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Journal of the Geological Society; 1995; v. 152; issue.6; p. 979-983;
DOI: 10.1144/GSL.JGS.1995.152.01.17
© 1995 Geological Society of London

Papers

Magnesian basalts from the Hebrides, Scotland: chemical composition and relationship to the Iceland plume

Ray W. Kent1,2

1 Department of Geology & Geophysics, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, UK
2 Department of Geology, University of Leicester, Leicester LE1 7RH, UK

The Hebridean Tertiary igneous province lay 700–900 km south of a presumed plume centre, and >500 km landward of a rifted continental margin prior to opening of the northeast Atlantic. The Province includes a small number of magnesian basalts containing olivine phenocrysts with core compositions equal to, or in excess of, Fo89. Olivine-liquid equilibrium calculations suggest that these phenocrysts formed from liquids with MgO contents of 14–15 wt%, and in rare instances, 18–20 wt%. The liquidus temperatures of these magmas imply mantle potential temperatures of 1350–1460°C at distances up to 900 km from the axis of the Iceland plume. Their emplacement at c. 60 Ma implies either a long-established hotspot, or active channeling of plume material along the base of the plate towards a region undergoing considerable lower crustal extension.


Keywords: Hebrides, basalt, olivine, temperature, plumes.




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