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The Skye igneous centre, forming part of the British Tertiary magmatic province, developed over a ∼7 Myr period (61–54 Ma) and is characterized by a complex suite of lavas, hypabyssal and intrusive rocks of picritic to granitic composition. The intrusion of magma from mantle to crust at ∼2×10−3km3/yr (6 Mt/yr) advected magmatic heat of roughly 0·2 GW averaged over the period of magmatism supportin...

Magmatic Evolution of the Skye Igneous Centre, Western Scotland: Modelling of Assimilation, Recharge and Fractional Crystallization