Data for: Ordovician shoshonitic to ultrapotassic volcanism in the central Norwegian Caledonides: the result of sediment subduction, mantle metasomatism and mantle partial melting

Published: 31-03-2020| Version 1 | DOI: 10.17632/djhtht4sch.1
Contributor:
Bjørgunn Dalslåen

Description

Geochemical analyses (XRF, ICP-MS)

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