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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):
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):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Latitude of eventLatitude
Longitude of eventLongitude
Elevation of eventElevationm
Latitude of event 2Latitude 2
Longitude of event 2Longitude 2
Elevation of event 2Elevation 2m
Sample typeSamp typeKharin, Gennady S
Number of observationsNOBS#Kharin, Gennady S
10 Silicon dioxideSiO2%Kharin, Gennady SWet chemistry
11 Titanium dioxideTiO2%Kharin, Gennady SWet chemistry
12 Aluminium oxideAl2O3%Kharin, Gennady SWet chemistry
13 Iron oxide, Fe2O3Fe2O3%Kharin, Gennady SWet chemistry
14 Iron oxide, FeOFeO%Kharin, Gennady SWet chemistry
15 Manganese oxideMnO%Kharin, Gennady SWet chemistry
16 Magnesium oxideMgO%Kharin, Gennady SWet chemistry
17 Calcium oxideCaO%Kharin, Gennady SWet chemistry
18 Sodium oxideNa2O%Kharin, Gennady SWet chemistry
19 Potassium oxideK2O%Kharin, Gennady SWet chemistry
20 Phosphorus pentoxideP2O5%Kharin, Gennady SWet chemistry
21 Oxides/hydroxidesOx/hydrox%Kharin, Gennady SCalculatedother
22 SumSum%Kharin, Gennady SCalculated
Size:
135 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Latitude

Longitude

Elevation [m]

Latitude 2

Longitude 2

Elevation 2 [m]

Samp type

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 70.550-14.900-175070.567-15.267-1740conical 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 augite348.201.3314.723.758.510.318.3711.602.000.170.160.5999.71
AK10-807 67.750-18.503-70067.750-18.533-490angular fragments and blocks of crystallized basalts with augite pheno-crysts; some specimens are porous348.891.8314.571.8211.920.256.0010.872.270.230.240.9099.79
AK15-1343-1 68.417-18.900-144068.400-18.850-1200angular fragments of crystallized basalts with small plagioclase segregations149.762.6517.612.297.470.214.077.523.722.551.300.1699.31
AK15-1349 70.350-15.400-105070.367-15.433-800conical 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 oxides148.880.9015.410.739.250.188.7612.531.810.160.150.2699.00
AK15-1350 70.667-14.300-140070.650-14.333basalts represented by specimens of two kinds: 1) fragments of spheroidal lavas with hyaline crust; 2) porphyritic basalts with plagioclase (An 37-68) and olivine segregations848.371.7814.493.998.280.317.4211.122.130.540.250.9299.60
AK15-1351 71.067-12.950-65071.050-13.017-400fragments of spheroidal lavas with pores and hyaline quenched crust; segregations of plagioclase (An 40-70) and olivine449.201.1514.021.758.540.209.3611.961.840.230.120.7199.08
AK23-2105 67.167-18.883-450sharp angular fragments of black basaltic glass and porous hyalobasalts with segregations of plagioclase (An 51-65) and augite148.652.5012.915.989.350.215.748.832.520.630.371.2598.94
AK23-2117 67.800-18.483-540small angular fragments of scoriaceous basalts and fine-porous hyalobasalts144.531.8213.803.0311.300.197.359.112.521.110.384.7799.91
AK23-2118 67.833-18.350-53067.850-18.550-600specimens 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 flow949.651.0214.311.6611.180.217.7111.692.080.110.090.85100.56