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Zircon populations in Lewisian quartzite, gneiss and granite north of Loch Laxford, Sutherland
Published online by Cambridge University Press: 01 May 2009
Summary
Zircon populations in quartzo-feldspathic gneisses of the Rhiconich group of the Lewisian are indicative of a sedimentary derivation of the rocks. They are similar to the zircon population of an interbanded quartzite but differ markedly from that of an intrusive granite vein.
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