(Table 3) Chemical composition of basalts from Kolbeinsey Ridge and adjacent areas

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...

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Bibliographic Details
Main Author: Kharin, Gennady S
Format: Dataset
Language:English
Published: PANGAEA 1980
Subjects:
AK10-793-2
AK10-807
AK15-1343-1
AK15-1349
AK15-1350
AK15-1351
AK23-2105
AK23-2117
AK23-2118
Akademik Kurchatov
AKU10
AKU15
AKU23
Aluminium oxide
Archive of Ocean Data
ARCOD
Calcium oxide
Calculated
Dredge
DRG
Elevation of event
Elevation of event 2
Event label
Iron oxide
Fe2O3
FeO
Kolbeinsey Ridge
Latitude of event
Latitude of event 2
Longitude of event
Longitude of event 2
Magnesium oxide
Manganese oxide
Number of observations
Oxides/hydroxides
Phosphorus oxide
Potassium oxide
Sample type
Silicon dioxide
Sodium oxide
Sum
Titanium dioxide
Wet chemistry
Jan Mayen
Kolbeinsey
Iceland
Jan Mayen Island
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.755431
https://doi.org/10.1594/PANGAEA.755431
Description
Summary: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.

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