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

DOI

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.

Supplement to: Kharin, Gennady S (1980): The basalts of the Kolbeinsey submarine ridge (Norwegian-Greenland Basin). Oceanology, 20(1), 50-55

Identifier
DOI https://doi.org/10.1594/PANGAEA.755431
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.755431
Provenance
Creator Kharin, Gennady S
Publisher PANGAEA
Publication Year 1980
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 135 data points
Discipline Chemistry; Natural Sciences
Spatial Coverage (-18.900W, 67.167S, -12.950E, 71.067N); Kolbeinsey Ridge