Partial melting of metabasic rocks in Val Strona di Omegna, Ivrea Zone, northern Italy

Field and petrographic observations combined with major and trace element bulk rock geochemistry show that metabasic rocks within Val Strona di Omegna in the central Ivrea Zone partially melted during granulite facies regional metamorphism. A transition from granoblastic amphibolite facies metabasic...

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Bibliographic Details
Main Authors: Kunz, B., Johnson, Tim, White, R., Redler, C.
Format: Journal Article
Published: Elsevier BV 2014
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/14040