1.99 Ga mafic magmatism in the Rona terrane of the Lewisian Gneiss Complex in Scotland

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1.99 Ga mafic magmatism in the Rona terrane of the Lewisian Gneiss Complex in Scotland

The Scourie dyke swarm has long been important to unravelling the geological history of the Lewisian Gneiss Complex (LGC) and the North Atlantic Craton. Recent dating has documented that the majority of those dykes were emplaced between c. 2418–2375 Ma. Here we show that a quartz dolerite dyke in th...

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Bibliographic Details
Main Authors:	Baker, T., Prave, A., Spencer, Christopher
Format:	Journal Article
Published:	Elsevier BV 2019
Online Access:	http://hdl.handle.net/20.500.11937/74309

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