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Emplacement of mantle-derived magma (magmatic accretion) is often presumed or inferred to be an important cause of regional granulite facies metamorphism and crustal anatexis. The juxtaposition of mafic cumulates and regionally distributed granulite facies rocks has led some to consider the Ivrea zone (northern Italy, Southern Alps) as an important exposure that demonstrates this causal relationsh...

Metamorphism and Anatexis in the Mafic Complex Contact Aureole, Ivrea Zone, Northern Italy