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The parental magma on Rhum: evidence from alkaline segregations and veins in the peridotites from Salisbury's Dam

Published online by Cambridge University Press:  01 May 2009

D. E. Kitchen
D. E. Kitchen
Affiliation:
University of Ulsterat Jordanstown, Shore Road, Newtownabbey, Co. Antrim, BT37 0QB, Northern Ireland
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Abstract

Feldspathic peridotites on Rhum contain teschenite segregations and veins. Bulk rock and mineral compositional trends define a path of alkali and iron enrichment related to discontinuous isolation of evolving intercumulus melts. Compositionally zoned and skeletal crystals of actinolite, zircon, apatite, sphene, epidote and chlorite are enclosed by clear analcime, and appear to have grown directly from a water-rich fluid at some undercooling, and below dry equilibrium solidus temperatures. The occurrence of late stage residua with undersaturated alkalirich characteristics in the Rhum ultrabasic complex suggests that the patental magma was alkaline rather than tholeiitic, and had similarities to the Plateau Magmas on Skye.

Type
Articles
Information
Geological Magazine , Volume 122 , Issue 5 , September 1985 , pp. 529 - 537
Copyright
Copyright © Cambridge University Press 1985

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