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
Published in:Precambrian Research
Main Authors: Baker, T.R., Prave, A.R., Spencer, C.J.
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://risweb.st-andrews.ac.uk/portal/en/researchoutput/199-ga-mafic-magmatism-in-the-rona-terrane-of-the-lewisian-gneiss-complex-in-scotland(920d462f-99fe-4786-b5a3-8ec1167b4ab1).html
https://doi.org/10.1016/j.precamres.2018.12.027