG)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | Elevation of event | Elevation | m | |||
5 | Latitude of event 2 | Latitude 2 | ||||
6 | Longitude of event 2 | Longitude 2 | ||||
7 | Elevation of event 2 | Elevation 2 | m | |||
8 | Sample type | Samp type | Kharin, Gennady S | |||
9 | Number of observations | NOBS | # | Kharin, Gennady S | ||
10 | Silicon dioxide | SiO2 | % | Kharin, Gennady S | Wet chemistry | |
11 | Titanium dioxide | TiO2 | % | Kharin, Gennady S | Wet chemistry | |
12 | Aluminium oxide | Al2O3 | % | Kharin, Gennady S | Wet chemistry | |
13 | Iron oxide, Fe2O3 | Fe2O3 | % | Kharin, Gennady S | Wet chemistry | |
14 | Iron oxide, FeO | FeO | % | Kharin, Gennady S | Wet chemistry | |
15 | Manganese oxide | MnO | % | Kharin, Gennady S | Wet chemistry | |
16 | Magnesium oxide | MgO | % | Kharin, Gennady S | Wet chemistry | |
17 | Calcium oxide | CaO | % | Kharin, Gennady S | Wet chemistry | |
18 | Sodium oxide | Na2O | % | Kharin, Gennady S | Wet chemistry | |
19 | Potassium oxide | K2O | % | Kharin, Gennady S | Wet chemistry | |
20 | Phosphorus pentoxide | P2O5 | % | Kharin, Gennady S | Wet chemistry | |
21 | Oxides/hydroxides | Ox/hydrox | % | Kharin, Gennady S | Calculated | other |
22 | Sum | Sum | % | Kharin, Gennady S | Calculated |
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 Latitude 2 | 6 Longitude 2 | 7 Elevation 2 [m] | 8 Samp type | 9 NOBS [#] | 10 SiO2 [%] | 11 TiO2 [%] | 12 Al2O3 [%] | 13 Fe2O3 [%] | 14 FeO [%] | 15 MnO [%] | 16 MgO [%] | 17 CaO [%] | 18 Na2O [%] | 19 K2O [%] | 20 P2O5 [%] | 21 Ox/hydrox [%] | 22 Sum [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
AK10-793-2 | 70.550 | -14.900 | -1750 | 70.567 | -15.267 | -1740 | conical fragments of spheroidal lavas with small pores and well developed quench crusts. Individual specimens contain up to 20% pheno-crysts of plagioclase (An 50-70) and augite | 3 | 48.20 | 1.33 | 14.72 | 3.75 | 8.51 | 0.31 | 8.37 | 11.60 | 2.00 | 0.17 | 0.16 | 0.59 | 99.71 |
AK10-807 | 67.750 | -18.503 | -700 | 67.750 | -18.533 | -490 | angular fragments and blocks of crystallized basalts with augite pheno-crysts; some specimens are porous | 3 | 48.89 | 1.83 | 14.57 | 1.82 | 11.92 | 0.25 | 6.00 | 10.87 | 2.27 | 0.23 | 0.24 | 0.90 | 99.79 |
AK15-1343-1 | 68.417 | -18.900 | -1440 | 68.400 | -18.850 | -1200 | angular fragments of crystallized basalts with small plagioclase segregations | 1 | 49.76 | 2.65 | 17.61 | 2.29 | 7.47 | 0.21 | 4.07 | 7.52 | 3.72 | 2.55 | 1.30 | 0.16 | 99.31 |
AK15-1349 | 70.350 | -15.400 | -1050 | 70.367 | -15.433 | -800 | conical fragments of spheroidal lavas with small pores and labradorite segregations; surfaces in contact with water are overgrown with serpulae and covered with bloom of Fe-Mn oxides | 1 | 48.88 | 0.90 | 15.41 | 0.73 | 9.25 | 0.18 | 8.76 | 12.53 | 1.81 | 0.16 | 0.15 | 0.26 | 99.00 |
AK15-1350 | 70.667 | -14.300 | -1400 | 70.650 | -14.333 | basalts represented by specimens of two kinds: 1) fragments of spheroidal lavas with hyaline crust; 2) porphyritic basalts with plagioclase (An 37-68) and olivine segregations | 8 | 48.37 | 1.78 | 14.49 | 3.99 | 8.28 | 0.31 | 7.42 | 11.12 | 2.13 | 0.54 | 0.25 | 0.92 | 99.60 | |
AK15-1351 | 71.067 | -12.950 | -650 | 71.050 | -13.017 | -400 | fragments of spheroidal lavas with pores and hyaline quenched crust; segregations of plagioclase (An 40-70) and olivine | 4 | 49.20 | 1.15 | 14.02 | 1.75 | 8.54 | 0.20 | 9.36 | 11.96 | 1.84 | 0.23 | 0.12 | 0.71 | 99.08 |
AK23-2105 | 67.167 | -18.883 | -450 | sharp angular fragments of black basaltic glass and porous hyalobasalts with segregations of plagioclase (An 51-65) and augite | 1 | 48.65 | 2.50 | 12.91 | 5.98 | 9.35 | 0.21 | 5.74 | 8.83 | 2.52 | 0.63 | 0.37 | 1.25 | 98.94 | |||
AK23-2117 | 67.800 | -18.483 | -540 | small angular fragments of scoriaceous basalts and fine-porous hyalobasalts | 1 | 44.53 | 1.82 | 13.80 | 3.03 | 11.30 | 0.19 | 7.35 | 9.11 | 2.52 | 1.11 | 0.38 | 4.77 | 99.91 | |||
AK23-2118 | 67.833 | -18.350 | -530 | 67.850 | -18.550 | -600 | specimens of two types: 1) crustal (20 cm thick) hyalobasalts with black glass covered by thin films of hydrogoethite; weakly magnetic; 2) isometric porphyritic basalts without crust; magnetic and strongly magnetic, evidently from interior of a lava flow | 9 | 49.65 | 1.02 | 14.31 | 1.66 | 11.18 | 0.21 | 7.71 | 11.69 | 2.08 | 0.11 | 0.09 | 0.85 | 100.56 |